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Article

Using Disaster Outcomes to Validate Components of Social Vulnerability to Floods: Flood Deaths and Property Damage across the USA

1
The Earth Institute, Columbia University, New York, NY 10025, USA
2
Cloud to Street, New York, NY 112131, USA
3
Dell EMC, Austin, TX 78759, USA
4
Department of Environment and Society, Utah State University, Logan, UT 84321, USA
5
Center for International Earth Science Information Network (CIESIN), The Earth Institute at Columbia University, Palisades, NY 10964, USA
*
Author to whom correspondence should be addressed.
Sustainability 2020, 12(15), 6006; https://doi.org/10.3390/su12156006
Submission received: 12 June 2020 / Revised: 18 July 2020 / Accepted: 20 July 2020 / Published: 27 July 2020
(This article belongs to the Special Issue Climate Risk and Vulnerability Mapping)

Abstract

:
Social vulnerability indicators seek to identify populations susceptible to hazards based on aggregated sociodemographic data. Vulnerability indices are rarely validated with disaster outcome data at broad spatial scales, making it difficult to develop effective national scale strategies to mitigate loss for vulnerable populations. This paper validates social vulnerability indicators using two flood outcomes: death and damage. Regression models identify sociodemographic factors associated with variation in outcomes from 11,629 non-coastal flood events in the USA (2008–2012), controlling for flood intensity using stream gauge data. We compare models with (i) socioeconomic variables, (ii) the composite social vulnerability index (SoVI), and (iii) flood intensity variables only. The SoVI explains a larger portion of the variance in death (AIC = 2829) and damage (R2 = 0.125) than flood intensity alone (death—AIC = 2894; damage—R2 = 0.089), and models with individual sociodemographic factors perform best (death—AIC = 2696; damage—R2 = 0.229). Socioeconomic variables correlated with death (rural counties with a high proportion of elderly and young) differ from those related to property damage (rural counties with high percentage of Black, Hispanic and Native American populations below the poverty line). Results confirm that social vulnerability influences death and damage from floods in the USA. Model results indicate that social vulnerability models related to specific hazards and outcomes perform better than generic social vulnerability indices (e.g., SoVI) in predicting non-coastal flood death and damage. Hazard- and outcome-specific indices could be used to better direct efforts to ameliorate flood death and damage towards the people and places that need it most. Future validation studies should examine other flood outcomes, such as evacuation, migration and health, across scales.

1. Introduction

1.1. From Risk to Vulnerability

Social vulnerability research has its contemporary origins in risk–hazard research focused on the exposure of people or places to environmental threats [1], demonstrating how various types of environmental or “natural” hazards differentially affect populations based on their underlying susceptibility to harm. The National Flood Insurance Program in the United States reflects the policy impacts of this research [2]. This significance notwithstanding, inadequate attention to the socio-economic conditions that predispose specific populations to greater exposure and consequences has led to various critiques of the risk–hazard approach [3]. New frameworks emerged that focused on societal vulnerability to hazards and captured the root causes of exposure, sensitivity and coping capacity in relation to hazards [4,5]. These frameworks were ultimately enlarged to include the vulnerability of the environment or ecosystem in question and its impacts on exposed populations [6]. A simple definition emerging from this research is that vulnerability is the propensity for loss of lives, livelihood or property when exposed to a hazard [6,7].
Scientists studying the impacts, vulnerability and adaptation associated with climate change grew beyond the risk–hazards framework and began to focus on quantifying and understanding the relationships between hazards, exposure, sensitivity and coping capacity [8,9,10,11,12,13,14,15]. Place-based assessments of vulnerability provided insights into these relationships [16,17,18,19,20,21,22,23,24,25] but limited the ability to generalize an understanding of vulnerability across wider geographies. Thus, efforts were made to quantify the social factors that predict the people and locations with a high propensity for loss of life, livelihood and property from a hazard [26] in order to guide disaster management and climate change adaptation policy [11,12]. Indices such as the Social Vulnerability Index (SoVI) are widely used in the literature [25,27,28] and have been formally adopted by government agencies [29], and in vulnerability maps used for adaptation planning [30]. Yet until recently there has been insufficient attention paid to validation [31,32,33,34,35]. The predictive ability of social vulnerability indices remains largely untested, since few studies have examined how vulnerability indices relate to loss and damages, or which socio-demographic factors are most predictive of harm [28,32]. This limits the ability of policy makers to target adaptation strategies that could reduce harm to populations most at risk, because the indices available may be inadequate for predicting loss in a hazard. Validation of widely used indices aids understanding of how factors of social vulnerability may remain constant or change over spatial, temporal and socio-political scales, as well as across different types of hazards [31]. Quantitative social vulnerability assessment requires more attention to internal validity through sensitivity and uncertainty analysis (e.g., Tate et al. [32]) and external validity through the comparison of disaster outcomes with vulnerability metrics (e.g., [34]). As climate-related hazards become more severe, it is important to assess the validity of vulnerability indicators and maps increasingly used to target adaptation resources [35].
Vulnerability assessments increasingly analyze coping capacity, the ability of an individual or population to mobilize assets, or entitlements to cope with loss or mitigate future harm from hazards [36,37,38,39,40,41,42,43,44]. Coping capacity is markedly difficult to measure over large geographic scales, and among diverse populations, because of data gaps and difficulties in quantifying the complexity of interactions among social structures, institutions and human agency. Metrics tend to capture this complexity inadequately, although a positive relationship between coping capacity and higher levels of education and investment in health has been proposed [10,39,45]. Research on resilience (sometimes defined as the ability to bounce back after a shock) has attempted to construct indices and quantitative assessments that include coping capacity [46,47,48]. These efforts, however, also lack empirical validation at large geographic scales. Overall, surprisingly few quantitative assessments of the specific factors leading to loss from hazards—or resilience to hazards—based on disaster outcomes exist [34]. Here we add to existing social vulnerability external validation studies of flooding [34,49] by assessing two outcome measures—fatality and property damage—across the continental United States from 2008 to 2012 at the county scale, adopting the above definition of vulnerability. This study represents a larger geospatial extent than previous studies, identifying social factors that transcend local place context that are related to loss and damage across the USA. We focus on riverine flooding and control for flood magnitude, with stream gauge data to examine social factors leading to additional death and damage. The many other potential outcomes related to flooding, such as health effects or long-term economic loss, remain a subject for future research.

1.2. Measuring and Validating Social Vulnerability to Flood Hazards

Flood events affect more people globally than any other type of environmental hazard, and are expected to increase in severity and frequency because of climate and demographic changes [50,51,52,53]. Flood vulnerability research has typically focused on hazard (the flood event) and exposure (population and livelihoods that could be impacted by the event). Exposure analyses, as explored in the environmental sciences and engineering, commonly rely on physically-based hydrologic and hydraulic modeling to estimate the extent, depth or frequency of flooding for a given storm event, and calculate the assets and population affected [54,55,56]. Both qualitative case studies [57,58] and indicator approaches (e.g., the SoVI or similar indices) [21,22,24,59,60,61,62] explore the differential impacts of floods on vulnerable people and places.
SoVI was developed by Cutter et al. [26] using a principal component analysis (PCA) on over 30 socio-demographic variables selected through a literature review, which are primarily derived from US census data. PCA is a data reduction technique that uses an orthogonal transformation to convert a set of correlated variables into a new reduced set of uncorrelated variables, or components. The new components that represent a large proportion of variance in the data form the indicators for an additive social vulnerability index.
Social vulnerability is multi-faceted, and no one hazard outcome can serve as a comprehensive proxy for vulnerability validation. Social factors associated with flood vulnerability differ depending on whether the focus is on ex ante mitigation, immediate response, or longer-term recovery from flood events [58]. Therefore, comprehensive validation of social vulnerability to floods requires assessing multiple outcomes, and the social conditions related to each, across the three aforementioned phases of the disaster cycle. Death and property damage, the focus of this analysis, spans the mitigation and immediate aftermath phases of the disaster cycle. Death and property damage were chosen as the outcomes for analysis because of data availability for every county, allowing us to examine salient social vulnerability factors generalizable to the continental US. Outcomes of flood events related to social vulnerability not covered in this paper include agricultural damage, ability to invest in future agricultural adaptation [63], out-migration, rate of return, ability to rebuild [64,65], property buyouts, health impacts not related to morality [15], and psychological impacts (see Rufat et al. [58] for a review of these and other outcomes). We focus our review more on empirical US case studies, the study area for this paper.

1.2.1. Flood Fatality

Social factors leading to fatalities from floods during the event (e.g., from drowning) and morbidity after the event (e.g., health complications; see [66]) differ between high–medium income and low-income countries [58,67]. In lower income countries, females and those who are poor are at a higher risk of flood fatality, often related to increased exposure by residing in the floodplain [67,68,69]. For example, more women than men drowned in the 1991 cyclone in Bangladesh, potentially due to women being homebound looking after children and valuables, traditional dress that restricts movements, or lower literacy rates [70]. In higher income countries, such as the USA, most fatalities during flood events are due to males drowning in vehicles [71,72,73]. Fatalities are more common in flash flood events, and in particular regions of the USA on the East Coast along Interstate 95, the Ohio River valley, and south-central Texas [71]. In the US, men exhibit riskier behavior than women in flood events, leading to high fatalities, in contrast to other hazard events in which women are generally more sensitive [72].
Common to all countries is the increased risk of flood-related death among the very young and very old [67,73,74,75]. The elderly are at risk of death because they may have difficulty evacuating or accessing medical services to treat heat, dehydration, stokes or heart attacks [72]. Furthermore, common to all countries is the higher risk of injury, death and damage from floods and hurricanes for ethnic minorities or communities of color (as well as other disasters, see [76]). Hurricane Katrina, for example, disproportionately affected African-American communities in terms of flood fatality [77]. In Hurricane Katrina, mortality rates were up to four times higher for Blacks than Whites, particularly among elderly populations, suggesting an interaction between race and age [78]. Economic disadvantages, residential choices and difficulty evacuating are all factors, related to systemic and institutional racism, that lead to higher fatality rates among minority populations [79]. Preparedness and mitigation investment by governments may also be systematically lower in communities of color, especially African-American communities [80], increasing their exposure and subsequent flood impacts.
Factors that reduce flood fatality include flood mitigation infrastructure [79,81], being in an urban area, and institutional investment in adaptation. Adaptation investments related to preparedness, early warning systems and evacuation plans have effectively lowered property damage and death rates [81]. In all regions of the world (except Sub-Saharan Africa [82]), flood fatality rates have declined since 1980, especially for countries with the largest GDP growth who are hypothesized to be investing in additional adaptation and mitigation [83]. However, early warning systems are less common in rural areas and emergency services more dispersed, compared to urban areas [84,85]. Other studies have found rural areas of the US to be more vulnerable to flood fatalities [86]. Differences may exist among urban areas. For example, rapidly urbanizing areas with less road connectivity were found to be more vulnerable in the Amazon [62] compared to other cities, and social vulnerability hotspots are located both in the urban center and periphery in Shanghai [27].

1.2.2. Property Damage

Property damage represents one component of total economic loss in flood hazard events. Other longer-term economic losses include job loss, crop damage, lost sales or closure of business [87,88], costs of relocation or return, migration, and difficulty finding new work if displaced. Previous research identifying social factors that lead to a higher propensity for property damages have included renter status, income, race and poverty in said factors [89]. Research on property damage at the household level indicates that lower socioeconomic status (e.g., poverty) is correlated with high damage rates because of lower building material quality and reduced ability to withstand flood damage [90]. In the US, for example, unreinforced masonry buildings, which are more susceptible to flood damage [91], are a more common housing type among minority populations in the US [76]. Other studies indicate African-American populations are more likely to experience disproportionate flood damage due to their location in floodplains where homes are cheaper, their reduced access to investments in home protection infrastructure, and receiving less protections from government-built flood mitigation infrastructure [76,80,92,93]. Race may interact with poverty to affect economic damage. For example, in Hurricane Katrina, only low income African-American populations had lower rates of returning and rebuilding, but not African-American populations in general [94]. Studies on tornado damage have found that US census blocks become significantly less poor and more White post-disaster, suggesting poor and minoritized populations may not be able to recover in place, and so migrate [64].
Research indicates that locations with higher rental rates experience a higher propensity for property damage. One exception may be for mobile homeowners: 40% of all tornado deaths occur in mobile homes, but the relationship for floods has, to our knowledge, not been tested [89]. Homeowners have higher rates of purchasing insurance and investing in flood mitigation [58,95], and therefore experience less damage [73,96]. Government programs for disaster assistance in the US, for example, privilege homeowners by design [97]. The relationship between purchasing insurance and race is unclear. One study in Georgia finds African-American populations over the age 45 are more likely to purchase insurance [98], while other studies point to lower rates of insurance purchase by minorities [99]. A recent study in South Carolina after the 2015 floods there, however, showed that National Flood Insurance payouts, loans for small business and Community Development Block Grants for disaster recovery were not reaching all socially vulnerable populations—especially Black populations [65].
Finally, rural areas are hypothesized to be more vulnerable to property loss as a share of total assets (e.g., normalized by total property value). Flood insurance for property owners is twice as common in urban as opposed to rural areas, for example [86]. Rural areas appear to have less flood-protective infrastructure (e.g., dams and levees) per capita compared to densely populated areas with high property values (the National Dam Database, which contains this information, is not available for public download. However, derivative reports using the data from Texas and New Mexico describe more flood protection levees in urban areas. The visual maps appear to favor flood control structure in urban areas.) [100,101,102]. In this regard, it is noteworthy that the US Federal Emergency Management Agency map modernization project, which updated and produced new flood maps for the US from 2003 to 2008 (immediately prior to this study), focused on highly populated and urban areas [103]. Finally, in the US, development in floodplains has increased in rural areas, but decreased in urban areas from 1980 to 2016, implying increased flood exposure in rural areas of the country [104].

