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Impacts of Anthropogenic Structures in Long- and Short-Term Shoreline Evolution of Santa Marta Bay (Colombian Caribbean)
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Abstract
Interaction of Anthropic interventions (rigid structures) with coasts is an essential aspect for understanding their geomorphic evolution and incorporating these data into adequate coastal management. This study analyses the short and long-term behavior (1985 to 2019) of shoreline at Santa Marta Bay (Caribbean - Colombia) and their relationship with coastal protection structures. The shoreline variations were analyzed through aerial photographs and satellite images using DSAS tools. The short-term assessment revealed initial intense 1985–1991 erosion, with an average retreat speed of − 1.6 m·y− 1. It changed gradually since 2003, due to the construction of rigid structures and beach nourishment, decreasing shoreline retreat and even a progradation of 0.2 m·y− 1 was observed. The 2009–2019 period, despite recording a positive average value, exhibited a high percentage of erosion profiles. Therefore, in a decadal or long-term analysis (1985–2019), despite engineering works present positive results in the short term, new interventions are required. The coastal erosion is not uniform along the shoreline, because the area is a closed bay with small sediment contribution, the variations in erosion and accretion rates change with human intervention and the installation of new structures. Therefore, quantifying the scale and rate of shoreline changes and correlating them with anthropogenic structures is an essential step in assessing shoreline vulnerability.
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Title: Impacts of Anthropogenic Structures in Long- and Short-Term Shoreline Evolution of Santa Marta Bay (Colombian Caribbean)
Description:
Abstract
Interaction of Anthropic interventions (rigid structures) with coasts is an essential aspect for understanding their geomorphic evolution and incorporating these data into adequate coastal management.
This study analyses the short and long-term behavior (1985 to 2019) of shoreline at Santa Marta Bay (Caribbean - Colombia) and their relationship with coastal protection structures.
The shoreline variations were analyzed through aerial photographs and satellite images using DSAS tools.
The short-term assessment revealed initial intense 1985–1991 erosion, with an average retreat speed of − 1.
6 m·y− 1.
It changed gradually since 2003, due to the construction of rigid structures and beach nourishment, decreasing shoreline retreat and even a progradation of 0.
2 m·y− 1 was observed.
The 2009–2019 period, despite recording a positive average value, exhibited a high percentage of erosion profiles.
Therefore, in a decadal or long-term analysis (1985–2019), despite engineering works present positive results in the short term, new interventions are required.
The coastal erosion is not uniform along the shoreline, because the area is a closed bay with small sediment contribution, the variations in erosion and accretion rates change with human intervention and the installation of new structures.
Therefore, quantifying the scale and rate of shoreline changes and correlating them with anthropogenic structures is an essential step in assessing shoreline vulnerability.
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