Sensitivity of the West African hydrological cycle in ORCHIDEE to infiltration processes

The aim of this article is to test the sensitivity of the West African hydrological cycle to infiltration processes and to river reinfiltration pathways. This is done through sensitivity experiments to both inputs and paramterization settings of the ORCHIDEE Land-Surface Model. The parameterizations...

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Main Authors: T. d'Orgeval, J. Polcher, P. de Rosnay
Format: Article
Language:English
Published: Copernicus Publications 2008-12-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/12/1387/2008/hess-12-1387-2008.pdf
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spelling doaj-9d688f5d22f04594bb5e03f69cd32fe32020-11-24T23:53:55ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382008-12-0112613871401Sensitivity of the West African hydrological cycle in ORCHIDEE to infiltration processesT. d'OrgevalJ. PolcherP. de RosnayThe aim of this article is to test the sensitivity of the West African hydrological cycle to infiltration processes and to river reinfiltration pathways. This is done through sensitivity experiments to both inputs and paramterization settings of the ORCHIDEE Land-Surface Model. The parameterizations to take into account the effects of flat areas, ponds and floodplains on surface infiltration, and the effect of roots and deep-soil compactness on infiltration are first described. The sensitivity analysis to parameterization settings shows that the surface infiltration processes have a stronger impact in the soudano-sahelian region and more generally in semi-arid African regions, whereas the rootzone and deep-soil infiltration also play a role in the guinean and intermediate regions between arid and humid ones. In the equatorial and semi-humid regions, infiltration processes generally play a minor role. The infiltration parameterizations may explain part of the difference between simulated and observed river discharge in semi-arid and intermediate basins. The sensitivity analysis to the Land-Surface Model inputs shows that different sources of uncertainty might also explain part of the error. Indeed, the precipitation forcing in the whole West African region, the long-term storage in the soudano-sahelian region, the soil types in the guinean region and the vegetation types in the equatorial region are significant sources of errors. Therefore, observations and analyses of small scale infiltration processes as well as continuous measurements of river discharges in West Africa are essential to ensure the reliability of future calibration for the infiltration parameterizations. http://www.hydrol-earth-syst-sci.net/12/1387/2008/hess-12-1387-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. d'Orgeval
J. Polcher
P. de Rosnay
spellingShingle T. d'Orgeval
J. Polcher
P. de Rosnay
Sensitivity of the West African hydrological cycle in ORCHIDEE to infiltration processes
Hydrology and Earth System Sciences
author_facet T. d'Orgeval
J. Polcher
P. de Rosnay
author_sort T. d'Orgeval
title Sensitivity of the West African hydrological cycle in ORCHIDEE to infiltration processes
title_short Sensitivity of the West African hydrological cycle in ORCHIDEE to infiltration processes
title_full Sensitivity of the West African hydrological cycle in ORCHIDEE to infiltration processes
title_fullStr Sensitivity of the West African hydrological cycle in ORCHIDEE to infiltration processes
title_full_unstemmed Sensitivity of the West African hydrological cycle in ORCHIDEE to infiltration processes
title_sort sensitivity of the west african hydrological cycle in orchidee to infiltration processes
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2008-12-01
description The aim of this article is to test the sensitivity of the West African hydrological cycle to infiltration processes and to river reinfiltration pathways. This is done through sensitivity experiments to both inputs and paramterization settings of the ORCHIDEE Land-Surface Model. The parameterizations to take into account the effects of flat areas, ponds and floodplains on surface infiltration, and the effect of roots and deep-soil compactness on infiltration are first described. The sensitivity analysis to parameterization settings shows that the surface infiltration processes have a stronger impact in the soudano-sahelian region and more generally in semi-arid African regions, whereas the rootzone and deep-soil infiltration also play a role in the guinean and intermediate regions between arid and humid ones. In the equatorial and semi-humid regions, infiltration processes generally play a minor role. The infiltration parameterizations may explain part of the difference between simulated and observed river discharge in semi-arid and intermediate basins. The sensitivity analysis to the Land-Surface Model inputs shows that different sources of uncertainty might also explain part of the error. Indeed, the precipitation forcing in the whole West African region, the long-term storage in the soudano-sahelian region, the soil types in the guinean region and the vegetation types in the equatorial region are significant sources of errors. Therefore, observations and analyses of small scale infiltration processes as well as continuous measurements of river discharges in West Africa are essential to ensure the reliability of future calibration for the infiltration parameterizations.
url http://www.hydrol-earth-syst-sci.net/12/1387/2008/hess-12-1387-2008.pdf
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