Abstract
Increasingly used shore-based video stations enable a high spatiotemporal frequency analysis of shoreline migration. Shoreline detection techniques combined with hydrodynamic conditions enable the creation of digital elevation models (DEMs). However, shoreline elevations are often estimated based on nearshore process empirical equations leading to uncertainties in video-based topography. To achieve high DEM correspondence between both techniques, we assessed video-derived DEMs against LiDAR surveys during low energy conditions. A newly installed video system on a tidal flat in the St. Lawrence Estuary, Atlantic Canada, served as a test case. Shorelines were automatically detected from time-averaged (TIMEX) images using color ratios in low energy conditions synchronously with mobile terrestrial LiDAR during two different surveys. Hydrodynamic (waves and tides) data were recorded in-situ, and established two different cases of water elevation models as a basis for shoreline elevations. DEMs were created and tested against LiDAR. Statistical analysis of shoreline elevations and migrations were made, and morphological variability was assessed between both surveys. Results indicate that the best shoreline elevation model includes both the significant wave height and the mean water level. Low energy conditions and in-situ hydrodynamic measurements made it possible to produce video-derived DEMs virtually as accurate as a LiDAR product, and therefore make an effective tool for coastal managers.
Highlights
Beaches evolve through time and space, influenced by morphogenetic processes occurring in multiple dimensions in the surf and swash zones [1]
These results indicate that the overall contribution from Hs is small in the total water level approximation (M2) but it reduces the origin contribution from Hs is small in the total water level approximation (M2) but it reduces the origin offset by 2 cm
Two shoreline elevation models were tested against LiDAR-derived shorelines and interpolated topography
Summary
Beaches evolve through time and space, influenced by morphogenetic processes occurring in multiple dimensions in the surf and swash zones [1]. Different short-term dynamic processes occur on a beach, mostly wave-induced high/low-frequency swash motions [2], groundwater/bed interactions [3,4], and scouring [5]. The beach morphology usually tends toward an equilibrium slope resulting from an onshore/offshore sediment transport induced by waves and currents [6,7,8]. Changes occur on longer time scales where beaches are affected by strong seasonal cycles. In cold regions, the presence of sea ice can protect (i.e., consolidates beach sediments) or erode (i.e., scouring at the icefoot’s toe, transport by drift ice, etc.) the beach profile [9].
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