1.3. Validating Social Vulnerability Based on Disaster Outcomes

Several quantitative flood vulnerability analyses combine exposure and sensitivity, and include both biophysical and social variables [15,21,25,59,72,79,105]. Most quantitative assessments use social vulnerability indicators, such as the SoVI, that are generalized for all types of natural hazards [26], and which do not choose sociodemographic variables specific to flood hazards. Different weighting of variables and scales of analysis can lead to unstable results that predict different communities being at risk when small changes in the weights of specific variables are made [31,32,33]. Even more problematic is the fact that often, social vulnerability indicators are not derived from empirical data on disaster loss specific to flood hazards [58].
We summarize relevant social vulnerability validation studies that use flood disaster outcomes in a regression in the USA (Table 1). We include the studies reviewed for social vulnerability validation by Rufat et al. [34], and an additional study that they exclude [79]. We exclude from this table studies that analyze all hazards, those using Pearson correlation, or qualitative validation. Regression analyses, rather than two variable Pearson correlations, importantly estimate the magnitude and direction of multiple effects while controlling for variation. To validate social vulnerability from flood hazard events, it is essential to control for event magnitude so as to assess the additional variance explained by social factors above and beyond hazard size. We report the geographic extent, temporal extent, scale of analysis, sample size, flood hazard control variable and main finding (statistically significant, with a + for positive correlation and—for negative) of the previous validation studies (Table 1).
Most previous attempts to validate the components of social vulnerability based on hazard outcomes have been general to all hazards [19], based on one flood disaster or place [34,60,61], use Pearson correlation [66,110], or are qualitative [23,111]. A few notable exceptions exist. Zahran et al. [79] analyzed over 800 flood events in Texas. Using precipitation and property damage data to control for flood magnitudes, they found two county-level demographic variables correlated to fatalities: high proportions of minorities and lower incomes. In other work, Finch et al. [61] found that high social vulnerability, when controlling for flood depth, predicts lower rate of residents returning home post-Katrina. Other single event flood studies [34,60] validate social vulnerability metrics and other social factors in relation to a variety of flood outcomes, including displacement rate, shelter, property loss and FEMA assistance. The largest spatial and temporal validation study (across the southeastern USA, and the highest sample size, from Bakkensen et al. [49]) included five hazard types (including floods). They found that the social vulnerability indices correlated with higher rates of property damage, but only one social vulnerability index (SVI; see [106]) was positively correlated with fatality rates.
Quantitative validations of social vulnerability to hazards, and to flooding in particular, at large spatial scales remain elusive. One of the challenges is selecting outcome variables that link to one or more of the components of vulnerability [112]. Possible outcome variables range from the immediate, such as fatalities and injuries, to the long-term, such as economic recovery [56]. Various outcome metrics, such as psychological wellbeing, are lacking in availability or are difficult to derive from extant sources, such as demographic data. Data-poor areas of the world are even more challenging to assess, and prevent broad-scale regional or global comparisons.
Despite these challenges, it is imperative to develop methods based on extant data to test the hypothesis that certain social dimensions increase vulnerability to hazards, such as floods [113]. Many researchers who develop social vulnerability indicators do so with the goal of drawing attention to the differential risks faced by those who are most disadvantaged [114,115]. Yet, without rigorous validation efforts, the development and use of such indicators risks being discredited owing to claims that they are unable to predict future harm [35,116]. The ability to understand and predict future risks is particularly important as discourse around loss and damage rises in the UN Framework Convention on Climate Change [117]. Recent social vulnerability validation studies call for more research in order to identify which social vulnerability models and factors consistently explain disaster outcomes, across hazards, outcomes and spatial and temporal scales [58]. This paper contributes to this research by providing the broadest spatial scale validation of social vulnerability to flood hazards to date. We estimate the socio-economic dimensions of vulnerability to death and damage in floods over a large number of events (n = 11,938, all major flood events from 2008 to 2012) in the contiguous United States, controlling for hazard magnitude. Generalized linear regression models address four primary research questions at the US county scale:
  • Which demographic variables predict fatalities directly attributed to floods?
  • Which demographic variables are associated with higher relative flood property damages?
  • Does a composite index of social vulnerability (SoVI) correlate with flood death and damage when accounting for hazard intensity?
  • Which populations and their locations are most likely to experience death and damage in a large (500-year) future flood event?

2. Materials and Methods

Our general approach to social vulnerability validation for floods was to regress flood outcome variables for which data across the contiguous USA were available, and the relative hazard magnitude could be controlled. Property damage and fatalities are two outcomes that fit these criteria, and have been used in other vulnerability validation studies as dependent variables in regression [34,49,79]. Stream gauges can control for riverine and flash flood (but not coastal floods), and we focus on these two flood types for validation. Data analysis and methodological details are provided below.

2.1. Data

2.1.1. Property and Fatality Data

Model response variables—fatality and property damage—are available through SHELDUS [118] version 14.1, downloaded in July 2016 (more recent versions of these data are now available through the Center for Emergency Management and Homeland Security at Arizona State University: https://cemhs.asu.edu/node/7). All flood outcome data were limited to flood events in the contiguous US from 2008 to 2012, excluding coastal floods (n = 11,938). The years 2008–2012 were chosen because they represented the two years precluding and following the 2010 Census, and we assume social dynamics to be stationary for approximately the 5 years of this analysis. We used stream gauge data to control for hazard magnitude, effective for riverine and flash flooding, the flood types included in this analysis. We excluded coastal floods from our analysis as these would have required windspeed or storm surge to control for hazard magnitude, and storm surge data across the US is unavailable. Flood fatalities and damage are the only consistent flood event outcomes in SHELDUS, and were the only ones available across the contiguous US at the time of this study.
Flood fatality data in SHELDUS are from the Storm Data publication provided by the US National Centers for Environmental Information (NCEI, formerly the National Climatic Data Center). Storm Data preparers from the National Weather Service report fatality information in total numbers per event (and usually per county). When the NCEI data report fatalities across several counties, SHELDUS splits the fatality data into each location reported. It is unclear how many fatalities are “direct” (e.g., drowning in water) vs. “indirect” (e.g., medical supplies at a home ran out due to the flood preventing gathering supplies), but these descriptions are sometimes included the event narrative. A total of 247 non-coastal flood fatality events (an event for which at least one death occurred), and a total of 335 deaths, occurred between 2008 and 2012, 238 of which had event descriptions. The quality of these data are subject to National Weather Service reporting, but it is considered the best officially verified and highest quality dataset for significant weather phenomena in the United States (https://www.ncdc.noaa.gov/stormevents/faq.jsp). Undercounts of fatalities or missing records from small events could result in biases in this dataset due to resource constraints in reporting.
For cross validation and for interpretation of the regression models, we text-mined the 238 flood fatality events for select causes and variables based on the limited descriptions. After reading event narratives, we mined the text for trends in age, gender and cause of death. For the gender of the fatalities, the words “woman”, “girl”, “mother” or “lady” were used to determine if there was a female involved in the fatality; “man”, “boy”, “son”, and “father” were used to determine if a male was involved; “child”, “baby”, “daughter”, “son”, “boy”, and “girl” were used to determine if there was a young person involved; “elderly” or “senior” were used to determine if there was an elderly person involved; “mobile” and “RV” were used to search to mobile home deaths; “truck”, “car”, and “vehicle” were used to determine if a car was involved; and “drown*” (to cover “drown”, “drowned”, and “drowning”) were used to search for drowning fatalities. Note that not all event narratives have words that indicate gender, age or cause of death, so this represents patterns in types and causes of death, and not a comprehensive characterization. The number of cases with the presence or absence of each word was added and used to calculate the percentage of cases where these words appeared, in order to gain a sense of the demographic factors in the fatality descriptions.
We analyzed property damage data from SHELDUS, reported at the county scale (n = 11,245 events with damage data). A total of USD 24 billion in losses was recorded, with a mean of USD 2.06 million in damage per event per county, and a median of USD 200,000. Unlike fatality data, where the NCEI data report deaths across several counties, SHELDUS splits the damage data equally across each county affected. These data have a large uncertainty and are characterized as “guesstimates” in the SHELDUS metadata. Property damage data had values greater than 0 for almost all flood events; only 408 had a value of “0”. Storm data preparers reporting to the government might use the US Army Corps of Engineers, newspapers, utility companies, insurance adjuster data or other information to estimate monetary damage. Damage includes both private property and public infrastructure. Crop damage amounts are reported separately and are not used in this analysis. Property damage data have been used in vulnerability validation assessments [49]. Other analyses have shown inaccuracies in these data, however, particularly concerning the fact that small or moderate damage is often underreported, and counties vary in what they count as “damage”, leading to inaccuracies of up to 40% in estimates [119]. These issues notwithstanding, they remain the best publicly available property damage estimate datasets at a country scale. Recent studies have obtained insurance adjustment data from FEMA, which likely provides improved private household loss estimates, but those data are not publicly available at the time of this study [120]. We considered using the FEMA Public Assistance data [121] federally declared disaster events (n = 351). These property damage estimates are considered to be of higher quality, and have been used in other vulnerability validation studies [34]. However, due to its much smaller sample size, it was not used in this analysis. We normalized property damages by the estimated total housing value in each county in the 2010 US Census. Our normalization approach is similar to studies which have used the ratio of property losses to total value [34] or added a capital stock variable (multiplying income times population) as a control in regression [49]. We recognize the limits of using property data to validate the economic outcomes of flood hazards, because they only represent direct loss and not long-term business and employment loss.

2.1.2. Flood Hazard Magnitude and Built Environment Data

We accounted for riverine and flash flood hazard intensity by using USGS (United States Geologic Service) stream gauge data [122] to calculate the flood return period of each storm event. The NCEI dataset reports a latitude and longitude location of each event, either by the Storm Data preparer entering in the latitude and longitude directly, or by NCEI calculations from a reported location, distance and 16-point compass direction (e.g., 5 miles east-southeast of Atlanta). It was difficult to know which stream gauge best represented the hazard intensity, especially given uncertainty in event coordinates. Our strategy for connecting events to relevant stream gauges was to match event coordinates to the USGS Watershed Boundary Dataset using HUC (Hydrologic Unit Maps) levels 4, 6, 8, 10 and 12. Each HUC level is a different-sized watershed at nested levels of spatial aggregation; level 12 watersheds are small subwatersheds (the smallest size we used), 10 digit are watersheds, 8 digit are subbasin, 6 digit are basins and 4 digit are subregions (the largest size we used). We then selected all stream gauges in all HUCs that overlapped the storm event point, and gathered all stream gauge readings in between the start and end of the flood event as reported by SHELDUS. We selected the maximum instantaneous discharge reading across all HUC levels and days during the event. We assume the maximum discharge represents peak hazard intensity and would provide the best control for the regression. In order to compare hazard intensity for different events, discharge was converted into flood return times using USGS Stream Stats [123]. This method interpolates discharge data using a log-linear model to develop a continuous curve. We matched the flood event discharge data to its location on the Stream Stats curve to estimate the flood return period of the storm event.
We included data on impervious surface, which has been found to increase property damage associated with flood events [124]. We controlled for built environment by including percent of developed impervious surface by county from the National Land Cover Dataset for 2011 [125].

2.1.3. Social Vulnerability Data

Predictor variables are available through the US Decennial Census (2010) and the American Community Survey (ACS). We used all 29 individual predictor variables used in the 2006–2010 version of the Social Vulnerability Index (SOVI) (Cutter et al. 2003), plus two additional variables consistent with the literature that increased propensity for fatalities or damages during a flood event (percent rural [86] and interactions of race and class [94]) (Table 2). The SoVI indicator was purchased from the University of South Carolina (2006–2010 version), at the county scale [118]. The spatial unit of analysis is the county or county-equivalent. Broad-scale geographic effects were controlled for by including US Census regional and division designations as dummy variables for models. All continuous variables, including property damage, social factors, impervious surface and hazard intensity data were converted to Z-scores with a mean of zero and standard deviation of one.

