Articles | Volume 24, issue 5
https://doi.org/10.5194/hess-24-2609-2020
https://doi.org/10.5194/hess-24-2609-2020
Research article
 | 
20 May 2020
Research article |  | 20 May 2020

Should altitudinal gradients of temperature and precipitation inputs be inferred from key parameters in snow-hydrological models?

Denis Ruelland

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (18 Apr 2020) by Günter Blöschl
AR by Denis Ruelland on behalf of the Authors (19 Apr 2020)  Author's response   Manuscript 
ED: Publish as is (23 Apr 2020) by Günter Blöschl
AR by Denis Ruelland on behalf of the Authors (24 Apr 2020)
Download
Short summary
Interpolation methods accounting for elevation dependency from scattered gauges result in inaccurate inputs for snow-hydrological models. Altitudinal gradients of temperature and precipitation can be successfully inferred using an inverse snow-hydrological modelling approach. This approach can significantly improve the simulation of snow cover and streamflow dynamics through more parsimonious parametrization.