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Volumn 2, Issue , 2005, Pages 237-241

What happens after the catchment caught the storm? Hydrological processes at the small, semi-arid Weatherley catchment, South-Africa

Author keywords

[No Author keywords available]

Indexed keywords

CATCHMENT; HYDROLOGICAL RESPONSE; PRECIPITATION (CLIMATOLOGY); RAINSTORM; RESIDENCE TIME; RUNOFF; SEMIARID REGION; WATER FLOW;

EID: 33748061299     PISSN: 16807340     EISSN: 16807359     Source Type: Journal    
DOI: 10.5194/adgeo-2-237-2005     Document Type: Article
Times cited : (11)

References (16)
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  • 4
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    • Jones, J.A.1
  • 10
    • 0002416686 scopus 로고
    • The precipitation - Runoff modelling system - PRMS
    • edited by: Singh, V. P., Water Resources Publications, Fort Collins, Colorado, USA
    • Leavesley, G. H. and Stannard, L. G.: The precipitation - runoff modelling system - PRMS, in: Computer Models of Watershed Hydrology, edited by: Singh, V. P., Water Resources Publications, Fort Collins, Colorado, USA, 281-310, 1995.
    • (1995) Computer Models of Watershed Hydrology , pp. 281-310
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    • McDonnell, J.J.1
  • 12
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    • Where does water go when it rains? Moving beyond the variable source area concept of rainfall-runoff response
    • McDonnell, J. J.: Where does water go when it rains? Moving beyond the variable source area concept of rainfall-runoff response, Hydrological Processes, 17, 9, 1869-1875, 2003.
    • (2003) Hydrological Processes , vol.17 , Issue.9 , pp. 1869-1875
    • McDonnell, J.J.1
  • 13
    • 0019999075 scopus 로고
    • Subsurface flow velocities through selected forest soils, south island, New Zealand
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  • 14
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    • Effects of experimental uncertainty on the calculation of hillslope flow paths
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  • 15
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    • Hydrological process representation at the meso-scale: The potential of a distributed, conceptual catchment model
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.