2.2. Regression Models

We used regressions on fatality and property damage to test which individual socioeconomic factors, SoVI index values, and biophysical factors (flood intensity and impervious surface) significantly influenced each outcome. We treated fatalities per flood event per county as count data. We use a zero-inflated model (Equation (1)) to relate socio-demographic data to flood fatalities, because there may be one process predicting if any flood fatalities occur (e.g., flood hazard intensity above a certain threshold) and a second process that predicts the number of fatalities (j), if a fatality does occur (e.g., social vulnerability factors). Zero-inflated models were implemented with R package ‘pscl’ [126]. We controlled for fatality exposure (in this case, larger populations that would increase the likelihood one person would die) with an offset (logged population of each county). Count data are often modeled with the Poisson distribution, unless there is over dispersion (variance of fatality count is much higher than the mean of counts). We used the Pearson Chi-squared dispersion test and found over dispersion using a Poisson distribution (using the msme package; [127]). We thus used the negative binomial distribution, recommended for zero-inflated models with overdispersed count data.
P r ( y i t = j ) = { π i + ( 1 π i ) g ( y i t = 0 )   i f   j = 0 ( 1 π i ) g ( y i t )   i f   j > 0
y i   = the dependent variable (fatalities) per spatial unit (i), counties for each event (t)
π i = logistic link function, λ i 1 + λ i
g = the negative binomial distribution
λ i = e x p   ( β x i + β x t )
β x i   = coefficients for the time invariant independent variables for each county, i
β x t = coefficients for the time varying independent variables for each event, t, such as hazard intensity or presence of a flash flood.
For property models we used an ordinary least squared (OLS) regression as specified in Equation (2).
Y i =   α + B 1 x t + B 1 x i   B n x i + ε i t
α is the intercept.
B n x i is the coefficient for each independent variable for each county i.
B n x t are the coefficients for time-varying independent variables for each event, t, such as hazard intensity or presence of a flash flood.
ε i t is the error term for each event (t) per county (i).
AIC is used to compare model fits [128] for fatality models. AIC (−2(log likelihood) + 2K, where K = number of model parameters) is the Akaike Information Criterion [129], which is used in non-linear models (e.g., when maximum likelihood estimation is used for model fits, which is used for the zero-inflated models in this study) to compare relative model fits. Lower AIC indicates lower out of sample prediction error and a better relative model. AIC numeric values have no range and cannot be interpreted on their own, as the AIC calculation includes constants related to sample size. AIC values for models with the same outcome variable and sample size can be compared relative to each other. Absolute differences between models if AIC > 10 indicate that the two models offer substantially different evidence, and models with lower AIC have better fits. We used percent deviance explained (nulldeviance–modeldeviance)/nulldeviance where deviance = −2(loglikelihood)) [130] to compare the a priori or null model. In this case, the null hypothesis and model is that social vulnerability does not explain any variance in flood outcomes; models 1 and 2 in Table 3, which was compared to models that include sociodemographic or social vulnerability indices. The relative contribution of social factors predicting death above and beyond biophysical factors was quantified via deviance explained.
R2 (coefficient of determination) was used to compare model fit for property models, and varies between 0 and 1, with higher values explaining a higher proportion of variance (and a better model). Unlike AIC numeric values, R2 values can be interpreted as a ratio of variation that the independent variables explain with respect to the dependent variable. The contribution of social factors predicting damage above and beyond biophysical factors was quantified by directly comparing R2 values. Regressions using observations from spatial data, such as US counties, can be influenced by spatial autocorrelation, meaning the county observations are not independent observations. If the model residuals from a regression are spatially clustered beyond random chance, it indicates a lack of independence and violates the regression assumptions. Standard regression estimates cannot be trusted when spatial autocorrelation is present, because some variables could have inflated the coefficient values, invalidating the tests of significance. We tested for spatial autocorrelation for neighboring counties using queen contiguity (for both the mean and maximum residuals per county, since there are multiple observations for many counties) for both property and damage models using Moran’s I. Moran’s I is a measure of spatial clustering, assessing the difference between a mean value in a sample, and the relative difference in values of a given observation in the sample with its spatial neighbors from the spdep package (version 1.1-3, [131]). If the spatial clustering of regression residuals is greater than random chance, spatial autocorrelation could inflate model coefficients and significance tests. If the p value for the Moran’s I is significant, it indicates spatial autocorrelation is present, the model residuals are clustered beyond random chance, and the correlation coefficients could be artificially inflated.

2.3. Variable Selection and Model Construction

Our approach differs from previous flood studies, which regress disaster outcomes on constructed social vulnerability indices or the combined components of socioeconomic data (e.g., expert weighting, principal component analysis or other statistical transformations termed “vulnerability profiles”). Social vulnerability indices are very sensitive to weighting or combination schemes [132]. Therefore, we take a different approach, and examine individual socioeconomic components of vulnerability to identify which significantly predict hazard outcomes. The aim of our model’s strategy was to identify social factors that systematically increase property damage or fatalities across the USA. We compare models constructed using theory (e.g., including variables identified from the literature, discussed above) versus data mining (e.g., machine learning) to identify factors increasing death and damage. We used a machine learning-generalized boosted regression (Gbm) [133] algorithm to estimate the relative importance of the social variables from Table 2 to death and damage events, respectively. We added dummy variables at both regional and division census levels to control for geographic differences in fatality and flood outcomes. We ensured no models included variables that were significantly correlated (>0.55) to prevent multicollinearity, and also calculated variable inflation coefficients to ensure none were greater than 5 [134]. Variable inflation coefficients indicate multi-collinearity in a model, e.g., when the possibility any single variable could be false is inflated by a correlated relationship with another variable in the model. Significance tests (for p values) are unreliable in models with high variable inflation coefficients, and cannot be used for hypothesis testing.
We constructed six types of models to answer our research questions (Table 3). Model 1 is the null model of fatality and property damage. Model 2 contains only the biophysical variables of flood return time, impervious surface and flash floods, while model 3 adds the SoVI index, and both are regressed against both flood fatalities and property damage. Models 4a, 4b and 4c were theoretically informed models for predicting fatalities, controlling for hazard intensity (4a), regional effects (4b) and division effects (4c). Social factors theoretically predicting death include gender, percent Black, percent rural, age (% < 5 years and % > 65 years), mobile homes, poverty, owning a car, factors that could make heeding early warning difficult (difficulty understanding English, ambulatory difficulty, low education) and health (hospitals, health insurance). Social factors theoretically predicting damage include minoritized populations (%Black, %Native American, %Hispanic, %Asian), housing stock and ownership, mobile homes, renters, people per unit, vacancies and and poverty (correlated with per capital income, which was discarded). Median house value was correlated with households making over USD 200,000, median rent and per capital income, variables which we excluded. Female heads of house theoretically are vulnerable to more flood damage, but this variable was correlated with %Black, so it was not included. Percent impervious is also not included in social models, as it is significantly correlated with percent rural (Pearson Correlation = −0.54, p < 0.001). Models 6a,6b, 6c and 6d were theoretically informed models to estimate property damage, controlling for hazard intensity (6a), regional effects (6b), division effects (6c), and interacting race and class (6d). Models 5a, 5b and 5c include variables identified through machine learning associated with fatalities as count data (5a), fatalities as binary (5b), and property damage.

2.4. Predictive Maps

Our final research question aims to identify which counties are most vulnerable to riverine flood fatalities and relative property damage for a large event. We use the best fitting models (based on AIC or R2) to predict the number of fatalities and property damage ratio for an infrequent and large flood event. To make predictions, we set the population in each county to 100,000, so the predicted death count can be interpreted as a fatality rate per 100,000 people. We assume a flood return time of 500 years, which is the largest flood time we can estimate using the Stream Stats model. Property damage is predicted as the ratio of damage. The top 10 counties for predicted fatalities and property damage are listed in Table 7, together with their percentile in the SoVI index (higher percentile = higher social vulnerability, ranging from 0 to 1). A bivariate choropleth map visualizes the predictions from the zero-inflated fatality model and the property damage model. This map uses Fishers’ classification to define breaks in the data that display optimal variation in a choropleth map with three classes for each variable, for a total of nine classes. We use Spearmen’s rank correlation to compare how the counties most at risk of flood death and property damage compare to high social vulnerability counties identified by the 2006–2010 SoVI index.

3. Results

3.1. Fatalities

Results from textual analysis of the Storm Events Database indicate that the typical flood fatality involves a drowning incident in a car, commonly a man alone, but sometimes involving mothers and children, while crossing a river in a rural area of the country. While not all narratives contained information on gender and age of the people who died, more than 50% of the cases involve men drowning in cars (Figure 1).
Machine learning using fatality counts, as the response revealed that three county-level variables had a relative importance greater than zero (in order of importance): percent rural (85.9%), percent of that population speaking no English (9.67%), and percent Asian (4.44%). These three variables form model 5a (Table 3). Using a binary variable for fatalities (e.g., presence or absence of a death in a flood event) as the response, the machine learning identified 10 variables with a relative importance greater than zero (Table 4). These 10 variables form model 5b (Table 3).
The regression analysis of fatalities indicates that model fit is lowest for models that only include biophysical variables (Model 2, AIC = 2894, Table 5). Model fit increases when SoVI is added (Model 3, AIC = 2829), but performs better when adding the individual social components identified in the literature (Model 4a, AIC = 2732) and geographic controls (Model4c, AIC = 2696). Models constructed with the social factors identified in machine learning do not perform as well as models constructed with theory (Model 5a and Model 5b AIC = 2728 and 2744, respectively). Higher flood magnitude is consistently a significant predictor for increased death counts across all models (p < 0.01), while flash floods in particular were not found to be associated with increased death counts. Residuals were significantly spatially autocorrelated for death model residuals (Moran’s I = 0.282, p < 0.001). However, methods for implementing spatial weights for zero-inflated regression with a negative binomial distribution were not available at the time this paper was written (for a zero-inflated geographically weighted regression with a Poisson distribution, see the lctools package from [135]). Spatial autocorrelation urges caution in model interpretation, as the model fit and coefficient estimates could be overestimated. We only interpret variables as significant that are p < 0.05, and not those that are 0.5 < p < 0.1, due to the potential inflation of coefficient estimates, induced by spatial autocorrelation.
Three social variables have significant and positive coefficients across all model formulations: percent rural, percent of the population under 5 years old, and percent of the population over 65 years old. These three characteristics were also found in the text mining analysis (Figure 1), providing additional validation. Rural percent of the county population is the strongest predictor of death count across all models (p < 0.01). Two of the eight regional division variables, both in the southern US (west south central and east south central), have a significant effect in increasing death counts (model 4c: p < 0.01, p < 0.01, respectively). Counties with higher proportions of younger (<5 years) and elderly populations are correlated with higher flood death counts (p < 0.01). Other variables are inconsistent across models. For example, counties with a lower percentage of health insurance coverage for the population are positively correlated with death counts in models 4a (p < 0.05) and 4b (p < 0.1), but when geographic division controls are added, this significant effect disappears.

3.2. Property Damage

Property damage models reveal trends similar to fatality models (Table 6). Models using only biophysical variables are correlated with a small amount of variation in property damage ratios (Model 2, R2 = 0.09). Variation explained increases with models adding SoVI, which is significantly correlated with damage ratios (Model 3: R2 = 0.13, p < 0.01). Models with social factors selected from both the literature and machine learning explained more variation compared to SoVI only models (Models 4a, 4b, and 5c: R2 = 0.20 for each). The best performing model includes race and poverty interactions and geographic divisions (Model 5d: R2 = 0.23). Flood magnitude is significantly and positive correlated, and larger floods increase damage across all models (p < 0.01). We did not find spatial autocorrelation in residuals for property damage models (Moran’s I = 0.0007, p = 0.28)
Five social factors significantly increase property damage ratios across all models. Damage is higher in rural counties, and in counties with lower median house values, lower housing density (people per home), higher percentages of population below the poverty line, and in counties with lower percentages of Asian populations across all models (p < 0.01). Counties with higher Native American populations experience higher property damage ratios across two models (6a and 6b: p < 0.05). An interaction between the percent of Native Americans and people below the poverty line is also significant (model 6d: p < 0.001). In the best-performing model (6d), race and class interactions reveal that property damage increases particularly in locations with more poor Black, Hispanic and Native American populations, but decreases in counties with more Asian populations below the poverty line (p < 0.01 for all interactions). These results suggest that high damage ratios are concentrated in counties with populations with higher poverty rates and minoritized populations. Geographic location is a significant predictor of property damage in seven of the eight census divisions tested. Damage is significantly higher for the west south central (p < 0.01), middle Atlantic (p < 0.05) and New England (p < 0.01), western Pacific (p < 0.01) and western central Midwest (p < 0.05), and lower for the eastern central Midwest and south Atlantic division (p < 0.05 for both).

3.3. Social versus Biophysical Influence Explaining Variation in Death and Damage

Social factors increase model performance and add significant predictability to flood death (Figure 2A) and damage in the US. Deviance explained from death count models is smaller in models with only biophysical variables (model 2, 0.014), and deviance explained increases when adding SoVI (model 3, 0.037), individual social factors identified in machine learning (model 5a, 0.072), social variables identified in the literature (model 4a, 0.076 and model 4c, 0.091). Variance explained in property damaged increased from just 9% in a biophysical model (model 2) to over 23% when social and geographic factors were added to the model (model 6d) (Figure 2B).

3.4. Predicted Spatial Distribution of Death and Damage in a 500-Year Flood Event

The best-performing models for flood fatalities (Model 4c, social vulnerability variables selected from the literature including geographic controls) and damage (Model 6d, social vulnerability variables selected from the literature including geographic control) were used to predict death and damage across the USA for a hypothetical 500-year flood (Figure 3). Results show that in a large flood event, property damages occur across a wide portion of the USA, and are highest across the south east, southwest, Midwest, and in the northern portion of New England. Deaths are highest in the Appalachian region, and in the south-central portions of the US and Plains states, and coincide with high property damage ratios. Only in portions of Utah are there regions with predicted higher deaths but not property damage. Counties with predicted higher death and damage are significantly correlated (Spearman’s Rank Correlation = 0.79, p < 0.001). Counties with higher predicted damage are more correlated with counties with high SoVI (Spearman’s Rank Correlation = 0.63, p < 0.001) than counties with predicted fatalities (Spearman’s Rank Correlation = 0.42, p < 0.001). This suggests SoVI is more predictive of the spatial distribution of counties with higher flood damage relative to local property values than the spatial distribution of flood fatality. The top 10 counties for predicted death and damage do not share any counties (Table 7), but the top three counties for predicted damage also coincide with some of the high SoVI counties (Todd and Shannon, SD and Sioux, ND).

4. Discussion

Results provide strong support that social vulnerability is correlated with higher death and damage in non-coastal flood events in the US. In general, we found that models including social factors explain about twice as much variation in flood outcomes for death and damage as models including only flood magnitude, flood type and impervious surface. The main variable associated with outsized death and property damage as a proportion of total property value is rurality, which is related to other factors of high social vulnerability. The models of damage and death count both improved significantly in variation or deviance explained when they included SoVI, a composite indicator of social vulnerability. This finding is consistent with previous validation studies, which find that SoVI is correlated with property damage [34,49]. Our study is the first validation of SoVI in relation to flood events across the US. However, the explained variance and deviance of both death and damage continued to increase when specific demographic variables, selected via machine learning or literature review, were added to the models (Figure 2, Table 5). Previous research on Hurricane Sandy likewise found that models constructed with specific components of social vulnerability (termed vulnerability profiles, Rufat et al. [34]) offered higher predictability for distinct flood outcomes than a general index like the SoVI. We found that in addition to general social vulnerability (from the SoVI), rural counties and counties in the central southwestern US have a higher propensity for losses of both lives and property. However, other specific components of vulnerability are related to distinct death versus property loss outcomes.

