Articles | Volume 13, issue 7
Clim. Past, 13, 833–853, 2017
https://doi.org/10.5194/cp-13-833-2017
Clim. Past, 13, 833–853, 2017
https://doi.org/10.5194/cp-13-833-2017

Research article 13 Jul 2017

Research article | 13 Jul 2017

Modelling firn thickness evolution during the last deglaciation: constraints on sensitivity to temperature and impurities

Camille Bréant et al.

Viewed

Total article views: 1,587 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
914 553 120 1,587 251 74 129
  • HTML: 914
  • PDF: 553
  • XML: 120
  • Total: 1,587
  • Supplement: 251
  • BibTeX: 74
  • EndNote: 129
Views and downloads (calculated since 12 Oct 2016)
Cumulative views and downloads (calculated since 12 Oct 2016)

Viewed (geographical distribution)

Total article views: 1,560 (including HTML, PDF, and XML) Thereof 1,553 with geography defined and 7 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 03 Mar 2021
Download
Short summary
All firn densification models applied to deglaciations show a large disagreement with δ15N measurements at sites in East Antarctica, predicting larger firn thickness during the Last Glacial Maximum, whereas δ15N suggests a reduced firn thickness compared to the Holocene. Here we present modifications, which significantly reduce the model–data mismatch for the gas trapping depth evolution over the last deglaciation at the coldest sites in East Antarctica, to the LGGE firn densification model.