| Abstract: | In the North Fork Toutle River at Kid Valley, Washington, weak correlation between flow depth and the standard deviation of bed elevation was noted. Dunes were often superposed on larger bed forms with wave periods between 10 and 30 min. Gradual changes in waveform height and periodicity occurred over several hours during storm runoff. Rates of migration for typical dunes were estimated to be 3 cm s-1, and dune wavelengths were estimated to be 6 to 7 m. -from Author |
| Genre: | Article |
| ProdID: | 70015750 |
| Citation Author: | Dinehart, R. L. |
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| Citation End Page: | 923 |
| Citation Issue: | 5 |
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| Citation Language: | English |
| Citation Larger Work Title: | Water Resources Research |
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| Citation Number Of Pages: | 13 |
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| Citation Search Results Text: | Dune migration in a steep, coarse-bedded stream; 1989; Article; Journal; Water Resources Research; Dinehart, R. L. |
| Citation Start Page: | 911 |
| Citation Volume: | 25 |
| Citation Year: | 1989 |
| Type: | citation/reference |
| Text: | Dune migration in a steep, coarse-bedded stream; 1989; Article; Journal; Water Resources Research; Dinehart, R. L. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sun, 1 Jan 1989 00:00 -0600 |
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