4.1. Flood Fatalities

Consistent with the previous literature, the model results indicate that counties with more elderly and young populations, as well as rural locations, are related to higher flood fatalities. Quantitative and qualitative studies have found that very old and very young populations are more likely to die in a flood event either from drowning or complications related to medical access post-event [67,72,73,74,75]. Rural locations also have an older age distribution in the USA [136], although when including rurality and percent elderly in a county, the same model did not cause multi-collinearity (based on variable inflation coefficient tests). While rurality and age are likely related to higher levels of flood deaths, causation cannot be ascribed from the correlative results presented here.
We found SoVI was positively and significantly associated with flood death counts, contrary to a previous study which did not find SoVI to be a significant factor of flood death across multiple hazards across southeastern States [49]. Bakkensen et al. [49] did not use a direct measure of flood magnitude to control for hazards. Contrary to previous work (e.g., Zahran et al. [79]), we found neither race nor poverty to be significantly correlated with flood deaths. Our sample size, however, did not include significant events such as Hurricane Katrina (2005) and Hurricane Audrey (1957), which indicated that Black populations had higher propensities for flood death [77,78]. Our nation-wide study found regional patterns of flood death in Appalachia, the Ohio River Valley, and in South Central Texas, consistent with previous studies [71,79]. Our models include riverine and flash flood events only, and should not be generalized to coastal flood events. Flood fatalities (for flash floods in particular) could occur in hillslope regions with extreme rainfall patterns, and could be related to other factors not controlled for in this study. Efforts to reduce flood deaths in these locations could include better early warning and near real-time warning systems, especially to indicate evacuation routes on safe roads, since most deaths involved driving in a car. Installing sensors on road crossings where flash floods tend to occur, or where flood deaths have occurred in the past, to alert drivers of dangerous crossings could also be effective.

4.2. Property Damage

Consistent with previous studies, we found SoVI and poverty to be significantly correlated with flood damage [34,49]. Other studies, such as that of Yoon et al. [19], using absolute property damage across multiple hazard types in coastal areas from 1990 to 2010, found urban areas and high ratios of female population to be correlated with property loss. Their results could contradict ours due to differences in spatial extent, temporal extent, and most likely normalization of the dependent variables (our regressions are on property damage ratios, theirs are absolute loss estimates, which one would expect to be very high in urban areas). The significant social factors in the best-performing model indicate that rural areas, and the interaction of race and poverty, have the largest influence on property damage. The most striking result from our models was the significant role of some races (Black, Native American and Hispanic) and poverty in predicting property damage ratios. Previous qualitative research has found, for example, that it is not Black communities generally that suffered greatest property losses in Hurricane Katrina, but low-income Black communities specifically [94]. We found the interaction of poverty and Asian populations to be negative, suggesting regions with poor Asian communities experience less property loss in riverine floods than other populations.
Our results indicate that the influences of poverty–race interactions associated with greater property losses extend beyond Hurricane Katrina, and could be a generalizable phenomenon across the contiguous US, validated by empirical data for over 11,000 riverine events. Other studies of quantitative hazard outcomes have also found significant race interactions; populations census blocks with tornado events in the US from 1980 to 2010 across 25 states became more White and had lower rates of poverty post-hazard, suggesting out-migration by poor and non-White populations [64]. The high propensity for flood-related property loss in poor communities of color could be due to increased flood exposure (due to limited housing choices and more accessible housing in floodplains), poor housing quality, structural racism (e.g., systematic underinvestment in flood mitigation structures such as levees), or institutional racism and bias (e.g., low flood insurance coverage (7%) in Native American communities, because FEMA was not mapping them, a prerequisite for the National Flood Insurance Program [103]). While flood insurance can create moral hazards and increase vulnerability [137], other studies find that payouts from insurance are less likely to reach socially vulnerability communities [65]. Investments in flood mitigation infrastructure, improved zoning, opportunities for buyout and relocation [138], disaster recovery from public programs [65], and financial support for risk transfer mechanisms such as insurance should be targeted towards poor communities of color—Black, Hispanic and Native American specifically—to address this gap.

4.3. Spatial Distribution of Death and Damage and Model Limitations

Our model results indicate significant geographic variation in riverine flood death and damage. Figure 3 suggests specific regions are susceptible to riverine flood outcomes, and the interaction of death and damage. Previous flood research has found that flood exposure trends also exhibit geographic hotspots over the contiguous US [104]. Some of the hotspots of increasing flood exposure due to urbanization in floodplains found in previous studies, for example in Appalachia and along the Ohio River, are the same regions where our model finds coincident high propensities for death and damage in a predicted 500-year riverine flood event (Figure 3). Spatial autocorrelation in flood death models suggests the results presented here may not provide a robust validation of social vulnerability to riverine flood deaths. Developing geographically weighted zero-inflated regression models with negative binomial distributions will be required to provide robust validation of social vulnerability and specific socio-demographic factors for flood death in the US. Subsequent research could extend this study by developing geographically weighted models to explore how social factors at different scales significantly predict death and damage, or vary across the country. We only assessed non-coastal flood events from 2008 to 2012, two years before and after the 2010 census. Efforts to integrate flood events near the 2000 census, and the upcoming 2020 census, could both increase the sample and permit the examination of potential changes in social vulnerability to floods over time.
We only assess aggregate property damage at the county level in this study for non-coastal floods from 2008 to 2012. Future work could compare flood damage directly from FEMA public assistance data or insurance claims, to examine if factors identified in this study prediction flood damage ratios differ in homeowner loss-specific datasets. Vulnerability and resilience to hazards in the US may also change over time [28], and we encourage future studies to empirically validate vulnerability across time to test this hypothesis. Social vulnerability is also likely to change in the future, which can be modeled to improve the understanding of how climate hazards such as sea-level rise may disproportionally expose vulnerable communities [139].
The hazard controls related to flood magnitude from stream gauges are an improvement over past studies, which used precipitation [79] or NCEI intensity scores [49]. Stream gauges represent one point on a river and are an imperfect measure of flood hazard across the county-watershed units used here. Direct measures of spatially explicit flood extent or depth per hazard (as used by Rufat et al. [34]) for each flood hazard in the Storm Events database would be the preferred control variables, but these were unavailable at the time of this study. We exclude all coastal flood events, which likely represent an even larger number of flood deaths and flood damages. Future flood social vulnerability validation studies should seek to integrate and compare differences across riverine, flash and coastal flood events.
An important qualification of our results is that social factors were aggregated at the county level, and variations in flood outcomes at the household level are excluded at this unit of analysis. This means that the relationships described in this study here apply at broad geographic scales, but different relationships may apply at more local scales or at the individual level. A county level analysis of flood fatalities, for example, does not completely control for the excess flood exposure in counties where populations are more concentrated along a river or on floodplains. Other modeling techniques, such as hierarchical or spatio-temporal Bayesian analysis, are increasingly common in epidemiology [140] and natural sciences [141], but to our knowledge these are not yet used in social vulnerability analysis (but there is an example of a resilience assessment based on a Bayesian network [142]). Bayesian methods should be used to test the hypotheses examined here, and will allow for uncertainty analysis in order to better understand the strength of relationships between sociodemographic variables and hazard outcomes. Other important components of social vulnerability, including social cohesion, social capital and risk perception [23] identified in place-based and qualitative studies, are difficult to meaningfully measure at county scales, but their validation across large geospatial scales remains important.

4.4. Further Research Needs

This study adds to a small but growing number of social vulnerability validation studies, further identifying specific social factors that lead to higher propensities for loss in hazard events. While we found indices like SoVI to be correlated with flood death and damage outcomes at the county scale, digging deeper into specific social factors revealed that some, but not all, SoVI components are significant predictors of riverine flood death and damage. Recent studies [34] have suggested validating constructed vulnerability profiles of related social factors as a way forward. We confirm their recommendation that more social vulnerability validation is needed across a wider array of spatial and temporal scales, since the scale and accuracy of both the flood hazard and social vulnerability variables critically affect findings [143]. Socioeconomic and demographic factors at the household, community and larger scales need to be tested in additional multi-scale validation studies, in order to understand how gender, for example, may increase risk of death in a non-coastal flood at a household but not at county scales. Social vulnerability validation across hazards is necessary in order to direct policy interventions to address floods, heat waves and tornados to the populations and places that need them most. Knowing, for example, that people above the age of 65 are more at risk of death from a non-coastal flood may enable policy makers to identify those populations in advance, for early evacuation before floods occur, or to reinforce riverine flood protections near long term care facilities. SoVI scores may serve as a general guide of vulnerability, but hazard-specific models are likely to yield more specific and useful policy recommendations. Finally, social vulnerability validation across phases of the disaster cycle is needed. For example, while populations with young age distributions may have greater propensities for flood death in a hazard event, they might also have higher rates of recovery if children are more psychologically resilient to hazards in the recovery phase [75].

5. Conclusions

Overall, the methods explored in this study indicate that the hazards-of-place model [5], which has inspired decades of research into the social conditions that influence the vulnerability of people-in-place to specific hazards, can be extended by building empirically validated social vulnerability models of hazard-specific disaster outcomes. In this case, sensitivities to non-coastal flood events regarding mortality and economic damage are validated for the 48 contiguous United States using the 2010 census. The results support some of the vulnerability factors identified in past research, including county-level measures of racial/ethnic composition, poverty, the elderly and young population, and rural location. Other factors identified in past research were not related to flood impacts in our analysis, including gender and mobile home prevalence.
The data-driven validation method presented here to assess vulnerability could also be used to validate commonly used indicators of resilience or coping capacity, which also suffer from inadequate validation. Validation not only identifies factors to which disaster mitigation policies should pay attention, but also allows for a more systematic study of changes in social vulnerability over space and time. A place-based yet broad-scale understanding of validated factors leading to social vulnerability is crucial, as urbanization and climate change influence and change the rate, intensity and location of hazards across the globe.

Author Contributions

Conceptualization, P.H. and A.d.S.; Data curation, C.S.; Formal analysis, B.T.; Funding acquisition, B.S.; Investigation, B.T.; Methodology, C.S. and P.D.H.; Project administration, B.T.; Visualization, B.T.; Writing: original draft, B.T. and C.S.; Writing: review and editing, B.T., A.d.S., P.D.H. and B.D. All authors have read and agreed to the published version of the manuscript.

Funding

This research was partially funded by a Google Earth Engine Research Award, and The Utah State University.

Acknowledgments

Thanks to the Cloud to Street team and B.L. Turner II for comments on earlier versions of this manuscript, for Cole Erikson with responses to reviewers regarding use of the term institutional racism, and for James Doss-Gollin and Carolynne Hultquist for their comments. The manuscript also benefited from the reviews of four anonymous reviewers. A.d.S acknowledges support under NASA contract NNG13HQ04C for the continued operation of the Socioeconomic Data and Applications Center (SEDAC).

Conflicts of Interest

Author declare no conflict of interest.

Data Availability

Data from 500-year return period model prediction for death counts and relative damage form regression models are available at: https://github.com/cloudtostreet/socialvulnerability. Contact the lead author for copies of r code, models or additional data which is available upon request.

