Contrasted land-surface processes along the West African rainfall gradient
Séguis, L
Boulain, N
Cappelaere, B
Cohard, JM
Favreau, G
Galle, S
Guyot, A
Hiernaux, P
Mougin, E
Peugeot, C
Ramier, D
Seghieri, J
Timouk, F
Demarez, V
Demarty, J
Descroix, L
Descloitres, M
Grippa, M
Guichard, F
Kamagaté, B
Kergoat, L
Lebel, T
Le Dantec, V
Le Lay, M
Massuel, S
Trichon, V
- Publication Type:
- Journal Article
- Citation:
- Atmospheric Science Letters, 2011, 12 (1), pp. 31 - 37
- Issue Date:
- 2011-01-01
Closed Access
Filename | Description | Size | |||
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2010005100OK.pdf | 304.95 kB | Adobe PDF |
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Full metadata record
Field | Value | Language |
---|---|---|
dc.contributor.author | Séguis, L | en_US |
dc.contributor.author | Boulain, N | en_US |
dc.contributor.author | Cappelaere, B | en_US |
dc.contributor.author | Cohard, JM | en_US |
dc.contributor.author | Favreau, G | en_US |
dc.contributor.author | Galle, S | en_US |
dc.contributor.author | Guyot, A | en_US |
dc.contributor.author | Hiernaux, P | en_US |
dc.contributor.author | Mougin, E | en_US |
dc.contributor.author | Peugeot, C | en_US |
dc.contributor.author | Ramier, D | en_US |
dc.contributor.author | Seghieri, J | en_US |
dc.contributor.author | Timouk, F | en_US |
dc.contributor.author | Demarez, V | en_US |
dc.contributor.author | Demarty, J | en_US |
dc.contributor.author | Descroix, L | en_US |
dc.contributor.author | Descloitres, M | en_US |
dc.contributor.author | Grippa, M | en_US |
dc.contributor.author | Guichard, F | en_US |
dc.contributor.author | Kamagaté, B | en_US |
dc.contributor.author | Kergoat, L | en_US |
dc.contributor.author | Lebel, T | en_US |
dc.contributor.author | Le Dantec, V | en_US |
dc.contributor.author | Le Lay, M | en_US |
dc.contributor.author | Massuel, S | en_US |
dc.contributor.author | Trichon, V | en_US |
dc.date.issued | 2011-01-01 | en_US |
dc.identifier.citation | Atmospheric Science Letters, 2011, 12 (1), pp. 31 - 37 | en_US |
dc.identifier.uri | http://hdl.handle.net/10453/18055 | |
dc.description.abstract | We review the main results of land-surface studies obtained in the three sites of the long-term observing system AMMA-CATCH. Runoff in the Sahel enhances the variability of energy partitioning between non-infiltrative areas where sensible heat is dominant and infiltrative areas where soil water availability increases the latent flux. In terms of water resources, an increase in runoff over the past 50 years, already reported for the exoreic Sahel, was revealed in the endoreic Sahel. In the Sudanian domain, the subsurface origin of streamflow could explain its decrease over the same period. Copyright © 2011 Royal Meteorological Society. | en_US |
dc.relation.ispartof | Atmospheric Science Letters | en_US |
dc.relation.isbasedon | 10.1002/asl.327 | en_US |
dc.subject.classification | Meteorology & Atmospheric Sciences | en_US |
dc.title | Contrasted land-surface processes along the West African rainfall gradient | en_US |
dc.type | Journal Article | |
utslib.citation.volume | 1 | en_US |
utslib.citation.volume | 12 | en_US |
utslib.for | 0401 Atmospheric Sciences | en_US |
pubs.embargo.period | Not known | en_US |
pubs.organisational-group | /University of Technology Sydney | |
pubs.organisational-group | /University of Technology Sydney/Faculty of Science | |
utslib.copyright.status | closed_access | |
pubs.issue | 1 | en_US |
pubs.publication-status | Published | en_US |
pubs.volume | 12 | en_US |
Abstract:
We review the main results of land-surface studies obtained in the three sites of the long-term observing system AMMA-CATCH. Runoff in the Sahel enhances the variability of energy partitioning between non-infiltrative areas where sensible heat is dominant and infiltrative areas where soil water availability increases the latent flux. In terms of water resources, an increase in runoff over the past 50 years, already reported for the exoreic Sahel, was revealed in the endoreic Sahel. In the Sudanian domain, the subsurface origin of streamflow could explain its decrease over the same period. Copyright © 2011 Royal Meteorological Society.
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