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Stephen E. Darby

Researcher at University of Southampton

Publications -  138
Citations -  7382

Stephen E. Darby is an academic researcher from University of Southampton. The author has contributed to research in topics: Bank erosion & Fluvial. The author has an hindex of 41, co-authored 116 publications receiving 6040 citations. Previous affiliations of Stephen E. Darby include Agricultural Research Service & University of Tehran.

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Modelling the response of soft cliffs to climate change: a statistical, process-response model using accumulated excess energy

TL;DR: In this article, a new statistical, process-response model of soft cliff erosion is proposed, based on the premise that wave energy delivered to the cliff toe is the key parameter forcing erosion.
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Experimental and numerical investigation of the stability of overhanging riverbanks

TL;DR: In this article, a laboratory study of cantilever failure was carried out using two types of materials to form overhanging banks with three different densities, and the results showed that the occurrence of toppling failures is more probable than the simple shear-type mechanism that has been analyzed most frequently by prior researchers.
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The use of one- and two-dimensional hydraulic modelling to reconstruct a glacial outburst flood in a steep Alpine valley

TL;DR: In this article, the hydrologic characteristics of the 1943 outburst flood from the Glacier du Mont Mine, Switzerland, were reconstructed using field evidence (palaeostage indicators) in conjunction with shallow water modelling techniques.
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First direct measurements of hydraulic jumps in an active submarine density current

TL;DR: In this paper, the authors provide the first direct evidence of hydraulic jumps in a submarine density current and show that the observed hydraulic jumps are in phase with seafloor scours.
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Decoding the drivers of bank erosion on the Mekong river: The roles of the Asian monsoon, tropical storms, and snowmelt

TL;DR: There is an intense and prolonged epoch of strong coherence between ENSo and AER from the early 1980s to present, such that in recent decades derived Mekong River bank erosion has been more strongly affected by ENSO.