Alpine Evapotranspiration
Alpine Evapotranspiration is a hydrological process variable denoting the combined flux of water vapor transferred to the atmosphere through evaporation from snow, ice, soil, and open water surfaces and transpiration from alpine vegetation, specifically occurring within high-elevation mountain environments above the tree line where climatic conditions are characterized by low temperatures, high solar radiation, and seasonal snow cover.
71
Publications
3.2K
Citations
296
Authors
121
Institutions
Publications per year
2017–2026
24
Parents
71
Giovanni Ravazzani, Chiara Corbari, Stefano Morella et al. · Journal of Irrigation and Drainage Engineering · 2011 · 150 citations · Full text
Natural Resources, Hydrology, Water Resources Management +16
Markus Hollaus, Wolfgang Wagner, C. Eberhöfer et al. · ISPRS Journal of Photogrammetry and Remote Sensing · 2006 · 147 citations
1–5 of 71
296
4
h-index
4
h-index
4
h-index
4
h-index
4
h-index
1–5 of 296
121

Chinese Academy of Sciences
Beijing, China
16 h-index
105 publications
4.4K citations
University of Chinese Academy of Sciences
Beijing, China
8 h-index
17 publications
1.1K citations
Northwest Institute of Eco-Environment and Resources
Lanzhou, China
8 h-index
27 publications
800 citations
Institute of Geographic Sciences and Natural Resources Research
Beijing, China
6 h-index
13 publications
265 citations

Beijing Normal University
Beijing, China
5 h-index
23 publications
655 citations
Institute of Tibetan Plateau Research
Beijing, China
5 h-index
17 publications
1.4K citations
Center for Excellence in Tibetan Plateau Earth Sciences
Beijing, China
4 h-index
5 publications
355 citations
Northwest University
Xi'an, China
4 h-index
4 publications
166 citations
1–8 of 121
8 publications · 368 citations
8
h-index
5 publications · 148 citations
5
h-index
4 publications · 316 citations
4
h-index
3 publications · 217 citations
3
h-index
3 publications · 69 citations
3
h-index
1–5