Climate-driven Recharge Variability
Climate-Driven Recharge Variability is a hydrological phenomenon characterized by fluctuations in groundwater recharge rates attributable to temporal and spatial variations in climatic forcings such as precipitation, temperature, and evapotranspiration.
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Andreas Hartmann, Tom Gleeson, Yoshihide Wada et al. · Proceedings of the National Academy of Sciences · 2017 · 264 citations · Full text
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United States Geological Survey
Reston, United States
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13 publications
3.1K citations
CSIRO Land and Water
Canberra, Australia
3 h-index
14 publications
1.5K citations

Centre National de la Recherche Scientifique
Paris, France
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6 publications
510 citations

Chinese Academy of Sciences
Beijing, China
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10 publications
297 citations
University of Arizona
Tucson, United States
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7 publications
2.1K citations

Commonwealth Scientific and Industrial Research Organisation
Canberra, Australia
3 h-index
13 publications
1.3K citations
International Institute for Applied Systems Analysis
Laxenburg, Austria
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2 publications
281 citations

UNSW Sydney
Sydney, Australia
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2 publications
519 citations
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