References

  1. Burton, I. The Environment as Hazard; Guilford Press: New York, NY, USA, 1993; ISBN 0-89862-159-3. [Google Scholar]
  2. Kates, R.W.; Burton, I. Gilbert F. White, 1911–2006 Local Legacies, National Achievements, and Global Visions. Ann. Assoc. Am. Geogr. 2008, 98, 479–486. [Google Scholar] [CrossRef]
  3. Watts, M. On the poverty of theory: Natural hazards research in context. In Interpretations of Calamity from the Viewpoint of Human Ecology; Hewitt, K., Ed.; Allen & Unwin: Boston, MA, USA, 1983; pp. 231–262. [Google Scholar]
  4. Blaikie, P.; Terry, C.; Ian, D.; Ben, W. At Risk: Natural Hazards, People’s Vulnerability, and Disasters. Hum. Ecol. 1996, 24, 141–145. [Google Scholar] [CrossRef]
  5. Cutter, S.L. Vulnerability to environmental hazards. Prog. Hum. Geogr. 1996, 20, 529–539. [Google Scholar] [CrossRef]
  6. Turner, B.L.; Kasperson, R.E.; Matson, P.A.; McCarthy, J.J.; Corell, R.W.; Christensen, L.; Eckley, N.; Kasperson, J.X.; Luers, A.; Martello, M.L.; et al. A framework for vulnerability analysis in sustainability science. Proc. Natl. Acad. Sci. USA 2003, 100, 8074–8079. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  7. White, G.F. Natural Hazards, Local, National, Global; Oxford University Press: Oxford, UK, 1974. [Google Scholar]
  8. Adger, W.N. Vulnerability. Glob. Environ. Chang. 2006, 16, 268–281. [Google Scholar] [CrossRef]
  9. Birkmann, J.; Wisner, B. Measuring the Unmeasurable: The Challenge of Vulnerability; UNU-EHS: Bonn, Germany, 2006; ISBN 3-9810582-6-7. [Google Scholar]
  10. Eakin, H.; Luers, A.L. Assessing the Vulnerability of Social-Environmental Systems. Annu. Rev. Environ. Resour. 2006, 31, 365–394. [Google Scholar] [CrossRef] [Green Version]
  11. Eriksen, S.H.; Kelly, P.M. Developing Credible Vulnerability Indicators for Climate Adaptation Policy Assessment. Mitig. Adapt. Strateg. Glob. Chang. 2007, 12, 495–524. [Google Scholar] [CrossRef]
  12. IPCC Climate Change 2014—Impacts, Adaptation and Vulnerability: Regional Aspects; Cambridge University Press: Cambridge, UK, 2014.
  13. Smit, B.; Wandel, J. Adaptation, adaptive capacity, and vulnerability. Glob. Environ. Chang. 2006, 16, 282–292. [Google Scholar] [CrossRef]
  14. Ford, J.D.; Smit, B. A Framework for Assessing the Vulnerability of Communities in the Canadian Arctic to Risks Associated with Climate Change. ARCTIC 2004, 57, 389–400. [Google Scholar] [CrossRef]
  15. Younus, M.; Kabir, M. Climate Change Vulnerability Assessment and Adaptation of Bangladesh: Mechanisms, Notions and Solutions. Sustainability 2018, 10, 4286. [Google Scholar] [CrossRef] [Green Version]
  16. Mustafa, D. The Production of an Urban Hazardscape in Pakistan: Modernity, Vulnerability, and the Range of Choice. Ann. Assoc. Am. Geogr. 2005, 95, 566–586. [Google Scholar] [CrossRef]
  17. Turner, B.L.; Matson, P.A.; McCarthy, J.J.; Corell, R.W.; Christensen, L.; Eckley, N.; Hovelsrud-Broda, G.K.; Kasperson, J.X.; Kasperson, R.E.; Luers, A.; et al. Illustrating the coupled human-environment system for vulnerability analysis: Three case studies. Proc. Natl. Acad. Sci. USA 2003, 100, 8080–8085. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  18. Schoon, M.; Fabricius, C.; Anderies, J.M.; Nelson, M. Synthesis: Vulnerability, traps, and transformations—long-term perspectives from archaeology. Ecol. Soc. 2011, 16, 24. [Google Scholar] [CrossRef] [Green Version]
  19. Yoon, D.K. Assessment of social vulnerability to natural disasters: A comparative study. Nat. Hazards 2012, 63, 823–843. [Google Scholar] [CrossRef]
  20. O’Brien, K.; Sygna, L.; Haugen, J.E. Vulnerable or Resilient? A Multi-Scale Assessment of Climate Impacts and Vulnerability in Norway. Clim. Chang. 2004, 64, 193–225. [Google Scholar] [CrossRef]
  21. Younus, M.A.F. An assessment of vulnerability and adaptation to cyclones through impact assessment guidelines: A bottom-up case study from Bangladesh coast. Nat. Hazards 2017, 89, 1437–1459. [Google Scholar] [CrossRef]
  22. Younus, M.A.F.; Harvey, N. Community-based flood vulnerability and adaptation assessment: A case study from Bangladesh. J. Environ. Assess. Policy Manag. 2013, 15, 1350010. [Google Scholar] [CrossRef]
  23. Rickless, D.S.; Yao, X.A.; Orland, B.; Welch-Devine, M. Assessing Social Vulnerability through a Local Lens: An Integrated Geovisual Approach. Ann. Am. Assoc. Geogr. 2020, 110, 36–55. [Google Scholar] [CrossRef]
  24. Tanim, S.H.; Tobin, G.A. Social Factors and Evacuation Vulnerability: An Application in Pinellas County, Florida. Pap. Appl. Geogr. 2018, 4, 123–136. [Google Scholar] [CrossRef]
  25. Shao, W.; Jackson, N.P.; Ha, H.; Winemiller, T. Assessing community vulnerability to floods and hurricanes along the Gulf Coast of the United States. Disasters 2020, 44, 518–547. [Google Scholar] [CrossRef]
  26. Cutter, S.L.; Boruff, B.J.; Shirley, W.L. Social vulnerability to environmental hazards. Soc. Sci. Q. 2003, 84, 242–261. [Google Scholar] [CrossRef]
  27. Gu, H.; Du, S.; Liao, B.; Wen, J.; Wang, C.; Chen, R.; Chen, B. A hierarchical pattern of urban social vulnerability in Shanghai, China and its implications for risk management. Sustain. Cities Soc. 2018, 41, 170–179. [Google Scholar] [CrossRef]
  28. Cutter, S.L.; Finch, C. Temporal and spatial changes in social vulnerability to natural hazards. Proc. Natl. Acad. Sci. USA 2008, 105, 2301–2306. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  29. Federal Emergency Management Agency National Risk Index. Available online: https://nationalriskindex-test.fema.gov/ (accessed on 27 July 2017).
  30. De Sherbinin, A.; Apotsos, A.; Chevrier, J. Mapping the future: Policy applications of climate vulnerability mapping in West Africa. Geogr. J. 2017, 183, 414–425. [Google Scholar] [CrossRef]
  31. Spielman, S.E.; Tuccillo, J.; Folch, D.C.; Schweikert, A.; Davies, R.; Wood, N.; Tate, E. Evaluating social vulnerability indicators: Criteria and their application to the Social Vulnerability Index. Nat. Hazards 2020, 100, 417–436. [Google Scholar] [CrossRef] [Green Version]
  32. Tate, E. Social vulnerability indices: A comparative assessment using uncertainty and sensitivity analysis. Nat. Hazards 2012, 63, 325–347. [Google Scholar] [CrossRef]
  33. Tate, E. Uncertainty Analysis for a Social Vulnerability Index. Ann. Assoc. Am. Geogr. 2013, 103, 526–543. [Google Scholar] [CrossRef]
  34. Rufat, S.; Tate, E.; Emrich, C.T.; Antolini, F. How Valid Are Social Vulnerability Models? Ann. Am. Assoc. Geogr. 2019, 109, 1131–1153. [Google Scholar] [CrossRef]
  35. De Sherbinin, A.; Bukvic, A.; Rohat, G.; Gall, M.; McCusker, B.; Preston, B.; Apotsos, A.; Fish, C.; Kienberger, S.; Muhonda, P.; et al. Climate vulnerability mapping: A systematic review and future prospects. Wiley Interdiscip. Rev. Clim. Chang. 2019. [Google Scholar] [CrossRef]
  36. Adger, W.N. Social and ecological resilience: Are they related? Prog. Hum. Geogr. 2000, 24, 347–364. [Google Scholar] [CrossRef]
  37. Adger, W.N.; Huq, S.; Brown, K.; Conway, D.; Hulme, M. Adaptation to climate change in the developing world. Prog. Dev. Stud. 2003, 3, 179–195. [Google Scholar] [CrossRef]
  38. Denevan, W.M. Adaptation, variation, and cultural geography. Prof. Geogr. 1983, 35, 399–407. [Google Scholar] [CrossRef]
  39. Eakin, H. The ‘turn to capacity’ in vulnerability research. In Applied Studies in Climate Adaptation; Palutikof, J.P., Boulter, S.L., Barnett, J., Rissik, D., Eds.; John Wiley & Sons Ltd.: Hoboken, NJ, USA, 2014; pp. 225–230. [Google Scholar]
  40. Holling, C.S. Understanding the complexity of economic, ecological, and social systems. Ecosystems 2001, 4, 390–405. [Google Scholar] [CrossRef]
  41. Kates, R.W.; Travis, W.R.; Wilbanks, T.J. Transformational adaptation when incremental adaptations to climate change are insufficient. Proc. Natl. Acad. Sci. USA 2012, 109, 7156–7161. [Google Scholar] [CrossRef] [Green Version]
  42. Turner, B.L. Vulnerability and resilience: Coalescing or paralleling approaches for sustainability science? Glob. Environ. Chang. 2010, 20, 570–576. [Google Scholar] [CrossRef]
  43. Wise, R.M.; Fazey, I.; Stafford Smith, M.; Park, S.E.; Eakin, H.C.; Archer Van Garderen, E.R.M.; Campbell, B. Reconceptualising adaptation to climate change as part of pathways of change and response. Glob. Environ. Chang. 2014, 28, 325–336. [Google Scholar] [CrossRef] [Green Version]
  44. Fischer, A.P.; Frazier, T.G. Social Vulnerability to Climate Change in Temperate Forest Areas: New Measures of Exposure, Sensitivity, and Adaptive Capacity. Ann. Am. Assoc. Geogr. 2018, 108, 658–678. [Google Scholar] [CrossRef]
  45. Lutz, W.; Muttarak, R.; Striessnig, E. Universal education is key to enhanced climate adaptation. Science 2014, 346, 1061–1062. [Google Scholar] [CrossRef]
  46. Cutter, S.L.; Ahearn, J.A.; Amadei, B.; Crawford, P.; Eide, E.A.; Galloway, G.E.; Goodchild, M.F.; Kunreuther, H.C.; Li-Vollmer, M.; Schoch-Spana, M.; et al. Disaster resilience: A national imperative. Environ. Sci. Policy Sustain. Dev. 2013, 55, 25–29. [Google Scholar] [CrossRef]
  47. Luers, A.L. The surface of vulnerability: An analytical framework for examining environmental change. Glob. Environ. Chang. Part A 2005, 15, 214–223. [Google Scholar] [CrossRef]
  48. Cutter, S.L.; Derakhshan, S. Temporal and spatial change in disaster resilience in US counties, 2010–2015. Environ. Hazards 2020, 19, 10–29. [Google Scholar] [CrossRef]
  49. Bakkensen, L.A.; Fox-Lent, C.; Read, L.K.; Linkov, I. Validating Resilience and Vulnerability Indices in the Context of Natural Disasters: Validating Resilience and Vulnerability Indices. Risk Anal. 2017, 37, 982–1004. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  50. Jongman, B.; Hochrainer-stigler, S.; Feyen, L.; Aerts, J.C.J.H.; Mechler, R.; Botzen, W.J.W.; Bouwer, L.M.; Pflug, G.; Rojas, R.; Ward, P.J. Increasing stress on disaster-risk finance due to large floods. Nat. Clim. Chang. 2014, 4, 1–5. [Google Scholar] [CrossRef]
  51. Jongman, B.; Ward, P.J.; Aerts, J.C.J.H. Global exposure to river and coastal flooding: Long term trends and changes. Glob. Environ. Chang. 2012, 22, 823–835. [Google Scholar] [CrossRef]
  52. Ward, P.J.; Jongman, B.; Weiland, F.S.; Bouwman, A.; van Beek, R.; Bierkens, M.F.P.; Ligtvoet, W.; Winsemius, H.C. Assessing flood risk at the global scale: Model setup, results, and sensitivity. Environ. Res. Lett. 2013, 8, 44019. [Google Scholar] [CrossRef]
  53. Winsemius, H.C.; Van Beek, L.P.H.; Jongman, B.; Ward, P.J.; Bouwman, A. A framework for global river flood risk assessments. Hydrol. Earth Syst. Sci. 2013, 17, 1871–1892. [Google Scholar] [CrossRef] [Green Version]
  54. Smith, A.; Bates, P.D.; Wing, O.; Sampson, C.; Quinn, N.; Neal, J. New estimates of flood exposure in developing countries using high-resolution population data. Nat. Commun. 2019, 10. [Google Scholar] [CrossRef] [Green Version]
  55. Wing, O.E.J.; Bates, P.D.; Smith, A.M.; Sampson, C.C.; Johnson, K.A.; Fargione, J.; Morefield, P. Estimates of present and future flood risk in the conterminous United States. Environ. Res. Lett. 2018, 13, 034023. [Google Scholar] [CrossRef]
  56. Nofal, O.M.; van de Lindt, J.W. Understanding flood risk in the context of community resilience modeling for the built environment: Research needs and trends. Sustain. Resilient Infrastruct. 2020, 1–17. [Google Scholar] [CrossRef]
  57. Mustafa, D. Reinforcing vulnerability? Disaster relief, recovery, and response to the 2001 flood in Rawalpindi, Pakistan. Glob. Environ. Chang. Part B Environ. Hazards 2003, 5, 71–82. [Google Scholar] [CrossRef]
  58. Rufat, S.; Tate, E.; Burton, C.G.; Maroof, A.S. Social vulnerability to floods: Review of case studies and implications for measurement. Int. J. Disaster Risk Reduct. 2015, 14, 470–486. [Google Scholar] [CrossRef] [Green Version]
  59. Azar, D.; Rain, D. Identifying population vulnerable to hydrological hazards in San Juan, Puerto Rico. GeoJournal 2007, 69, 23–43. [Google Scholar] [CrossRef]
  60. Fekete, A. Validation of a social vulnerability index in context to river-floods in Germany. Nat. Hazards Earth Syst. Sci. 2009, 9, 393–403. [Google Scholar] [CrossRef] [Green Version]
  61. Finch, C.; Emrich, C.T.; Cutter, S.L. Disaster disparities and differential recovery in New Orleans. Popul. Environ. 2010, 31, 179–202. [Google Scholar] [CrossRef]
