蒸散量
蒸腾作用
蒸汽压差
涡度相关法
环境科学
大气科学
显热
航程(航空)
鲍恩比率
植被(病理学)
降水
湿地
气候变化
焊剂(冶金)
水文学(农业)
生态系统
生态学
气象学
光合作用
地理
植物
化学
工程类
病理
地质学
复合材料
生物
有机化学
岩土工程
材料科学
医学
作者
Elke Eichelmann,Maurício Cruz Mantoani,Samuel D. Chamberlain,Kyle S. Hemes,Patricia Y. Oikawa,Daphne Szutu,Alex Valach,Joseph Verfaillie,Dennis Baldocchi
摘要
Reliable partitioning of micrometeorologically measured evapotranspiration (ET) into evaporation (E) and transpiration (T) would greatly enhance our understanding of the water cycle and its response to climate change related shifts in local-to-regional climate conditions and rising global levels of vapor pressure deficit (VPD). While some methods on ET partitioning have been developed, their underlying assumptions make them difficult to apply more generally, especially in sites with large contributions of E. Here, we report a novel ET partitioning method using artificial neural networks (ANNs) in combination with a range of environmental input variables to predict daytime E from nighttime ET measurements. The study uses eddy covariance data from four restored wetlands in the Sacramento-San Joaquin Delta, California, USA, as well as leaf-level T data for validation. The four wetlands vary in their vegetation make-up and structure, representing a range of ET conditions. The ANNs were built with increasing complexity by adding the input variable that resulted in the next highest average value of model testing R2 across all sites. The order of variable inclusion (and importance) was: VPD > gap-filled sensible heat flux (H_gf) > air temperature (Tair ) > friction velocity (u∗ ) > other variables. The model using VPD, H_gf, Tair , and u∗ showed the best performance during validation with independent data and had a mean testing R2 value of 0.853 (averaged across all sites, range from 0.728 to 0.910). In comparison to other methods, our ANN method generated T/ET partitioning results which were more consistent with CO2 exchange data especially for more heterogeneous sites with large E contributions. Our method improves the understanding of T/ET partitioning. While it may be particularly suited to flooded ecosystems, it can also improve T/ET partitioning in other systems, increasing our knowledge of the global water cycle and ecosystem functioning.
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