Cargando…
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...
Autores principales: | Ganeshan, Manisha, Yang, Yuekui, Palm, Stephen. P. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
John Wiley and Sons Inc.
2022
|
Materias: | |
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 |
Ejemplares similares
-
Uranium record from a 3 m snow pit at Dome Argus, East Antarctica
por: Zou, Xiang, et al.
Publicado: (2018) -
Snow Surface Microbiome on the High Antarctic Plateau (DOME C)
por: Michaud, Luigi, et al.
Publicado: (2014) -
Transitions in the wintertime near‐surface temperature inversion at Dome C, Antarctica
por: Baas, Peter, et al.
Publicado: (2019) -
Determination of Cd, Pb, and Cu in the Atmospheric Aerosol of Central East Antarctica at Dome C (Concordia Station)
por: Illuminati, Silvia, et al.
Publicado: (2021) -
Atmosphere‐Snow Exchange Explains Surface Snow Isotope Variability
por: Wahl, S., et al.
Publicado: (2022)