Articles | Volume 14, issue 2
https://doi.org/10.5194/tc-14-539-2020
https://doi.org/10.5194/tc-14-539-2020
Research article
 | 
11 Feb 2020
Research article |  | 11 Feb 2020

Melt in Antarctica derived from Soil Moisture and Ocean Salinity (SMOS) observations at L band

Marion Leduc-Leballeur, Ghislain Picard, Giovanni Macelloni, Arnaud Mialon, and Yann H. Kerr

Viewed

Total article views: 2,736 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,808 822 106 2,736 93 91
  • HTML: 1,808
  • PDF: 822
  • XML: 106
  • Total: 2,736
  • BibTeX: 93
  • EndNote: 91
Views and downloads (calculated since 20 Sep 2019)
Cumulative views and downloads (calculated since 20 Sep 2019)

Viewed (geographical distribution)

Total article views: 2,736 (including HTML, PDF, and XML) Thereof 2,402 with geography defined and 334 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 25 Dec 2024
Download
Short summary
To study the coast and ice shelves affected by melt in Antarctica during the austral summer, we exploited the 1.4 GHz radiometric satellite observations. We showed that this frequency provides additional information on melt occurrence and on the location of the water in the snowpack compared to the 19 GHz observations. This opens an avenue for improving the melting season monitoring with a combination of both frequencies and exploring the possibility of deep-water detection in the snowpack.