Articles | Volume 16, issue 1
https://doi.org/10.5194/tc-16-103-2022
https://doi.org/10.5194/tc-16-103-2022
Research article
 | 
13 Jan 2022
Research article |  | 13 Jan 2022

An empirical algorithm to map perennial firn aquifers and ice slabs within the Greenland Ice Sheet using satellite L-band microwave radiometry

Julie Z. Miller, Riley Culberg, David G. Long, Christopher A. Shuman, Dustin M. Schroeder, and Mary J. Brodzik

Viewed

Total article views: 3,399 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,335 979 85 3,399 72 61
  • HTML: 2,335
  • PDF: 979
  • XML: 85
  • Total: 3,399
  • BibTeX: 72
  • EndNote: 61
Views and downloads (calculated since 30 Apr 2021)
Cumulative views and downloads (calculated since 30 Apr 2021)

Viewed (geographical distribution)

Total article views: 3,399 (including HTML, PDF, and XML) Thereof 3,257 with geography defined and 142 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 29 Jun 2024
Download
Short summary
We use L-band brightness temperature imagery from NASA's Soil Moisture Active Passive (SMAP) satellite to map the extent of perennial firn aquifer and ice slab areas within the Greenland Ice Sheet. As Greenland's climate continues to warm and seasonal surface melting increases in extent, intensity, and duration, quantifying the possible rapid expansion of perennial firn aquifers and ice slab areas has significant implications for understanding the stability of the Greenland Ice Sheet.