Threshold friction velocity influenced by soil particle size within the Columbia Plateau, northwestern United States
Wind erosion is a geomorphic process in arid and semi-arid areas and has substantial implications for regional climate and desertification. In the Columbia Plateau of northwestern United States, the emissions from fine particles of loessial soils often contribute to the exceedance of inhalable parti...
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Veröffentlicht in: | Journal of arid land 2024-08, Vol.16 (8), p.1147-1162 |
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