Spectral Analysis of Hydrological Signals to Estimate Watershed Properties Considering Impacts of Unsaturated Zone by Yunqiu Zhou, Xiuyu Liang, Enze Ma, Kewei Chen, Keith Schilling, Tianyuan Zheng, Yuhu Zheng, You‐Kuan Zhang, Chunmiao Zheng

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A Three‐Stage Partitioning Framework for Modeling Mean Annual Groundwater Evapotranspiration by Fanzhang Zeng, Yu Zhang, Jeffrey S. Geurink, Kshitij Parajuli, Lili Yao, Dingbao Wang

“…In arid regions, the GWET ratio decreases as the parameter ‘a’ increases, mainly because of increased ET from a thicker unsaturated zone in environments with a deeper DWT. GWET ratio increases as parameter ‘b’ increases due to more watershed area with larger available water for GWET. …”
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