Simulation of daily discharges for the upper Durance catchment (French Alps) using subgrid parameterization for topography and a forest canopy climate model
Identifieur interne : 000D01 ( France/Analysis ); précédent : 000D00; suivant : 000D02Simulation of daily discharges for the upper Durance catchment (French Alps) using subgrid parameterization for topography and a forest canopy climate model
Auteurs : Ulrich Strasser [Allemagne] ; Pierre Etchevers [France]Source :
- Hydrological Processes [ 0885-6087 ] ; 2005-08-15.
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Abstract
This study describes the application of the coupled SAFRAN (meteorological variables), ISBA (soil–vegetation–atmosphere transfer) and CROCUS (snow cover evolution) models to simulate daily discharges for the upper Durance catchment (French Alps) from 1981 to 1994. The results are validated by comparison with measurements at three gauging stations located in the watershed. Previous investigations have shown a remarkable overestimation of the spring flood peak generated by the modelled snowmelt. It could be significantly improved by increasing the model resolution from 8 km to 1 km, thus more precisely considering the elevation‐dependent snowmelt process. However, it is also possible to use subgrid parameterizations at the coarse grid resolution to improve simulations. This paper investigates the influence of a subgrid parameterization for topography, a subgrid parameterization for the snow cover in a forest canopy and a combination of the two on the simulated spring flood peak. Results show a significant improvement in the simulations by both subgrid parameterizations, in particular by their combination: the Nash–Sutcliffe efficiency of the daily discharges is improved from 0·73 (original experiment) to 0·77 (subgrid topography), to 0·75 (forest) and to 0·78 (combination of subgrid topography and forest). Copyright © 2005 John Wiley & Sons, Ltd.
Url:
DOI: 10.1002/hyp.5889
Affiliations:
- Allemagne, France
- Bavière, District de Haute-Bavière
- Grenoble, Munich, Saint-Martin-d'Hères
- Université Louis-et-Maximilien de Munich
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Process.</title><idno type="ISSN">0885-6087</idno><idno type="eISSN">1099-1085</idno><imprint><publisher>John Wiley & Sons, Ltd.</publisher><pubPlace>Chichester, UK</pubPlace><date type="published" when="2005-08-15">2005-08-15</date><biblScope unit="volume">19</biblScope><biblScope unit="issue">12</biblScope><biblScope unit="page" from="2361">2361</biblScope><biblScope unit="page" to="2373">2373</biblScope></imprint><idno type="ISSN">0885-6087</idno></series><idno type="istex">BA848EA0FF7D0880A4FD8F82FF367CE429DA79A6</idno><idno type="DOI">10.1002/hyp.5889</idno><idno type="ArticleID">HYP5889</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0885-6087</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>daily discharge</term><term>forest climate</term><term>interception</term><term>snowmelt</term><term>spring flood</term><term>subgrid parameterization</term><term>topography</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">This study describes the application of the coupled SAFRAN (meteorological variables), ISBA (soil–vegetation–atmosphere transfer) and CROCUS (snow cover evolution) models to simulate daily discharges for the upper Durance catchment (French Alps) from 1981 to 1994. The results are validated by comparison with measurements at three gauging stations located in the watershed. Previous investigations have shown a remarkable overestimation of the spring flood peak generated by the modelled snowmelt. It could be significantly improved by increasing the model resolution from 8 km to 1 km, thus more precisely considering the elevation‐dependent snowmelt process. However, it is also possible to use subgrid parameterizations at the coarse grid resolution to improve simulations. This paper investigates the influence of a subgrid parameterization for topography, a subgrid parameterization for the snow cover in a forest canopy and a combination of the two on the simulated spring flood peak. Results show a significant improvement in the simulations by both subgrid parameterizations, in particular by their combination: the Nash–Sutcliffe efficiency of the daily discharges is improved from 0·73 (original experiment) to 0·77 (subgrid topography), to 0·75 (forest) and to 0·78 (combination of subgrid topography and forest). Copyright © 2005 John Wiley & Sons, Ltd.</div></front></TEI><affiliations><list><country><li>Allemagne</li><li>France</li></country><region><li>Bavière</li><li>District de Haute-Bavière</li></region><settlement><li>Grenoble</li><li>Munich</li><li>Saint-Martin-d'Hères</li></settlement><orgName><li>Université Louis-et-Maximilien de Munich</li></orgName></list><tree><country name="Allemagne"><region name="Bavière"><name sortKey="Strasser, Ulrich" sort="Strasser, Ulrich" uniqKey="Strasser U" first="Ulrich" last="Strasser">Ulrich Strasser</name></region></country><country name="France"><noRegion><name sortKey="Etchevers, Pierre" sort="Etchevers, Pierre" uniqKey="Etchevers P" first="Pierre" last="Etchevers">Pierre Etchevers</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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