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Estimation of surface heat fluxes and evapotranspiration Using Community Land Model

机译:利用社区陆地模型估计表面热通量和蒸散蒸腾

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Land surface heat and water fluxes are key components of water and energy cycles between land and atmosphere. Information about these surface fluxes can guide agricultural production and environmental preservation, and manage different ecosystems to mitigate climate change. The main objective of this work is to estimate the surface heat fluxes and evapotranspiration. For this purpose, the Community Land Model Version 3 was used, atmospheric forcing data and flux observation were extracted from AmeriFlux standardized Level 2 database, then surface heat fluxes under two different underlying surfaces were modeled. The results showed that the model works well regarding the simulation of daily surface fluxes and diurnal surface fluxes although these values were underestimated relative to the values observed from eddy-covariance. After validation, evapotranspiration was chosen as the indicator for specific comparison. CLM3.0 showed a better performance in simulating the moisture and evapotranspiration.
机译:陆地表面热量和水通量是土地和大气之间的水和能量循环的关键组成部分。有关这些表面助熔剂的信息可以引导农业生产和环境保护,并管理不同的生态系统来缓解气候变化。这项工作的主要目标是估计表面热量和蒸散散热。为此目的,使用社区陆地模型版本3,从Ameriflux标准化2级数据库中提取大气强制数据和助焊剂观察,然后建模两个不同的下面表面的表面热通量。结果表明,该模型对日本表面助熔剂和昼夜表面助熔剂的模拟有效地效果很好,尽管这些值相对于从涡旋协方差观察到的值低估。验证后,选择蒸散作为特定比较的指标。 CLM3.0在模拟水分和蒸发过程中表现出更好的性能。

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