Abstract
Global change problems place a new set of demands on hydrologic models. The primary purpose for representation of land surface hydrology in the context of coupled land-atmosphere models is to partition downward solar and longwave radiation into latent, sensible, and ground heat fluxes, and upward longwave radiation, rather than to predict streamflow. Nonetheless, past work in the development and application of conceptual streamflow simulation models for operational applications, such as forecasting, can provide valuable lessons, especially with respect to model parameter parsimony, for the development and application of land surface parameterizations for coupled land-atmosphere models. Some important issues in model development and application are illustrated in the context of the Variable Infiltration Capacity two-layer (VIC-2L) model. Application of the VIC-2L model to FIFE (central Kansas Grassland) and ABRACOS (cleared Amazonia tropical forest) field data are described. A version of VIC-2L that incorporates streamflow routing is described, along with some results of its application off-line (climatalogical forcing) to the Columbia River basin. Finally, an approach for regional estimation of the parameters of VIC-2L is described, along with preliminary results for an application to the Columbia River basin (drainage area approximately 615,000 km2) at a one degree by one degree spatial resolution.
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Lettenmaier, D.P. (1995). Modeling of Runoff and Streamflow at Regional to Global Scales. In: Oliver, H.R., Oliver, S.A. (eds) The Role of Water and the Hydrological Cycle in Global Change. NATO ASI Series, vol 31. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-79830-6_10
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DOI: https://doi.org/10.1007/978-3-642-79830-6_10
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