Hydrologic implications of projected changes in rain-on-snow melt for Great Lakes Basin watersheds

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Abstract - 2  ∘ C have ROS regimes that are resilient to mid-21st century warming projections, but ROS occurrence in areas that have mean combined winter and spring temperatures near the freezing point are sensitive to changing air temperatures. Also, relationships between changes in the timing of ROS melt and water yield endure throughout spring but become weak by summer. As the influence of ROS melt events on hydrological systems is being altered in a changing climate, these conclusions are important to inform adaptive management of freshwater ecosystems and human uses in regions of the globe that are sensitive to changes in ROS events.

Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Hydrologic implications of projected changes in rain-on-snow melt for Great Lakes Basin watersheds ; volume:27 ; number:9 ; year:2023 ; pages:1755-1770 ; extent:16
Hydrology and earth system sciences ; 27, Heft 9 (2023), 1755-1770 (gesamt 16)

Creator: Myers, Daniel T.
Ficklin, Darren L.
Robeson, Scott M.

DOI: 10.5194/hess-27-1755-2023

URN: urn:nbn:de:101:1-2023051104393694841084

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.12.1046, 4:00 AM CET

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Myers, Daniel T.
Ficklin, Darren L.
Robeson, Scott M.

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