  62. Parry, L.; Davies, G.; Almeida, O.; Frausin, G.; de Moraés, A.; Rivero, S.; Filizola, N.; Torres, P. Social Vulnerability to Climatic Shocks Is Shaped by Urban Accessibility. Ann. Am. Assoc. Geogr. 2018, 108, 125–143. [Google Scholar] [CrossRef] [Green Version]
  63. Younus, M.A.F.; Harvey, N. Economic consequences of failed autonomous adaptation to extreme floods: A case study from Bangladesh. Local Econ. J. Local Econ. Policy Unit 2014, 29, 22–37. [Google Scholar] [CrossRef]
  64. Raker, E.J. Natural Hazards, Disasters, and Demographic Change: The Case of Severe Tornadoes in the United States, 1980–2010. Demography 2020, 57, 653–674. [Google Scholar] [CrossRef]
  65. Emrich, C.T.; Tate, E.; Larson, S.E.; Zhou, Y. Measuring social equity in flood recovery funding. Environ. Hazards 2020, 19, 228–250. [Google Scholar] [CrossRef]
  66. Abbas, H.B.; Routray, J.K. Vulnerability to flood-induced public health risks in Sudan. Disaster Prev. Manag. Int. J. 2014, 23, 395–419. [Google Scholar] [CrossRef]
  67. Alderman, K.; Turner, L.R.; Tong, S. Floods and human health: A systematic review. Environ. Int. 2012, 47, 37–47. [Google Scholar] [CrossRef] [Green Version]
  68. Fothergill, A. Gender, risk, and disaster. Int. J. Mass Emergencies Disasters 1996, 14, 33–56. [Google Scholar]
  69. Neumayer, E.; Plümper, T. The Gendered Nature of Natural Disasters: The Impact of Catastrophic Events on the Gender Gap in Life Expectancy, 1981–2002. Ann. Assoc. Am. Geogr. 2007, 97, 551–566. [Google Scholar] [CrossRef] [Green Version]
  70. Chowdhury, A.M.R.; Bhuyia, A.U.; Choudhury, A.Y.; Sen, R. The Bangladesh cyclone of 1991: Why so many people died. Disasters 1993, 17, 291–304. [Google Scholar] [CrossRef] [PubMed]
  71. Ashley, S.T.; Ashley, W.S. Flood Fatalities in the United States. J. Appl. Meteorol. Climatol. 2008, 47, 805–818. [Google Scholar] [CrossRef]
  72. Jonkman, S.N.; Kelman, I. An analysis of the causes and circumstances of flood disaster deaths. Disasters 2005, 29, 75–97. [Google Scholar] [CrossRef] [PubMed]
  73. Lowe, D.; Ebi, K.; Forsberg, B. Factors Increasing Vulnerability to Health Effects before, during and after Floods. Int. J. Environ. Res. Public. Health 2013, 10, 7015–7067. [Google Scholar] [CrossRef] [PubMed]
  74. Ngo, E.B. When disasters and age collide: Reviewing vulnerability of the elderly. Nat. Hazards Rev. 2001, 2, 80–89. [Google Scholar] [CrossRef]
  75. Peek, L. Children and disasters: Understanding vulnerability, developing capacities, and promoting resilience—An introduction. Child. Youth Environ. 2008, 18, 1–29. [Google Scholar]
  76. Fothergill, A.; Maestas, E.G.; Darlington, J.D. Race, ethnicity and disasters in the United States: A review of the literature. Disasters 1999, 23, 156–173. [Google Scholar] [CrossRef]
  77. Sharkey, P. Survival and Death in New Orleans: An Empirical Look at the Human Impact of Katrina. J. Black Stud. 2007, 37, 482–501. [Google Scholar] [CrossRef]
  78. Brunkard, J.; Namulanda, G.; Ratard, R. Hurricane Katrina Deaths, Louisiana, 2005. Disaster Med. Public Health Prep. 2008, 2, 215–223. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  79. Zahran, S.; Brody, S.D.; Peacock, W.G.; Vedlitz, A.; Grover, H. Social vulnerability and the natural and built environment: A model of flood casualties in Texas. Disasters 2008, 32, 537–560. [Google Scholar] [CrossRef] [PubMed]
  80. Rivera, J.D.; Miller, D.S. Continually Neglected: Situating Natural Disasters in the African American Experience. J. Black Stud. 2007, 37, 502–522. [Google Scholar] [CrossRef]
  81. Jongman, B.; Winsemius, H.C.; Aerts, J.C.J.H.; Coughlan de Perez, E.; van Aalst, M.K.; Kron, W.; Ward, P.J. Declining vulnerability to river floods and the global benefits of adaptation. Proc. Natl. Acad. Sci. USA 2015, 201414439. [Google Scholar] [CrossRef] [Green Version]
  82. Di Baldassarre, G.; Montanari, A.; Lins, H.; Koutsoyiannis, D.; Brandimarte, L.; Blöschl, G. Flood fatalities in Africa: From diagnosis to mitigation: FLOOD FATALITIES IN AFRICA. Geophys. Res. Lett. 2010, 37, 1–5. [Google Scholar] [CrossRef] [Green Version]
  83. Formetta, G.; Feyen, L. Empirical evidence of declining global vulnerability to climate-related hazards. Glob. Environ. Chang. 2019, 57, 101920. [Google Scholar] [CrossRef] [PubMed]
  84. Federal Interagency Committee on Emergency Medical Services 2011 National EMS Assessment; National Highway Traffic Safety Administration, DOT HS; The National Academies Presss: Washington, DC, USA, 2011; p. 538.
  85. Minge, E.D.; National Cooperative Highway Research Program; National Cooperative Highway Research Program Synthesis Program; Transportation Research Board; National Academies of Sciences, Engineering, and Medicine. Emergency Medical Services Response to Motor Vehicle Crashes in Rural Areas; Transportation Research Board: Washington, DC, USA, 2013; ISBN 978-0-309-27104-2. [Google Scholar]
  86. Cutter, S.L.; Ash, K.D.; Emrich, C.T. Urban–Rural Differences in Disaster Resilience. Ann. Am. Assoc. Geogr. 2016, 1–17. [Google Scholar] [CrossRef]
  87. Lam, N.S.N.; Arenas, H.; Pace, K.; LeSage, J.; Campanella, R. Predictors of Business Return in New Orleans after Hurricane Katrina. PLoS ONE 2012, 7, e47935. [Google Scholar] [CrossRef] [PubMed]
  88. Zhang, Y.; Lindell, M.K.; Prater, C.S. Vulnerability of community businesses to environmental disasters. Disasters 2009, 33, 38–57. [Google Scholar] [CrossRef] [Green Version]
  89. Fothergill, A.; Peek, L.A. Poverty and disasters in the United States: A review of recent sociological findings. Nat. Hazards 2004, 32, 89–110. [Google Scholar] [CrossRef]
  90. Chinh, D.; Gain, A.; Dung, N.; Haase, D.; Kreibich, H. Multi-Variate Analyses of Flood Loss in Can Tho City, Mekong Delta. Water 2015, 8, 6. [Google Scholar] [CrossRef] [Green Version]
  91. Kelman, I.; Spence, R. A limit analysis of unreinforced masonry failing under flood water pressure. Mason. Int. 2003, 16, 51–61. [Google Scholar]
  92. Norris, F.H.; Smith, T.; Kaniasty, K. Revisiting the experience–behavior hypothesis: The effects of hurricane Hugo on hazard preparedness and other self-protective acts. Basic Appl. Soc. Psychol. 1999, 21, 37–47. [Google Scholar]
  93. Peacock, W.G.; Girard, C. Ethnic and racial inequalities in hurricane damage and insurance settlements. Hurric. Andrew Ethn. Gend. Sociol. Disasters 1997, 171–190. [Google Scholar]
  94. Elliott, J.R.; Pais, J. Race, class, and Hurricane Katrina: Social differences in human responses to disaster. Soc. Sci. Res. 2006, 35, 295–321. [Google Scholar] [CrossRef]
  95. Działek, J.; Biernacki, W.; Bokwa, A. Challenges to social capacity building in flood-affected areas of southern Poland. Nat. Hazards Earth Syst. Sci. 2013, 13, 2555–2566. [Google Scholar] [CrossRef]
  96. Khunwishit, S.; McEntire, D.A. Testing Social Vulnerability Theory: A Quantitative Study of Hurricane Katrina’s Perceived Impact on Residents living in FEMA Designated Disaster Areas. J. Homel. Secur. Emerg. Manag. 2012, 9, 16. [Google Scholar] [CrossRef]
  97. Kamel, N. Social Marginalisation, Federal Assistance and Repopulation Patterns in the New Orleans Metropolitan Area following Hurricane Katrina. Urban Stud. 2012, 49, 3211–3231. [Google Scholar] [CrossRef]
  98. Atreya, A.; Ferreira, S.; Michel-Kerjan, E. What drives households to buy flood insurance? New evidence from Georgia. Ecol. Econ. 2015, 117, 153–161. [Google Scholar] [CrossRef]
  99. Fothergill, A. Heads above Water: Gender, Class, and Family in the Grand Forks Flood; SUNY Press: New York, NY, USA, 2012; ISBN 0-7914-8472-6. [Google Scholar]
  100. American Society of Civil Engineers. 2012 Report Card For Texas’ Infrastructure; American Society of Civil Engineers: Reston, VA, USA, 2012. [Google Scholar]
  101. American Society of Civil Engineers. Flood Control in New Mexico; American Society of Civil Engineers: Reston, VA, USA, 2005. [Google Scholar]
  102. National Research Council Dam and Levee Safety and Community Resilience: A Vision for Future Practice; National Academies Press: Washington, DC, USA, 2012.
  103. Government Accounting Office (GAO) Flood Insurance: Participation of Indian Tribes in Federal and Private Programs; GAO: Washington, DC, USA, 2012.
  104. Qiang, Y.; Lam, N.S.N.; Cai, H.; Zou, L. Changes in Exposure to Flood Hazards in the United States. Ann. Am. Assoc. Geogr. 2017, 107, 1332–1350. [Google Scholar] [CrossRef]
  105. Koks, E.E.; Jongman, B.; Husby, T.G.; Botzen, W.J.W. Combining hazard, exposure and social vulnerability to provide lessons for flood risk management. Environ. Sci. Policy 2015, 47, 42–52. [Google Scholar] [CrossRef]
  106. Flanagan, B.E.; Gregory, E.W.; Hallisey, E.J.; Heitgerd, J.L.; Lewis, B. A Social Vulnerability Index for Disaster Management. J. Homel. Secur. Emerg. Manag. 2011, 8, 1–22. [Google Scholar] [CrossRef]
  107. Cutter, S.L.; Emrich, C.T. Social Vulnerability Index (SoVI®): Methodology and Limitations. Available online: https://data.femadata.com (accessed on 27 July 2017).
  108. Peacock, W.G.; Brody, S.D.; Seitz, W.A.; Merrell, W.J.; Vedlitz, A.; Zahran, S.; Harriss, R.C.; Stickney, R. Advancing Resilience of Coastal Localities: Developing, Implementing, and Sustaining the Use of Coastal Resilience Indicators: A Final Report; Hazard Reduction Recovery Center: College Station, TX, USA, 2010; pp. 1–148. [Google Scholar]
  109. Foster, K.A. In search of regional resilience. Urban Reg. Policy Its Eff. Build. Resilient Reg. 2012, 4, 24–59. [Google Scholar]
  110. Liu, D.; Li, Y. Social vulnerability of rural households to flood hazards in western mountainous regions of Henan province, China. Nat. Hazards Earth Syst. Sci. 2016, 16, 1123–1134. [Google Scholar] [CrossRef] [Green Version]
  111. Oulahen, G.; Mortsch, L.; Tang, K.; Harford, D. Unequal Vulnerability to Flood Hazards: “Ground Truthing” a Social Vulnerability Index of Five Municipalities in Metro Vancouver, Canada. Ann. Assoc. Am. Geogr. 2015, 105, 473–495. [Google Scholar] [CrossRef]
  112. Füssel, H.-M. Vulnerability: A generally applicable conceptual framework for climate change research. Glob. Environ. Chang. 2007, 17, 155–167. [Google Scholar] [CrossRef]
  113. Chen, C.; Noble, I.; Hellmann, J.; Coffee, J.; Murillo, M.; Chawla, N. University of Notre Dame Global Adaptation Index; University of Notre Dame: Notre Dame, IN, USA, 2015. [Google Scholar]
  114. Soares, M.B.; Gagnon, A.S.; Doherty, R.M. Conceptual elements of climate change vulnerability assessments: A review. Int. J. Clim. Chang. Strateg. Manag. 2012, 6–35. [Google Scholar] [CrossRef]
  115. Reckien, D.; Lwasa, S.; Satterthwaite, D.; McEvoy, D.; Creutzig, F.; Montgomery, M.; Schensul, D.; Balk, D.; Khan, I. Equity, environmental justice, and urban climate change. Clim. Chang. Cities Second Assess. Rep. Urban Clim. Chang. Res. Netw. 2018, 173–224. [Google Scholar]
  116. Hinkel, J. “Indicators of vulnerability and adaptive capacity”: Towards a clarification of the science–policy interface. Glob. Environ. Chang. 2011, 21, 198–208. [Google Scholar] [CrossRef]
  117. Mechler, R.; Bouwer, L.M.; Schinko, T.; Surminski, S.; Linnerooth-Bayer, J. Loss and Damage from Climate Change; Springer Nature: Basel, Switzerland, 2019. [Google Scholar]
  118. CEMHS The Spatial Hazard Events and Losses Database for the United States Version 14.1. 2019. Available online: https://cemhs.asu.edu/sites/default/files/2018-05/sheldus_readme.pdf (accessed on 17 July 2017).
  119. Downton, M.W.; Pielke, R.A. How Accurate are Disaster Loss Data? The Case of U.S. Flood Damage. Nat. Hazards 2005, 35, 211–228. [Google Scholar] [CrossRef] [Green Version]
  120. Wing, O.E.J.; Pinter, N.; Bates, P.D.; Kousky, C. New insights into US flood vulnerability revealed from flood insurance big data. Nat. Commun. 2020, 11, 1444. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  121. FEMA Public Assistance Funded Projects Detail; FEMA. 2017. Available online: https://www.fema.gov/openfema-dataset-public-assistance-funded-projects-details-v1 (accessed on 17 July 2017).
  122. Simley, J.D.; Carswell, W.J., Jr. The National Map—Hydrography: US Geological Survey Fact Sheet 2009–3054; US Geological Survey Nationcal Center: Reston, VA, USA, 2009. [Google Scholar]
  123. Ries, K.G., III; Guthrie, J.D.; Rea, A.H.; Steeves, P.A.; Stewart, D.W. StreamStats: A water resources web application. US Geol. Surv. Fact Sheet 2008, 3067. [Google Scholar] [CrossRef] [Green Version]
