Interrelationship between Wall and Beach Erosion in Loc An, Vietnam: Remote Sensing and Numerical Modeling Approaches
Author:
Van Duy Dinh1ORCID, Duc Anh Nguyen Quang2, Viet Nguyen Trung3ORCID, Tanaka Hitoshi4ORCID
Affiliation:
1. Faculty of Water Resource Engineering, College of Engineering, Can Tho University, Can Tho 94115, Vietnam 2. Institute of Civil Engineering, Thuyloi University, Ha Noi 11515, Vietnam 3. Faculty of Civil Engineering, Thuyloi University, Ha Noi 11515, Vietnam 4. Institute of Liberal Arts and Sciences, Tohoku University, 41 Kawauchi, Aoba-ku, Sendai 980-8576, Japan
Abstract
Beach erosion and coastal protection are complex and interconnected phenomena that have a substantial impact on coastal environments worldwide. Among the various coastal protection measures, seawalls have been widely implemented to mitigate erosion and protect coastal assets. However, the interrelationship between beach erosion and seawalls remains a critical topic for investigation to ensure effective and sustainable coastal management strategies. Seawalls impact the shoreline, particularly through the “end effect”, where the seawall functions similarly to a groin, causing erosion on the downdrift side relative to the direction of wave approach. This study provides a detailed analysis of the interplay between beach erosion and seawall structures in Loc An, Vietnam, employing both remote sensing and numerical approaches. Sentinel-2 images were employed together with an analytical solution to observe the shoreline change at the Loc An sand spit and to determine input values for the numerical model. Based on the shoreline dynamics, a numerical scheme was employed to study the shoreline evolution after the construction of a seawall. Our findings show that the shoreline evolution can be divided into three stages: (1) The first stage corresponds to the elongation of the sand spit without interference from coastal structures. (2) The second stage shows the effect of jetties on the shoreline, as signaled by the buildup of sand updrift of the jetties. (3) The third stage shows the effectiveness of the seawall, where the shoreline reaches its equilibrium condition. The study provides a quick and simple method for estimating shoreline diffusivity (ε) in situations where measured data is scarce.
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