The Cryosphere
The Cryosphere
TC
Articles | Volume 18, issue 4
Articles | Volume 18, issue 4
https://doi.org/10.5194/tc-18-1835-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-18-1835-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 18, issue 4
Research article
 | 
18 Apr 2024
Research article |  | 18 Apr 2024

Validation of pan-Arctic soil temperatures in modern reanalysis and data assimilation systems

Tyler C. Herrington, Christopher G. Fletcher, and Heather Kropp

Viewed

Total article views: 2,975 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,141 714 120 2,975 186 106 124
  • HTML: 2,141
  • PDF: 714
  • XML: 120
  • Total: 2,975
  • Supplement: 186
  • BibTeX: 106
  • EndNote: 124
Views and downloads (calculated since 25 Jan 2022)
Cumulative views and downloads (calculated since 25 Jan 2022)

Viewed (geographical distribution)

Total article views: 2,975 (including HTML, PDF, and XML) Thereof 2,873 with geography defined and 102 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 24 Oct 2025
Download
Short summary
Here we validate soil temperatures from eight reanalysis products across the pan-Arctic and compare their performance to a newly calculated ensemble mean soil temperature product. We find that most product soil temperatures have a relatively large RMSE of 2–9 K. It is found that the ensemble mean product outperforms individual reanalysis products. Therefore, we recommend the ensemble mean soil temperature product for the validation of climate models and for input to hydrological models.
Read more
Share