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• W2912685597 abstract "Abstract Shore platforms control wave energy transformation which, in turn, controls energy delivery to the cliff toe and nearshore sediment transport. Insight into shore platform erosion rates has conventionally been constrained at millimetre‐scales using micro‐erosion metres, and at metre‐scales using cartographic data. On apparently slowly eroding coasts, such approaches are fundamentally reliant upon long‐term observation to capture emergent erosion patterns. Where in practise timescales are short, and where change is either below the resolution or saturates the mode of measurement, the collection of data that enables the identification of the actual mechanisms of erosion is hindered. We developed a method to monitor shore platform erosion at millimetre resolution within metre‐scale monitoring plots using Structure‐from‐Motion photogrammetry. We conducted monthly surveys at 15 0.25 m 2 sites distributed across the Hartle Loup platform in North Yorkshire, UK, over one year. We derived topographic data at 0.001 m resolution, retaining a vertical precision of change detection of 0.001 m. We captured a mean erosion rate of 0.528 mm yr ‐1 , but this varied considerably both across the platform and through the year. We characterized the volume and shape of eroded material. The detachment volume–frequency and shape distributions suggest that erosion happens primarily via removal of shale platelets. We identify that the at‐a‐point erosion rate can be predicted by the distance from the cliff and the tidal level, whereby erosion rates are higher closer to the cliff and at locations of higher tidal duration. The size of individual detachments is controlled by local micro‐topography and rock structure, whereby larger detachments are observed on more rough sections of the platform. Faster erosion rates and larger detachments occur in summer months, rather than in more energetic winter conditions. These results have the potential to form the basis of improved models of how platforms erode over both short‐ and long‐timescales. © 2019 John Wiley & Sons, Ltd." @default.
• W2912685597 created "2019-02-21" @default.
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• W2912685597 date "2019-04-01" @default.
• W2912685597 modified "2023-09-25" @default.
• W2912685597 title "Identifying mechanisms of shore platform erosion using Structure‐from‐Motion (SfM) photogrammetry" @default.
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• W2912685597 cites W1932755381 @default.
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• W2912685597 cites W1967653411 @default.
• W2912685597 cites W1969207771 @default.
• W2912685597 cites W1970995698 @default.
• W2912685597 cites W1973463701 @default.
• W2912685597 cites W1978754515 @default.
• W2912685597 cites W1984098833 @default.
• W2912685597 cites W1984221800 @default.
• W2912685597 cites W1998081443 @default.
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• W2912685597 cites W2012091321 @default.
• W2912685597 cites W2014737435 @default.
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• W2912685597 doi "https://doi.org/10.1002/esp.4591" @default.
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