Anti clockwise hysteresis in suspended sediment concentration during individual storms: Holbeck catchment; Yorkshire, England

Micha Klein

doi:10.1016/0341-8162(84)90014-6

Anti clockwise hysteresis in suspended sediment concentration during individual storms: Holbeck catchment; Yorkshire, England

Micha Klein

Department of Geography and Environmental Studies

Research output: Contribution to journal › Article › peer-review

Abstract

Analysis of the flow sediment hysteresis shape may assist in determining the sediment source area in a small basin. A clockwise hysteresis occurs when sediment is derived from the bed and banks of the channel or areas adjacent to the channel, whereas an anti-clockwise hysteresis occurs when the upper part of the slopes is the sediment source area.

Original language	English
Pages (from-to)	251-257
Number of pages	7
Journal	Catena
Volume	11
Issue number	2-3
DOIs	https://doi.org/10.1016/0341-8162(84)90014-6
State	Published - Aug 1984

ASJC Scopus subject areas

Earth-Surface Processes

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10.1016/0341-8162(84)90014-6

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title = "Anti clockwise hysteresis in suspended sediment concentration during individual storms: Holbeck catchment; Yorkshire, England",

abstract = "Analysis of the flow sediment hysteresis shape may assist in determining the sediment source area in a small basin. A clockwise hysteresis occurs when sediment is derived from the bed and banks of the channel or areas adjacent to the channel, whereas an anti-clockwise hysteresis occurs when the upper part of the slopes is the sediment source area.",

author = "Micha Klein",

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AU - Klein, Micha

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AB - Analysis of the flow sediment hysteresis shape may assist in determining the sediment source area in a small basin. A clockwise hysteresis occurs when sediment is derived from the bed and banks of the channel or areas adjacent to the channel, whereas an anti-clockwise hysteresis occurs when the upper part of the slopes is the sediment source area.

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DO - 10.1016/0341-8162(84)90014-6

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Anti clockwise hysteresis in suspended sediment concentration during individual storms: Holbeck catchment; Yorkshire, England

Abstract

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