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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Published in | Earth surface processes and landforms Vol. 25; no. 7; pp. 723 - 728 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Chichester, UK
John Wiley & Sons, Ltd
01.07.2000
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Subjects | |
Online Access | Get full text |
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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. |
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Bibliography: | istex:5346BDFF203414DB1E1B98EC2356C252205C9122 ArticleID:ESP127 ark:/67375/WNG-S4MJ99LH-J ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0197-9337 1096-9837 |
DOI: | 10.1002/1096-9837(200007)25:7<723::AID-ESP127>3.0.CO;2-X |