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Sheet flow

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Sheet flow is described as overland flow that happens in a continuous sheet, characterized by relatively high frequency and low magnitude, and is limited to conditions of laminar flow.[1]

References

  1. ^ Hogg, Susan E. "Sheetfloods, sheetwash, sheetflow, or ... ?". Earth-Science Reviews. 18 (1): 59–76. doi:10.1016/0012-8252(82)90003-4. ISSN 0012-8252.


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