Articles | Volume 12, issue 3
https://doi.org/10.5194/tc-12-907-2018
https://doi.org/10.5194/tc-12-907-2018
Research article
 | 
14 Mar 2018
Research article |  | 14 Mar 2018

Near-surface temperature inversion during summer at Summit, Greenland, and its relation to MODIS-derived surface temperatures

Alden C. Adolph, Mary R. Albert, and Dorothy K. Hall

Viewed

Total article views: 3,762 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,397 1,245 120 3,762 403 84 108
  • HTML: 2,397
  • PDF: 1,245
  • XML: 120
  • Total: 3,762
  • Supplement: 403
  • BibTeX: 84
  • EndNote: 108
Views and downloads (calculated since 23 Oct 2017)
Cumulative views and downloads (calculated since 23 Oct 2017)

Viewed (geographical distribution)

Total article views: 3,762 (including HTML, PDF, and XML) Thereof 3,492 with geography defined and 270 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 19 Nov 2024
Download
Short summary
In our studies of surface temperature in Greenland, we found that there can be differences between the temperature of the snow surface and the air directly above, depending on wind speed and incoming solar radiation. We also found that temperature measurements of the snow surface from remote sensing instruments may be more accurate than previously thought. Our results are relevant to studies of climate change in the remote sensing community and in studies of the atmospheric boundary layer.