Department of Earth Ocean and Atmospheric Sciences (EOAS), The University of British Columbia, Vancouver, Canada
Rachel H. White
Department of Earth Ocean and Atmospheric Sciences (EOAS), The University of British Columbia, Vancouver, Canada
Mekdes Ayalew Tessema
Department of Earth Ocean and Atmospheric Sciences (EOAS), The University of British Columbia, Vancouver, Canada
Viewed
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 4,602 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
3,555
961
86
4,602
84
99
151
HTML: 3,555
PDF: 961
XML: 86
Total: 4,602
Supplement: 84
BibTeX: 99
EndNote: 151
Views and downloads (calculated since 13 Jun 2023)
Cumulative views and downloads
(calculated since 13 Jun 2023)
Total article views: 3,645 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,620
939
86
3,645
78
93
145
HTML: 2,620
PDF: 939
XML: 86
Total: 3,645
Supplement: 78
BibTeX: 93
EndNote: 145
Views and downloads (calculated since 02 Jan 2024)
Cumulative views and downloads
(calculated since 02 Jan 2024)
Total article views: 957 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
935
22
0
957
6
6
HTML: 935
PDF: 22
XML: 0
Total: 957
BibTeX: 6
EndNote: 6
Views and downloads (calculated since 13 Jun 2023)
Cumulative views and downloads
(calculated since 13 Jun 2023)
Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 4,602 (including HTML, PDF, and XML)
Thereof 4,498 with geography defined
and 104 with unknown origin.
Total article views: 3,645 (including HTML, PDF, and XML)
Thereof 3,546 with geography defined
and 99 with unknown origin.
Total article views: 957 (including HTML, PDF, and XML)
Thereof 952 with geography defined
and 5 with unknown origin.
Our study increases our confidence in using reanalysis data for reconstructions of past glacier melt and in using dynamical downscaling for long-term simulations from global climate models to project glacier melt. We find that the surface energy balance model, forced with reanalysis and dynamically downscaled reanalysis data, yields <10 % difference in the modeled total melt energy when compared to the same model being forced with observations at our glacier sites in western Canada.
Our study increases our confidence in using reanalysis data for reconstructions of past glacier...
