Uncertainty in modelling the detachment of soil by rainfall

In process‐based models of soil erosion, soil detachment by rainfall is commonly modelled as a simple function of rainfall intensity, based on the assumption of a relationship between drop‐size distribution and intensity. Here we show that rainfall kinetic energy (and hence soil detachment) does not...

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Bibliographic Details
Published inEarth surface processes and landforms Vol. 25; no. 7; pp. 723 - 728
Main Authors Parsons, Anthony J., Gadian, Alan M.
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 01.07.2000
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Summary:In process‐based models of soil erosion, soil detachment by rainfall is commonly modelled as a simple function of rainfall intensity, based on the assumption of a relationship between drop‐size distribution and intensity. Here we show that rainfall kinetic energy (and hence soil detachment) does not bear a simple relationship to intensity. For low‐intensity rainfall, observed variations in drop‐size distributions indicate that soil detachment, at a given rainfall intensity, may vary by about a factor of two. Comparable estimates of variation in soil detachment at high rainfall intensity are not possible because of a dearth of observational data on variation in drop‐size distributions in high‐intensity rainfall. Variation in drop‐size distributions in natural rainfall may, therefore, account for a significant component of differences between observed soil detachment and that predicted by models of soil erosion. Copyright © 2000 John Wiley & Sons, Ltd.
Bibliography:istex:5346BDFF203414DB1E1B98EC2356C252205C9122
ArticleID:ESP127
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ISSN:0197-9337
1096-9837
DOI:10.1002/1096-9837(200007)25:7<723::AID-ESP127>3.0.CO;2-X