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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書誌詳細
第一著者: Vanacker, Veerle (author)
その他の著者: Blanckenburg, F. von (author), Govers, Gerard (author), Molina, Armando (author), Campforts, B. (author), Kubik, P. W. (author)
フォーマット: article
言語:eng
出版事項: 2015
主題:
オンライン・アクセス:http://dspace.ucuenca.edu.ec/handle/123456789/22012
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