Transient river response, captured by channel steepness and its concavity
Mountain rivers draining tropical regions are known to be great conveyor belts carrying efficiently more than half of the global sediment flux to the oceans. Many tropical mountain areas are located in tectonically active belts where the hillslope and stream channel morphology are rapidly evolving i...
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| 格式: | article |
| 語言: | eng |
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2015
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| 在線閱讀: | http://dspace.ucuenca.edu.ec/handle/123456789/22012 |
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