机译:White方法在地下水变化剧烈的情况下估算地下水蒸发蒸腾量的性能
Chinese Academy of Sciences Key Laboratory of Ecosystem Network Observation and Modeling Institute of Geographical Sciences and Natural Resources Research Beijing China;
University of Chinese Academy of Sciences Beijing China;
Chinese Academy of Sciences Key Laboratory of Ecosystem Network Observation and Modeling Institute of Geographical Sciences and Natural Resources Research Beijing China;
Chinese Academy of Sciences Key Laboratory of Ecosystem Network Observation and Modeling Institute of Geographical Sciences and Natural Resources Research Beijing China;
Northwest AF University College of Natural Resources and Environments Yangling China;
Chinese Academy of Sciences Key Laboratory of Ecosystem Network Observation and Modeling Institute of Geographical Sciences and Natural Resources Research Beijing China;
University of Chinese Academy of Sciences Beijing China;
groundwater evapotranspiration; the White method; specific yield; recharge rate of groundwater; desert riparian forest; deep groundwater depth;
机译:干旱和半干旱地区利用日地下水位波动估算蒸散量的方法的比较和改进
机译:蒸散和浅层地下水波动:基于傅立叶的White方法改进
机译:再次利用White方法估算地下水的蒸散量:考虑日落和日出时间
机译:使用校正后的每日地下水位波动在浅层地下水位区域估算次日蒸散量
机译:开发一种新的方法来估算地下水的蒸散量。
机译:总地下水压力框架中全球地下水储量估算的不确定性
机译:在深部和波动的地下水条件下估算地下水蒸散量的White方法的性能
机译:储存库周围的地下水运动。区域地下水分析。第1部分。初始条件。第2部分。长期剩余条件