A novel approach to partitioning evapotranspiration into evaporation and transpiration in flooded ecosystems

被引:13
|
作者
Eichelmann, Elke [1 ]
Mantoani, Mauricio C. [1 ,4 ]
Chamberlain, Samuel D. [2 ]
Hemes, Kyle S. [2 ]
Oikawa, Patricia Y. [3 ]
Szutu, Daphne [2 ]
Valach, Alex [2 ,5 ]
Verfaillie, Joseph [2 ]
Baldocchi, Dennis D. [2 ]
机构
[1] Univ Coll Dublin, Sch Biol & Environm Sci, Dublin 4, Ireland
[2] Univ Calif Berkeley, Dept Environm Sci Policy & Management, Berkeley, CA USA
[3] Calif State Univ, Dept Earth & Environm Sci, Hayward, CA USA
[4] Univ Sao Paulo, Inst Astron Geophys & Atmosper Sci IAG, Sao Paulo, Brazil
[5] Agroscope, Climate & Agr Grp, 191 Reckenholzstr, CH-8046 Zurich, Switzerland
基金
欧盟地平线“2020”; 美国农业部;
关键词
artificial neural networks; eddy covariance; latent energy; machine learning; terrestrial water cycle; vapor pressure deficit; wetlands; VAPOR-PRESSURE DEFICIT; LEAF-AREA INDEX; EDDY-COVARIANCE; CARBON-DIOXIDE; INTERANNUAL VARIABILITY; FLUX MEASUREMENTS; WATER; EXCHANGE; CO2; RESPIRATION;
D O I
10.1111/gcb.15974
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
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 R-2 across all sites. The order of variable inclusion (and importance) was: VPD > gap-filled sensible heat flux (H_gf) > air temperature (T-air) > friction velocity (u(*)) > other variables. The model using VPD, H_gf, T-air, and u(*) showed the best performance during validation with independent data and had a mean testing R-2 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.
引用
收藏
页码:990 / 1007
页数:18
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