Articles | Volume 22, issue 4
https://doi.org/10.5194/hess-22-2211-2018
https://doi.org/10.5194/hess-22-2211-2018
Technical note
 | 
09 Apr 2018
Technical note |  | 09 Apr 2018

Technical note: Representing glacier geometry changes in a semi-distributed hydrological model

Jan Seibert, Marc J. P. Vis, Irene Kohn, Markus Weiler, and Kerstin Stahl

Viewed

Total article views: 5,716 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,557 1,950 209 5,716 151 213
  • HTML: 3,557
  • PDF: 1,950
  • XML: 209
  • Total: 5,716
  • BibTeX: 151
  • EndNote: 213
Views and downloads (calculated since 30 Mar 2017)
Cumulative views and downloads (calculated since 30 Mar 2017)

Viewed (geographical distribution)

Total article views: 5,716 (including HTML, PDF, and XML) Thereof 5,503 with geography defined and 213 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 06 Dec 2025
Download
Short summary
In many glacio-hydrological models glacier areas are assumed to be constant over time, which is a crucial limitation. Here we describe a novel approach to translate mass balances as simulated by the (glacio)hydrological model into glacier area changes. We combined the Δh approach of Huss et al. (2010) with the bucket-type model HBV and introduced a lookup table approach, which also allows periods with advancing glaciers to be represented, which is not possible with the original Huss method.
Share