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Title: Coastal topography and hydrogeology control critical groundwater gradients and potential beach surface instability during storm surges
Abstract. Ocean surges pose a global threat for coastal stability.These hazardous events alter flow conditions and pore pressures in floodedbeach areas during both inundation and subsequent retreat stages, which canmobilize beach material, potentially enhancing erosion significantly. Inthis study, the evolution of surge-induced pore-pressure gradients is studied through numerical hydrologic simulations of storm surges. The spatiotemporal variability of critically high gradients is analyzed in three dimensions. The analysis is based on a threshold value obtained for quicksand formationof beach materials under groundwater seepage. Simulations of surge eventsshow that, during the run-up stage, head gradients can rise to the calculated critical level landward of the advancing inundation line. During thereceding stage, critical gradients were simulated seaward of the retreatinginundation line. These gradients reach maximum magnitudes just as sea levelreturns to pre-surge levels and are most accentuated beneath the still-water shoreline, where the model surface changes slope. The gradients vary alongthe shore owing to variable beach morphology, with the largest gradientsseaward of intermediate-scale (1–3 m elevation) topographic elements (dunes)in the flood zone. These findings suggest that the common practices inmonitoring and mitigating surge-induced failures and erosion, which typically focus on the flattest areas of beaches, might need to be revised to include other topographic features.  more » « less
Award ID(s):
1948137 1757353 1751463 1829136
NSF-PAR ID:
10383528
Author(s) / Creator(s):
; ; ; ; ; ; ;
Date Published:
Journal Name:
Hydrology and Earth System Sciences
Volume:
26
Issue:
23
ISSN:
1607-7938
Page Range / eLocation ID:
5987 to 6002
Format(s):
Medium: X
Sponsoring Org:
National Science Foundation
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