水文循环模拟中蒸散发估算方法综述

doi:10.11821/xb201301014

Abstract

Abstract: Actual evapotranspiration is a key process of hydrological cycle and a sole term that links land surface water balance equation and land surface energy balance equation. Evapotranspiration plays a key role in simulating hydrological effect of climate change, and a review of evapotranspiration estimation methods in hydrological models is of vital importance. This paper firstly summarizes the evapotranspiration estimation methods in hydrological models and then classifies them into integrated discounting methods and classification gathering methods by their mechanism. Integrated discounting methods are usually used in hydrological models and two differences exist among these methods, one is in the potential evaporation estimation methods, and the other difference is the function for defining relationship between potential evaporation and actual evapotranspiration. Due to the higher information requirements of the Penman-Monteith method and the existing uncertainty in those data, simplified empirical methods for calculating potential and actual evapotranspiration are widely used in hydrological models. Different evapotranspiration calculation methods are used in different hydrological models, and importance and difficulty in the selection of most suitable evapotranspiration methods in various hydrological models with different complexity is discussed. Finally, this paper points out the development direction of the evapotranspiration estimating methods in hydrological models.

Key words: hydrological model, actual evaporation, potential evaporation, function of soil moisture

ZHAO Lingling, XIA Jun, XU Chong-yu, WANG Zhonggen, LeszekSOBKOWIAK. A review of evapotranspiration estimation methods in hydrological Models[J].Acta Geographica Sinica, 2013, 68(1): 127-136.

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A review of evapotranspiration estimation methods in hydrological Models

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