Articles | Volume 10, issue 1
https://doi.org/10.5194/tc-10-103-2016
https://doi.org/10.5194/tc-10-103-2016
Research article
 | 
18 Jan 2016
Research article |  | 18 Jan 2016

Feasibility of improving a priori regional climate model estimates of Greenland ice sheet surface mass loss through assimilation of measured ice surface temperatures

M. Navari, S. A. Margulis, S. M. Bateni, M. Tedesco, P. Alexander, and X. Fettweis

Viewed

Total article views: 3,040 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,628 1,215 197 3,040 227 203
  • HTML: 1,628
  • PDF: 1,215
  • XML: 197
  • Total: 3,040
  • BibTeX: 227
  • EndNote: 203
Views and downloads (calculated since 19 Jun 2015)
Cumulative views and downloads (calculated since 19 Jun 2015)

Cited

Saved (preprint)

Latest update: 02 Nov 2024
Download
Short summary
An ensemble batch smoother was used to assess the feasibility of generating a reanalysis estimate of the Greenland ice sheet (GrIS) surface mass fluxes (SMF) via integrating measured ice surface temperatures with a regional climate model estimate. The results showed that assimilation of IST were able to overcome uncertainties in meteorological forcings that drive the GrIS surface processes. We showed that the proposed methodology is able to generate posterior reanalysis estimates of the SMF.