Diurnal Streamflow Variability
Diurnal Streamflow Variability is a hydrological phenomenon characterized by daily fluctuations in stream discharge resulting from rhythmic processes such as snowmelt, evapotranspiration, or groundwater-surface water interactions that modulate flow magnitude within a 24-hour cycle.
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2.5K
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82
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2017–2026
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United States Geological Survey
Reston, United States
3 h-index
4 publications
451 citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
2 h-index
2 publications
171 citations

University of British Columbia
Vancouver, Canada
2 h-index
3 publications
217 citations
University of Wyoming
Laramie, United States
2 h-index
8 publications
111 citations

Scripps Institution of Oceanography
La Jolla, United States
2 h-index
5 publications
618 citations
Austral University of Chile
Valdivia, Chile
2 h-index
5 publications
157 citations

Old Dominion University
Norfolk, United States
2 h-index
4 publications
360 citations
Battelle
Geneva, Switzerland
1 h-index
4 publications
64 citations
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11 publications · 424 citations
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8 publications · 938 citations
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