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Coupling uncertain patterns of climatic variables in estimating evaporation from open water bodies

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Abstract

Since the variables involved in changing evaporation rate interact with each other, the result of first-order Sensitivity Analysis (SA1) is imperfect to reveal the dynamics of this phenomenon. The main goal of this study was to reveal coupling patterns of climatic agents in forming evaporation. The Partial Deviations (PaD) method, based on Back-Propagation Artificial Neural Network (BPNN), was used to reveal these patterns. While non-derivative methods survey only first-order sensitivity values, PaD can investigate higher-order sensitivity values. In this way, Summing Squares of partial Derivations (SSD) revealed magnitude of interactions. Also, gradient surfaces statistically reflected information on evaporation changes. To achieve better results, Wavelet-based denoising method was used to remove high-frequency component of inputs. The new method was tested at two neighboring sites (Ahvaz and Isfahan) in Iran. By feeding denoised input to BPNN, the uncertainty of first/ second order PaD values was reduced highly at Ahvaz station by 47.76 and 28.68%. At Ahvaz station coupling between one day-lagged evaporation with air temperature and humidity with magnitudes of 26.37 and 25.21%, respectively, had a major effect on the evaporation gradient. Similarly, the major effects on evaporation rate at Isfahan station belonged to coupling one day-lagged evaporation with air temperature and wind speed with magnitudes of 36.97 and 18.98%, respectively. The interaction patterns showed that rate of evaporation reversed for both stations in warm seasons because of an increase in atmospheric humidity. It seems cities near sea, despite having warm climate, show complex patterns of evaporation. Temperature, one-day-lagged evaporation, wind speed, and radiation aroused effect of other variables. The interaction of these variables caused an inverse rate of evaporation in some cases where the role of one day-lagged evaporation, as the ambient humidity memory, was more prominent than the rest.

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Acknowledgements

This study was supported by the National Key R&D Program of China (Grant No. 2022YFC3002804), CAS Pioneer Talents Program and CAS-PIFI professorial fellowship (Grant No. 2022VMA00).

Funding

National Key R&D Program of China (Grant No. 2022YFC3002804), CAS Pioneer Talents Program and CAS-PIFI professorial fellowship (Grant No. 2022VMA00).

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VN: Conceptualization, Supervision, Methodology, Writing—review & editing. MS-F: Project administration, Formal analysis, Methodology, Investigation, Resources, Data curation. YZ: Supervision, Formal analysis, Methodology, Writing—original draft.

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Correspondence to Vahid Nourani.

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Appendix A: Survey the noise affection on the quality of SA

Appendix A: Survey the noise affection on the quality of SA

Radar / Spider charts of Fig. A1 illustrate the width of CIs for the mean SSD values in the multidimensional space of noisy and denoised variables and examples at the Ahvaz station. From Fig. A1, the results show that denoised input vectors led to a decrease of CI width for both PaD1 and PaD2 mean values (also, led to enhance the model's performance as Figs. S4-S5) because of the reduction of the riot in the PaD values. It should be noted that the internal instability of ANNs because of random initial weights is also the inability to find the most optimal structure for it (here for Et modeling) in terms of the number of neurons are other reasons for the disturbance of results. An example of noise affection on coupling patterns was reported as Fig. A2 for the interaction of paired variables of Et-1 with T and Rh at Ahvaz station. It can be seen that a high-frequency component in the input vector amplifies disturbances and hinders the interpretation of the coupling patterns.

See Figs.

Fig. 10
figure 10

The noise affection on the quality of first- and second-order Partial Deviations (PaD1, 2) values regarding uncertainty reduction, for example at Ahvaz station a PaD1, b PaD2

10 and

Fig. 11
figure 11

The noise affection on the quality of coupling patterns for example at Ahvaz station, a interaction of one-day lagged evaporation (Et-1) and temperature (T), b interaction of Et-1 and relative humidity (Rh)

11

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Nourani, V., Sayyah-Fard, M. & Zhang, Y. Coupling uncertain patterns of climatic variables in estimating evaporation from open water bodies. Stoch Environ Res Risk Assess 38, 383–405 (2024). https://doi.org/10.1007/s00477-023-02549-3

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