Runoff curve numbers for steep hillslopes with natural vegetation in semi-arid tropical highlands, northern Ethiopia

Daily runoff from 27 plots (5 m × 2 m) recorded during two rainy seasons in the Tigray highlands (Ethiopia) were analysed together with daily rainfall to calculate runoff curve numbers for hillslopes covered by semi-natural vegetation in varying stages of vegetation restoration. Curve number model parameters were derived using a least squares fitting procedure on the collected rainfall-runoff datasets. Curve numbers varied from 29 to 97. Land use type was an important explanatory factor for the variation in curve numbers, whereas hydrologic soil group was not. Curve numbers were negatively correlated with vegetation cover. Taking into account antecedent soil moisture conditions did not improve runoff prediction using the curve number method. As runoff prediction was less accurate in areas with low curve numbers, two separate regression functions relating curve numbers with vegetation cover were proposed for different land use types.

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Main Authors: Descheemaeker, Katrien, Poesen, J., Borselli, L., Nyssen, Jan, Raes, Dirk, Haile, M., Muys, B., Deckers, J.
Format: Journal Article biblioteca
Language:English
Published: Wiley 2008-09-30
Subjects:rainwater, vegetation,
Online Access:https://hdl.handle.net/10568/2123
https://doi.org/10.1002/hyp.7011
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spelling dig-cgspace-10568-21232023-12-27T19:30:10Z Runoff curve numbers for steep hillslopes with natural vegetation in semi-arid tropical highlands, northern Ethiopia Descheemaeker, Katrien Poesen, J. Borselli, L. Nyssen, Jan Raes, Dirk Haile, M. Muys, B. Deckers, J. rainwater vegetation Daily runoff from 27 plots (5 m × 2 m) recorded during two rainy seasons in the Tigray highlands (Ethiopia) were analysed together with daily rainfall to calculate runoff curve numbers for hillslopes covered by semi-natural vegetation in varying stages of vegetation restoration. Curve number model parameters were derived using a least squares fitting procedure on the collected rainfall-runoff datasets. Curve numbers varied from 29 to 97. Land use type was an important explanatory factor for the variation in curve numbers, whereas hydrologic soil group was not. Curve numbers were negatively correlated with vegetation cover. Taking into account antecedent soil moisture conditions did not improve runoff prediction using the curve number method. As runoff prediction was less accurate in areas with low curve numbers, two separate regression functions relating curve numbers with vegetation cover were proposed for different land use types. 2008-09-30 2010-08-02T13:29:07Z 2010-08-02T13:29:07Z Journal Article Descheemaeker, K.; Poesen, J.; Borselli, L.; Nyssen, J.; Raes, D.; Haile, M.; Muys, B.; Deckers, J. 2008. Runoff curve numbers for steep hillslopes with natural vegetation in semi-arid tropical highlands, northern Ethiopia. Hydrological Processes 22(20):4097-4105. 0885-6087 1099-1085 https://hdl.handle.net/10568/2123 https://doi.org/10.1002/hyp.7011 en Copyrighted; all rights reserved Limited Access p. 4097-4105 Wiley Hydrological Processes
institution CGIAR
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-cgspace
tag biblioteca
region Europa del Oeste
libraryname Biblioteca del CGIAR
language English
topic rainwater
vegetation
rainwater
vegetation
spellingShingle rainwater
vegetation
rainwater
vegetation
Descheemaeker, Katrien
Poesen, J.
Borselli, L.
Nyssen, Jan
Raes, Dirk
Haile, M.
Muys, B.
Deckers, J.
Runoff curve numbers for steep hillslopes with natural vegetation in semi-arid tropical highlands, northern Ethiopia
description Daily runoff from 27 plots (5 m × 2 m) recorded during two rainy seasons in the Tigray highlands (Ethiopia) were analysed together with daily rainfall to calculate runoff curve numbers for hillslopes covered by semi-natural vegetation in varying stages of vegetation restoration. Curve number model parameters were derived using a least squares fitting procedure on the collected rainfall-runoff datasets. Curve numbers varied from 29 to 97. Land use type was an important explanatory factor for the variation in curve numbers, whereas hydrologic soil group was not. Curve numbers were negatively correlated with vegetation cover. Taking into account antecedent soil moisture conditions did not improve runoff prediction using the curve number method. As runoff prediction was less accurate in areas with low curve numbers, two separate regression functions relating curve numbers with vegetation cover were proposed for different land use types.
format Journal Article
topic_facet rainwater
vegetation
author Descheemaeker, Katrien
Poesen, J.
Borselli, L.
Nyssen, Jan
Raes, Dirk
Haile, M.
Muys, B.
Deckers, J.
author_facet Descheemaeker, Katrien
Poesen, J.
Borselli, L.
Nyssen, Jan
Raes, Dirk
Haile, M.
Muys, B.
Deckers, J.
author_sort Descheemaeker, Katrien
title Runoff curve numbers for steep hillslopes with natural vegetation in semi-arid tropical highlands, northern Ethiopia
title_short Runoff curve numbers for steep hillslopes with natural vegetation in semi-arid tropical highlands, northern Ethiopia
title_full Runoff curve numbers for steep hillslopes with natural vegetation in semi-arid tropical highlands, northern Ethiopia
title_fullStr Runoff curve numbers for steep hillslopes with natural vegetation in semi-arid tropical highlands, northern Ethiopia
title_full_unstemmed Runoff curve numbers for steep hillslopes with natural vegetation in semi-arid tropical highlands, northern Ethiopia
title_sort runoff curve numbers for steep hillslopes with natural vegetation in semi-arid tropical highlands, northern ethiopia
publisher Wiley
publishDate 2008-09-30
url https://hdl.handle.net/10568/2123
https://doi.org/10.1002/hyp.7011
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