The Impacts of Changing Winter Warm Spells on Snow Ablation Over Western North America

An increase in winter air temperature can amplify snowmelt and sublimation in mountain regions with implications to water resources and ecological systems. Winter Warm Spells (WWS) are defined as a winter period (December to February, DJF) of at least 3 consecutive days with daily maximum temperatur...

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Veröffentlicht in:	Water resources research 2024-05, Vol.60 (5), p.n/a
Hauptverfasser:	Scaff, Lucia, Krogh, Sebastian A., Musselman, Keith, Harpold, Adrian, Li, Yanping, Lillo‐Saavedra, Mario, Oyarzún, Ricardo, Rasmussen, Roy
Format:	Artikel
Sprache:	eng
Schlagworte:	Ablation Air temperature Arid regions Arid zones Atmospheric models Climate Climate models cold convection‐permitting simulation Daily temperatures Energy balance Future climates Mathematical models Maximum temperatures Mountain regions Mountains North America Numerical models Regions Reservoir operation Reservoirs Security Snow snowapack ablation Snowmelt Snowpack Statistical analysis Sublimation Temperature anomalies warmer climate water Water resources Water security Water supply Western North American mountains Winter Winter temperatures Winter Warm Spells
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