Yield of sediment in relation to mean annual precipitation
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Abstract
Effective mean annual precipitation is related to sediment yield from drainage basins throughout the climatic regions of the United States. Sediment yield is a maximum at about 10 to 14 inches of precipitation, decreasing sharply on both sides of this maximum in one case owing to a deficiency of runoff and in the other to increased density of vegetation. Data are presented illustrating the increase in bulk density of vegetation with increased annual precipitation and the relation of relative erosion to vegetative density. It is suggested that the effect of a climatic change on sediment yield depends not only upon direction of climate change, but also on the climate before the change. Sediment concentration in runoff is shown to increase with decreased annual precipitation, suggesting further that a decrease in precipitation will cause stream channel aggradation
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Yield of sediment in relation to mean annual precipitation |
| Series title | Eos, Transactions, American Geophysical Union |
| DOI | 10.1029/TR039i006p01076 |
| Volume | 39 |
| Issue | 6 |
| Language | English |
| Publisher | American Geophysical Union |
| Description | 9 p. |
| First page | 1076 |
| Last page | 1084 |
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