Impact of Clouds and Blowing Snow on Surface and Atmospheric Boundary Layer Properties Over Dome C, Antarctica

Clouds and blowing snow (BLSN) occur frequently over Antarctica, where it is critical to understand their feedbacks to surface and atmospheric boundary layer processes. Dome C, an elevated East Antarctic station, dominated by lengthy periods of surface longwave (LW) radiative cooling, is selected to...

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Detalles Bibliográficos
Autores principales: Ganeshan, Manisha, Yang, Yuekui, Palm, Stephen. P.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10078302/
https://www.ncbi.nlm.nih.gov/pubmed/37035762
http://dx.doi.org/10.1029/2022JD036801

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10078302/
https://www.ncbi.nlm.nih.gov/pubmed/37035762
http://dx.doi.org/10.1029/2022JD036801

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