Abstract

Land surface evapotranspiration (ET) is important in land-atmosphere interactions of water and energy cycles. However, regional ET simulation has a great uncertainty. In this study, a highly-efficient parameter optimization framework was applied to improve ET simulations of the Community Land Model version 4.0 (CLM4) in China. The CLM4 is a model at land scale, and therefore, the monthly ET observation was used to evaluate the simulation results. The optimization framework consisted of a parameter sensitivity analysis (also called parameter screening) by the multivariate adaptive regression spline (MARS) method and sensitivity parameter optimization by the adaptive surrogate modeling-based optimization (ASMO) method. The results show that seven sensitive parameters were screened from 38 adjustable parameters in CLM4 using the MARS sensitivity analysis method. Then, using only 133 model runs, the optimal values of the seven parameters were found by the ASMO method, demonstrating the high efficiency of the method. For the optimal parameters, the ET simulations of CLM4 were improved by 7.27%. The most significant improvement occurred in the Tibetan Plateau region. Additional ET simulations from the validation years were also improved by 5.34%, demonstrating the robustness of the optimal parameters. Overall, the ASMO method was found to be efficient for conducting parameter optimization for CLM4, and the optimal parameters effectively improved ET simulation of CLM4 in China.

Highlights

  • Land surface evapotranspiration (ET) refers to the loss of water from the land surface into the atmosphere through evaporation from ground and canopy rainfall interception and transpiration from vegetation

  • This study focused on the parametric optimization of Community Land Model version 4.0 (CLM4) to improve ET simulation in China

  • For canopy evaporation and transpiration, a significant decrease using the optimal simulations occurred between July and September and between October yr−1 in the mid-eastern regions of China. These results demonstrated that the optimal parameters obtained by the adaptive surrogate modeling-based optimization (ASMO) method effectively improved the ET simulation of CLM4

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Summary

Introduction

Land surface evapotranspiration (ET) refers to the loss of water from the land surface into the atmosphere through evaporation from ground and canopy rainfall interception and transpiration from vegetation. ET returns about 60% of global terrestrial precipitation to the atmosphere; in arid areas, the percentage reaches 90% [1,2]. 59% of global terrestrial available energy to the atmosphere in the form of latent heat [3]. It plays an important role in the land-atmosphere interactions of water and energy cycles. Precise estimation of ET is of great significance in accurately quantifying the land-atmosphere interaction, in monitoring land surface extreme events such as droughts and floods, and in assessing the potential impact of climate change.

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