  124. Brody, S.D.; Zahran, S.; Highfield, W.E.; Grover, H.; Vedlitz, A. Identifying the impact of the built environment on flood damage in Texas. Disasters 2008, 32, 1–18. [Google Scholar] [CrossRef] [PubMed]
  125. Homer, C.G.; Dewitz, J.A.; Yang, L.; Jin, S.; Danielson, P.; Xian, G.; Coulston, J.; Herold, N.D.; Wickham, J.D.; Megown, K. Completion of the 2011 National Land Cover Database for the conterminous United States-Representing a decade of land cover change information. Photogramm. Eng. Remote Sens. 2015, 81, 345–354. [Google Scholar]
  126. Zeileis, A.; Kleiber, C.; Jackman, S. Regression models for count data in R. J. Stat. Softw. 2008, 27, 1–25. [Google Scholar] [CrossRef] [Green Version]
  127. Hilbe, J.M.; Robinson, J.O. msme: Functions and Datasets for “Methods of Statistical Model Estimation”. 2018. Available online: https://cran.r-project.org/web/packages/msme/msme.pdf (accessed on 17 July 2017).
  128. Burnham, K.P.; Anderson, D.R. Multimodel Inference: Understanding AIC and BIC in Model Selection. Sociol. Methods Res. 2004, 33, 261–304. [Google Scholar] [CrossRef]
  129. Akaike, H. A new look at the statistical model identification. IEEE Trans. Autom. Control 1974, 19, 716–723. [Google Scholar] [CrossRef]
  130. Zuur, A.F.; Ieno, E.N.; Walker, N.; Saveliev, A.A.; Smith, G.M. Mixed Effects Models and Extensions in Ecology with R; Statistics for Biology and Health; Springer: New York, NY, USA, 2009; ISBN 978-0-387-87457-9. [Google Scholar]
  131. Bivand, R.S.; Wong, D.W. Comparing implementations of global and local indicators of spatial association. Test 2018, 27, 716–748. [Google Scholar] [CrossRef]
  132. Reckien, D. What is in an index? Construction method, data metric, and weighting scheme determine the outcome of composite social vulnerability indices in New York City. Reg. Environ. Chang. 2018, 18, 1439–1451. [Google Scholar] [CrossRef] [Green Version]
  133. Ridgeway, G.; Edwards, D.; Kriegler, B.; Schroedl, S.; Southworth, H. gbm: Generalized Boosted Regression Models. 2015. Available online: https://cran.r-project.org/web/packages/gbm/index.html (accessed on 17 July 2017).
  134. Fox, J.; Weisberg, S. An R Companion to Applied Regression; Sage publications: New York, NY, USA, 2018; ISBN 1-5443-3648-9. [Google Scholar]
  135. Kalogirou, S. Destination Choice of Athenians: An Application of Geographically Weighted Versions of Standard and Zero Inflated P oisson Spatial Interaction Models. Geogr. Anal. 2016, 48, 191–230. [Google Scholar] [CrossRef]
  136. CIESEN. Elderly Population, Percentage of People Who are Age 65 and Older. 2000. Available online: http://ciesin.columbia.edu/sub_guide.html (accessed on 17 July 2017).
  137. Mcleman, R.; Smit, B. Vulnerability to climate change hazards and risks: Crop and flood insurance. Can. Geogr. Geogr. Can. 2006, 50, 217–226. [Google Scholar] [CrossRef]
  138. Tate, E.; Strong, A.; Kraus, T.; Xiong, H. Flood recovery and property acquisition in Cedar Rapids, Iowa. Nat. Hazards 2016, 80, 2055–2079. [Google Scholar] [CrossRef] [Green Version]
  139. Hardy, R.D.; Hauer, M.E. Social vulnerability projections improve sea-level rise risk assessments. Appl. Geogr. 2018, 91, 10–20. [Google Scholar] [CrossRef] [Green Version]
  140. Parks, R.M.; Bennett, J.E.; Tamura-Wicks, H.; Kontis, V.; Toumi, R.; Danaei, G.; Ezzati, M. Anomalously warm temperatures are associated with increased injury deaths. Nat. Med. 2020, 26, 65–70. [Google Scholar] [CrossRef] [Green Version]
  141. Cooley, D.; Nychka, D.; Naveau, P. Bayesian Spatial Modeling of Extreme Precipitation Return Levels. J. Am. Stat. Assoc. 2007, 102, 824–840. [Google Scholar] [CrossRef]
  142. Cai, H.; Lam, N.S.N.; Zou, L.; Qiang, Y. Modeling the Dynamics of Community Resilience to Coastal Hazards Using a Bayesian Network. Ann. Am. Assoc. Geogr. 2018, 108, 1260–1279. [Google Scholar] [CrossRef]
  143. De Sherbinin, A.; Bardy, G. Social vulnerability to floods in two coastal megacities: New York City and Mumbai. Vienna Yearb. Popul. Res. 2016, 1, 131–165. [Google Scholar] [CrossRef] [Green Version]
Figure 1. Results of text mining for event narratives from flood fatalities data (n = 283). (A) Demographic trends (age and gender) in flood fatalities cases; (B) cause of death involving cars, drowning or RVs/mobile homes.
Figure 1. Results of text mining for event narratives from flood fatalities data (n = 283). (A) Demographic trends (age and gender) in flood fatalities cases; (B) cause of death involving cars, drowning or RVs/mobile homes.
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Figure 2. Deviance explained for (A) fatality models (difference between each model and a null model in predicting death counts) and R2 values for (B) property models.
Figure 2. Deviance explained for (A) fatality models (difference between each model and a null model in predicting death counts) and R2 values for (B) property models.
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Figure 3. Bivariate choropleth map showing predicted fatality rates (per 100,000 people) and property damage ratios (normalized by housing value across each county) for a 500-year riverine flood event universally affecting the entire contiguous US.
Figure 3. Bivariate choropleth map showing predicted fatality rates (per 100,000 people) and property damage ratios (normalized by housing value across each county) for a 500-year riverine flood event universally affecting the entire contiguous US.
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Table 1. Summary of quantitative validation for social vulnerability to flood outcomes using correlation or OLS (Ordinary Least Squares) regression. + denotes variables significantly positively correlated with the outcome, and—for variables significantly negatively correlated with outcomes. Note SoVI (The Social Vulnerability Index) is normalized on a z-score, and depending on the studies, positive SoVI scores may represent high or low social vulnerability. For simplification in this table we refer to positive SoVI scores as higher social vulnerability regardless of the numeric transformation employed in the paper. SVI = The Social Vulnerability Index from Flanagan et al. [106]; SoVI = The Social Vulnerability Index [107]; CDRI = Community Disaster Resilience Index [108] RCI = Resilience Capacity Index [109]. FEMA = Federal Emergency Management Authority.
Table 1. Summary of quantitative validation for social vulnerability to flood outcomes using correlation or OLS (Ordinary Least Squares) regression. + denotes variables significantly positively correlated with the outcome, and—for variables significantly negatively correlated with outcomes. Note SoVI (The Social Vulnerability Index) is normalized on a z-score, and depending on the studies, positive SoVI scores may represent high or low social vulnerability. For simplification in this table we refer to positive SoVI scores as higher social vulnerability regardless of the numeric transformation employed in the paper. SVI = The Social Vulnerability Index from Flanagan et al. [106]; SoVI = The Social Vulnerability Index [107]; CDRI = Community Disaster Resilience Index [108] RCI = Resilience Capacity Index [109]. FEMA = Federal Emergency Management Authority.
StudyGeographic ExtentTemporal ExtentScale NHazard ControlFlood Outcome VariableMain Sociodemographic Variables
Rufat et al. 2019New York and New Jersey affected Sandy areaone hazard (Sandy 2012)census track3947Flood depthFEMA Individual Assistance+SoVI
% property loss+socioeconomic status
Zahran et al. 2008Texas1997–2001county832precipitationFatality+ social vulnerability (defined as high minority and lower economic status)
Finch et al. 2010New Orleansone hazard (Katrina 2005)census tract181Flood DepthRate of return to home-SoVI
Bakkensen et al. 2017 *10 states (Southeastern USA)2000–2012county41,916NCDC (National Climate Data Center) magnitudeFatality+SVI -CDRI, -RCI
Damage+SoVI, +SVI, -CDRI, -RCI
Fekete et al. 20093 regions (River Elbe, Mulde, and Danube, Germany)one hazard in 2002house-hold1697noneDisplacement+urban, +homeowner, +rooms
Shelter+age, +homeowner
* includes flash flood, hail, wind, strong wind, thunderstorm, tornadoes.
Table 2. Social variables used in the analysis, description, rationale (from Cutter et al. 2003, unless otherwise specified with *), hypothesized relationship (+F for increase in fatalities, -F for decrease in fatalities, +D for increase in damage, -D for decrease in damage), and the data source (DC = decennial census).
Table 2. Social variables used in the analysis, description, rationale (from Cutter et al. 2003, unless otherwise specified with *), hypothesized relationship (+F for increase in fatalities, -F for decrease in fatalities, +D for increase in damage, -D for decrease in damage), and the data source (DC = decennial census).
VariableDescriptionRationaleHypothesized RelationshipSourceCensus Group or Table
totalPopulationTotal populationTo offset fatality models (control for highly populated areas) *+F2010 DCP3
%BlackPercent of population BlackResidential locations in high hazard areas+F, +D2010 DCP2
%NativeAmericanPercent of population Native American+F, +D2010 DCP3
%AsianPercent of population Asian+F, +D2010 DCP3
%HispanicPercent of population Hispanic+F, +D2010 DCP4
%FemalePercent of population femaleLower wages, family care responsibilities can increase vulnerability, but men more likely to die in floods-F2010 DCP12
%FemaleCivilianWorkforcePercent of women who are working+D2010 5-year ACSB23001
%FemaleHeadOfHousePercent households headed by females+F, +D2010 DCP18
%Under5yoPercent population under 5Higher potential for fatalities- drowning+F2010 DCP12
%Over65yoPercent population over 65Difficulty evacuating due to mobility constraints+F2010 DCP12
%NursingHomePercent population in nursing home+F2010 DCP42
%NoEnglishPercent of population with household has a limited English-speaking statusDifficulty communicating for evacuation *+F2010 5-year ACSB16002
perCapitaIncomePer capital income in past 12 monthsLower incomes indicate poverty+D2010 5-year ACSB19301
%RenterOccPercent population in rental homesLess invested in flood mitigation to prevent damage+D2010 DCH4
%UnoccupiedPercent of houses unoccupiedValue, quality, of housing stock may indicate “economic health” of a community, overcrowded and vacant housing may be likely to experience more damage+D2010 DCH3
medianHouseValueMedian value of owner-occupied housing (USD)-D2010 5-year ACSB25077
medianRentMedian value of renter occupied housing (USD)-D2010 5-year ACSB25064
%MobileHomesPercent of population living in mobile homes+D, +F2010 5-year ACSB25024
peoplePerUnitNumber of people per room+D2010 5-year ACSB25014
totalHouseValueCalculated by summing number of homes in each value category, and adding total valueUsed to normalize property damage data *+D2010 5-year ACSB25075
%NoCarPercent of homes with no vehicleCould be easier to evacuate, also an indicator of relative less poverty+F2010 5-year ACSB25044
%UnderPovertyPercent of population living in poverty, defined threshold varies by age, household and number of childrenRelated to ability to absorb losses and invest in resilience to hazard impacts, access insurance and other programs+D2010 5-year ACSC17002
%Households200kPercent of households making at least USD 200,000 in joint income in past year-D2010 5-year ACSB19001
%LessThan12yearsEducationPercent of population who have not completed 12th grade (high school)Low education constrains ability to understanding warning information+F2010 5-year ACSB15002
%NoHealthInsurancePercent of population with no health insuranceHospitals, and ability to access care due to mobility constraints and health insurance, could affect disaster impacts+F2010 5-year ACSB27001
%AmbulatoryDifficultyPercent of population with mobility constraints+F2013 5-year ACSB18105
HOSTPTCPer capita number of community hospitals+FSOVI variables
%SocialSecurityPercent population with social security incomeSocial dependence indicates economic marginalization requiring extra support+long term D (not property)2010 5-year ACSB19055
%EmployedInServicesPercent population employed in services including healthcare support, fire-fighting, policing, food preparing and maintenanceOccupations that could be affected by hazard event (e.g., jobs that may not return post-disaster)+long term D (not property)2010 5-year ACSC24010
