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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 equilibrium bed topography of submarine meanders that exhibit reversed secondary flows

TL;DR: In this paper, the authors explored the possible morphological implications of a reversal of secondary flow by modelling the force balance on sediment grains moving through either field and laboratory submarine meander bends that are known to exhibit reversed secondary flows, or inactive submarine bends where the nature of the secondary flow in the formative turbidity currents can be inferred to be reversed.
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An analytical method to estimate failure plane angle and tension crack depth for use in riverbank stability analyses

TL;DR: In this article, a new analytical method was proposed to estimate the failure plane angle and the depth of the tension crack in a riverbank with planar failure. But this method is not suitable for the case of steep, relatively low banks composed of cohesive sediments.
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Regional analysis of multivariate compound coastal flooding potential around Europe and environs: sensitivity analysis and spatial patterns

TL;DR: In this paper, the authors analyzed compound flooding potential in Europe and environs caused by these four main flooding sources using state-of-the-art databases with coherent forcing (i.e. ERA5).
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Effects of Holocene climate and sea‐level changes on coastal gully evolution: insights from numerical modelling

TL;DR: In this paper, the authors explore the Holocene erosional history of the Chines using a numerical landscape evolution model that has been modified to include a cliff recession function, and they suggest that the rate of sea-level rise is the key control on Chine formation and that it is only in this late Holocene period, and specifically in the last 2000 years, that sealevel rise has slowed sufficiently for knickpoint recession rates to exceed cliff recession rates and create sustainable gully networks.