蒸散发总量 total evapotranspiration
蒸发光散射质量检测器 Evaporative Light-Scatting Mass Detector
蒸发蒸散总量 Evapo-transpiration
The total evapotranspiration in the Tarim River basin in 2000 decreased by 6.80×104 m3 compared with in 1985,because the total daily evapotranspiration in the middle and lower reaches decreased while the upper reaches increased by 3.02×105 m3.
2000年塔里木河干流区日总蒸散发比1985年减少了6.80×104m3,原因是中游和下游日总蒸散发减小,而上游日总蒸散发量却增加了3.02×105m3。
参考来源 - 基于遥感和SEBAL模型的塔里木河干流区蒸散发估算The latent heat flux is minus（-95.67～0W/m2）in Xi Juyan Lake. The mean of evapotranspiration is 1.61mm in Sept.12,2003 in study area.
研究区2003年9月12日的蒸散发量集中在1～2mm内,均值为1.61mm。
参考来源 - 黑河下游地下水波动带生态需水量空间分布研究·2,447,543篇论文数据，部分数据来源于NoteExpress
介绍了佳木斯市精测研究区蒸散发量的各种计算方法。
Various calculating methods of evaporation for the precision survey research area of Jiamusi city were introduced.
结合气象观测数据反演作物系数，最后计算月蒸散发量。
With aid of observed climate data, FAO Penman-Monteith equaption is used to calculate the reference ET and crop coefficient.
用水量平衡法计算的流域多年平均实际蒸散发量对估算结果进行检验。
Actual evapotranspiration was reckoned by model and results were verified by explored the secular annual mean basin actual evapotranspiration which was calculated from water model.
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