Impacts of snow assimilation on seasonal snow and meteorological forecasts for the Tibetan Plateau
Abstract ∘ E. The higher temperature after snow assimilation, in particular the cold bias reduction after initialization, can be attributed to the effects of a more realistic, decreased snowpack, providing favourable conditions for generating more precipitation. Overall, snow assimilation can improve seasonal forecasts through the interaction between land and atmosphere.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Impacts of snow assimilation on seasonal snow and meteorological forecasts for the Tibetan Plateau ; volume:16 ; number:12 ; year:2022 ; pages:4985-5000 ; extent:16
The Cryosphere ; 16, Heft 12 (2022), 4985-5000 (gesamt 16)
- Creator
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Li, Wei
Chen, Jie
Li, Lu
Orsolini, Yvan J.
Xiang, Yiheng
Senan, Retish
de Rosnay, Patricia
- DOI
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10.5194/tc-16-4985-2022
- URN
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urn:nbn:de:101:1-2022122204305304074823
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:22 AM CEST
Data provider
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Associated
- Li, Wei
- Chen, Jie
- Li, Lu
- Orsolini, Yvan J.
- Xiang, Yiheng
- Senan, Retish
- de Rosnay, Patricia
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