祁连山北麓黑河流域中下游植被蒸腾（T）逐月模拟数据（2001-2015）是由生态水文耦合模型HEIFLOW模拟得到的。HEIFLOW模型是一个三维分布式生态水文模拟，由一个地表水模型（PRMS）、一个地下水模型（MODFLOW）和几个生态模块组成，能较为完整地描述流域水循环和植被生态过程。生成此数据的建模细节请参考Han et al. (2021)，关于HEIFLOW模型的技术细节请参考Han e
Brief Summary: Soil physics simulations showed water isotope ratios can differ among drainage, mobile and immobile storages due to transport processes alone, but effects were smaller than field data
The ratio of water absorbed by a theoretical plant canopy with a tree rooting distribution or a grass rooting distribution. The ratio is the ratio of total water absorbed across three growing seasons.