%EmployedInExtractivePercent population employed in mining, quarrying, gas extraction or forestry+long term D (not property)2010 5-year ACSC24030
%CivilianUnemployedPercent population unemployed in labor forceLess economic capacity to invest in resilience+D2010 5-year ACSB23001
%FamilyPercent of families where both parents are presentPotential for dual incomes or house labor may increase ability to invest in flood mitigation-D2010 DCP19
%RuralRural population/total population per countryRuralness related to flood fatalities due to access issues, less flood mitigation investment *+D, +F2010 DC(P002001/P002005) in P2
SoVI2006–2010 Social Vulnerability IndexHypothesized link to propensity for loss in hazards+D, +FUniversity South CarolinaNA
Race-povertyMultiplying %Black, Hispanic, Asian and Native American with povertyIntersectional race and poverty lead to outsized hazard impacts, not race alone (Elliot and Pais 2006)+D2010 DC and 2010 ACSP2,3,4 and C170002
Table 3. Fatality and Property damage validation models.
Table 3. Fatality and Property damage validation models.
Model #RationaleIndependent VariablesDependent Variables
1Null Model1Fatality, Damage
2Biophysical VariablesfloodReturnTime + %Impervious+ flashflood **
3SoVI index, controlling for hazard intensityUS_SOVI+ floodReturnTime+ %impervious+ flashFlood
4aSocial factors identified in literaturefloodReturnTime + flashFlood + %Rural + %MobileHomes + %UnderPoverty + %Under5yo + %Over65yo + %NoEnglish + %AmbulatoryDifficulty+ %NoHealthInsurance+ HOSPTPC +%LessThan12yearsEducation+ %NoCar
4bSocial factors identified in the literature + regional variationfloodReturnTime + flashFlood + %Rural + %MobileHomes + %UnderPoverty + %Under5yo + %Over65yo + %NoEnglish + %AmbulatoryDifficulty + %NoHealthInsurance+ %LessThan12yearsEducation + HOSPTPC + %NoCar + regions
4cSocial factors identified in the literature + divisional variationfloodReturnTime + flashFlood + %Rural + %MobileHomes + %UnderPoverty + %Under5yo + %Over65yo + %NoEnglish + %AmbulatoryDifficulty +%NoHealthInsurance+ %LessThan12yearsEducation + HOSPTPC + %NoCar +divisions
5aSocial factors identified via machine learningfloodReturnTime + flashFlood + %Rural + %NoEnglish + %Asian
5bfloodReturnTime + flashFlood + %MobileHomes + %Unoccupied + perCapitaIncome * + %Rural + peoplePerUnit + medianRent + %NoCar + %Hispanic + %NursingHomeFatality as binary (any deaths >1 set to 1)
5cfloodReturnTime + %Rural+ %Black ***+ %Asian+%Civilianunemployed+HOSPTPC+%NoCar+%Under5yo+%Unoccupied+ medianHouseValueProperty Damage (as ratio of housing value)
6aSocial factors identified in the literaturefloodReturnTime + medianHouseValue + %Black +%Asian+ %Hispanic + %Native American+peopleperunit+%unoccupied+ %renters + %Rural + %MobileHomes + %UnderPoverty
6bSocial factors identified in the literature + regional variationfloodReturnTime + medianHouseValue + %Black +%Asian+ %Hispanic + %Native American+peopleperunit+%unoccupied+ %renters + %Rural + %MobileHomes + %UnderPoverty + regions
6cSocial factors identified in the literature + divisional variationfloodReturnTime + medianHouseValue + %Black +%Asian+ %Hispanic + %Native American+peopleperunit+%unoccupied+ %renters + %Rural + %MobileHomes + %UnderPoverty + divisions
6dSocial factors identified in the literature with race–poverty interaction + divisional variationfloodReturnTime + medianHouseValue + %Black * %UnderPoverty +%Asian *%UnderPoverty + %Hispanic * %UnderPoverty + %Native American*%UnderPoverty +peopleperunit+%unoccupied+ %renters + %Rural + %MobileHomes + divisions
* correlated with households earning over USD 200,000, excluded from model; ** flash flood only included in fatality models (tied to death in the literature, but not property loss); *** correlated with %FemaleHeadofHouse.
Table 4. Social variables with non-zero relative importance from machine learning for fatalities and >1% importance for property damage ratios.
Table 4. Social variables with non-zero relative importance from machine learning for fatalities and >1% importance for property damage ratios.
VariableRelative Influence—Fatalities as CountsRelative Influence—Fatalities as BinaryRelative Influence—ln Property Damage Ratio
%MobileHomes 37.990.19
%Unoccupied 16.791.12
perCapitaIncome 14.761.25
%Rural85.8914.0149.28
%Households200k 5.903.06
peoplePerUnit 4.090
medianRent 3.8711.93
%NoCar 1.411.31
%Hispanic 0.760.54
%NursingHome 0.440.91
%No English9.67 0.48
%Asian4.44 3.51
%Hospital 7.76
%Black 1.93
%Unemployed 1.81
%FemaleHeadHouse 1.77
%under5 1.56
%perCapitaIncome 1.25
%Unoccupied
Other variables predicting property damage ratios with relative importance >0 but <1 include %Native American, %noInsurance, %EmployedinServices, %Underpoverty, %Female, %Femaleworkforce, %Socialsecurity and %employedinextractive.
Table 5. Zero-inflated fatality model results. ML = machine learning model. Lit indicates models formed from the literature. Table 3 links model descriptions to model numbers in this table.
Table 5. Zero-inflated fatality model results. ML = machine learning model. Lit indicates models formed from the literature. Table 3 links model descriptions to model numbers in this table.
Zero Inflated Fatality Models
Dependent Variable:
Death Count
Biophysical (2)SoVI (3)Social (Lit) (4a)Social (Lit)+reg (4b)Social (Lit)+div (4c)Social-ML (count) (5a)Social-ML (binary) (5b)
floodReturnTime0.199 *** (0.074)0.215 *** (0.070)0.212 *** (0.056)0.206 *** (0.055)0.108 ** (0.047)0.114 ** (0.049)0.201 *** (0.055)
flashFlood0.109 (0.197)0.041 (0.184)−0.093 (0.164)−0.137 (0.164)−0.049 (0.165)0.115 (0.165)−0.103 (0.164)
%Impervious−0.541 *** (0.080)−0.407 *** (0.075)
US_SOVI 0.331 *** (0.041)
%Black −0.077 (0.104)−0.191 * (0.114)−0.161 (0.117)
%Female −0.039 (0.149)−0.126 (0.150)−0.083 (0.155)
%NoHealthInsurance 0.326 ** (0.135)0.258 * (0.140)0.199 (0.146)
%Asian −0.149 * (0.080)
%NursingHome 0.296 ** (0.118)
%Rural 0.793 *** (0.127)0.784 *** (0.133)0.761 *** (0.128)1.102 *** (0.093)0.678 *** (0.147)
peoplePerUnit 0.177 (0.153)
%Unoccupied 0.311 *** (0.117)
%MobileHomes 0.070 (0.145)0.032 (0.153)0.082 (0.149) 0.413 *** (0.125)
%UnderPoverty −0.261 (0.207)−0.204 (0.207)−0.139 (0.212)
%Under5yo 0.429 *** (0.133)0.497 *** (0.142)0.448 *** (0.137)
%Over65yo 0.452 *** (0.139)0.555 *** (0.145)0.510 *** (0.144)
%NoEnglish −0.644 (0.498)−0.776 (0.511)−0.992 * (0.518)0.207 (0.383)
perCapitaIncome 0.287 (0.177)
%Hispanic 0.087 (0.174)
%NoCar 0.145 (0.147)0.225 (0.159)0.235 (0.166) 0.038 (0.117)
%AmbulatoryDifficulty 0.276 ** (0.140)0.150 (0.149)0.109 (0.151)
NE_region 0.123 (0.399)
S_region 0.597 * (0.306)
MW_region 0.015 (0.332)
NE_MA_division 0.357 (0.314)
S_SA_division 0.290 (0.313)
S_ESC_division 0.838 *** (0.301)
S_WSC_division 0.915 *** (0.259)
medianRent −0.340 * (0.174)
Constant−14.521 *** (0.158)−14.379 *** (0.146)−14.507 *** (0.159)−14.777 *** (0.298)−14.329 *** (0.235)−13.829 *** (0.200)−14.313 *** (0.135)
Observations11,62911,62911,62911,62911,62911,62911,629
Log Likelihood−1440.462−1406.797−1349.118−1345.736−1327.129−1355.418−1357.420
Akaike Inf. Crit.2894.9242829.5942732.2352731.4722696.2582728.8362744.839
Note: * p ** p *** p < 0.01.
Table 6. OLS Property damage ratio model results. ML = machine learning model. Lit indicates models formed from literature. Table 3 links model descriptions to model numbers in this table.
Table 6. OLS Property damage ratio model results. ML = machine learning model. Lit indicates models formed from literature. Table 3 links model descriptions to model numbers in this table.
OLS Property Models
Dependent Variable:
Property Damage as Ratio of Total Housing Value
Biophysical (2)SoVI (3)Social (Lit) (6a)Social (Lit)+reg (6b)Social (Lit)+div (6c)Social+div+race-class(6d)Social-ML (5c)
floodReturnTime0.354 *** (0.029)0.359 *** (0.028)0.392 *** (0.027)0.387 *** (0.027)0.401 *** (0.027)0.403 *** (0.027)0.397 *** (0.027)
%Impervious−1.013 *** (0.033)−0.827 *** (0.033)
US_SOVI 0.283 *** (0.013)
medianHouseValue −0.450 *** (0.048)−0.427 *** (0.052)−0.287 *** (0.057)−0.398 *** (0.059)−0.555 *** (0.045)
%Asian −0.207 *** (0.048)−0.211 *** (0.049)−0.277 *** (0.048)−0.400 *** (0.063)−0.229 *** (0.047)
%Hispanic −0.058 (0.067)−0.002 (0.072)−0.209 *** (0.073)−0.243 *** (0.078)
%NativeAmerican 0.087 ** (0.037)0.086 ** (0.039)0.037 (0.039)−0.027 (0.066)
%Black −0.032 (0.036)0.015 (0.039)0.038 (0.038)−0.193 *** (0.050)0.112 *** (0.035)
peoplePerUnit −0.227 *** (0.057)−0.221 *** (0.057)−0.267 *** (0.059)−0.274 *** (0.060)
%CivilianUnemployed −0.100 ** (0.045)
%NoCar −0.132 ** (0.059)
%Under5yo −0.072 ** (0.035)
%Unoccupied 0.088 ** (0.043)0.072 (0.045)0.073 (0.045)0.104 ** (0.045)0.116 *** (0.042)
%RenterOcc −0.086 * (0.048)−0.084 * (0.049)−0.190 *** (0.049)−0.031 (0.053)
HOSPTPC 0.231 *** (0.030)
%Rural 0.923 *** (0.049)0.917 *** (0.049)0.721 *** (0.050)0.680 *** (0.051)0.853 *** (0.040)
%MobileHomes −0.195 *** (0.044)−0.112 ** (0.050)0.045 (0.050)0.091 * (0.051)
%UnderPoverty 0.329 *** (0.066)0.346 *** (0.067)0.481 *** (0.067)0.315 *** (0.070)
NE_region 0.383 *** (0.146)
S_region −0.019 (0.128)
MW_region 0.242 * (0.141)
W_P_division 0.782 *** (0.203)0.989 *** (0.206)
NE_NE_division 0.798 *** (0.189)0.707 *** (0.193)
NE_MA_division 0.442 *** (0.165)0.389 ** (0.169)
MW_ENC_division −0.343 ** (0.152)−0.354 ** (0.155)
MW_WNC_division 1.057 *** (0.151)0.970 *** (0.153)
S_SA_division −0.577 *** (0.148)−0.392 ** (0.155)
S_ESC_division −0.172 (0.159)−0.071 (0.163)
S_WSC_division 0.729 *** (0.143)0.816 *** (0.148)
%Asian:%UnderPoverty −0.253 *** (0.059)
%tUnderPoverty:%Hispanic 0.158 *** (0.053)
%UnderPoverty:%NativeAmerican 0.057 * (0.032)
%UnderPoverty:%Black 0.231 *** (0.033)
Constant−11.446 *** (0.029)−11.334 *** (0.029)−11.337 *** (0.031)−11.445 *** (0.110)−11.651 *** (0.118)−11.842 *** (0.122)−11.355 *** (0.029)
Observations11,62911,62911,62911,62911,62911,62911,629
Adjusted R20.0890.1250.1960.1970.2240.2290.198
F Statistic568.158 *** (df = 2; 11,626)553.060 *** (df = 3; 11,625)237.754 *** (df = 12; 11,616)191.508 *** (df = 15; 11,613)168.896 *** (df = 20; 11,608)145.003 *** (df = 24; 11,604)288.230 *** (df = 10; 11,618)
Note: * p ** p *** p < 0.01.
Table 7. Top 10 US counties with highest predicted fatality rates (per 100,000 people) and property damage ratios for a 500-year riverine flood using the 2010 census. SoVI scores (from The Hazards and Vulnerability Institute, 2006–2010 version) reported in percentiles. Higher SoVI percentiles (ranging from 0 to 1) indicates higher social vulnerability.
Table 7. Top 10 US counties with highest predicted fatality rates (per 100,000 people) and property damage ratios for a 500-year riverine flood using the 2010 census. SoVI scores (from The Hazards and Vulnerability Institute, 2006–2010 version) reported in percentiles. Higher SoVI percentiles (ranging from 0 to 1) indicates higher social vulnerability.
CountyDeathsSoVICountyProperty DamageCountySoVI
Baylor, TX40.90Holmes, MS0.258Buffalo, SD0.87
Stone, AR40.88Jefferson, MS0.181Daniels, MT0.93
McIntosh, OK40.94Hudspeth, TX0.144Sioux, ND0.97
Letcher, KY40.79Shannon, SD0.099Brooks, TX1
Motley, TX40.94Todd, SD0.098Bronx, NY1
Sabine, LA40.85Wilcox, AL0.091Todd, SD0.88
McPherson, NE30.56Buffalo, IL0.080Shannon, SD1
Hickman, KY30.83Issaquena, MS0.064Menominee, WI0.99
Menard, TX30.99Allendale, SC0.062La Salle, TX0.90
Montgomery, AR30.96Sioux, ND0.059Clay, GA1

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Tellman, B.; Schank, C.; Schwarz, B.; Howe, P.D.; de Sherbinin, A. Using Disaster Outcomes to Validate Components of Social Vulnerability to Floods: Flood Deaths and Property Damage across the USA. Sustainability 2020, 12, 6006. https://doi.org/10.3390/su12156006

AMA Style

Tellman B, Schank C, Schwarz B, Howe PD, de Sherbinin A. Using Disaster Outcomes to Validate Components of Social Vulnerability to Floods: Flood Deaths and Property Damage across the USA. Sustainability. 2020; 12(15):6006. https://doi.org/10.3390/su12156006

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Tellman, Beth, Cody Schank, Bessie Schwarz, Peter D. Howe, and Alex de Sherbinin. 2020. "Using Disaster Outcomes to Validate Components of Social Vulnerability to Floods: Flood Deaths and Property Damage across the USA" Sustainability 12, no. 15: 6006. https://doi.org/10.3390/su12156006

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