4.7 Article

On-Site Investigations of Coastal Erosion and Accretion for the Northeast of Taiwan

Journal

Publisher

MDPI
DOI: 10.3390/jmse10020282

Keywords

erosion and accretion; cross-shore profile evolution; Lanyang River estuary; limit of estuarine sediment transport; northeastern coastal waters of Taiwan

Funding

  1. National Science and Technology Center for Disaster (NCDR), Ministry of Science and Technology (MOST), Taiwan

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Coastal erosion is a major natural hazard along the northeastern shoreline (i.e., Yilan County) of Taiwan, with erosion and accretion occurring at different parts due to jetty and groin construction. Topographic and bathymetric surveys conducted in 2006, 2012, 2013, and 2019 reveal that erosion is significant in the northern Jhuan River estuary while accretion is inevitable in the northern Lanyang River estuary. The bathymetric surveys also suggest that the shoreline of Yilan County tends to accrete in summer but erode in winter, with approximately 2 km of coastline impacted by estuarine sediment transport along the Lanyang River estuary.
Coastal erosion is a major natural hazard along the northeastern shoreline (i.e., Yilan County) of Taiwan. Analyses of the evolution of the 0 m isobath of the Yilan County coastline indicate that erosion and accretion are occurring north and south of Wushi Fishery Port, respectively, because of jetty and groin construction. Topographic and bathymetric surveys involving the measurement of 43 cross sections were conducted in 2006, 2012, 2013, and 2019. The cross-shore profile comparisons reveal that the erosion of onshore dunes is significant in the northern Jhuan River estuary. Due to the establishment of a nature reserve in the southern Lanyang River estuary, the sediments are carried northward by tidal currents, and accretion is inevitable in the northern Lanyang River estuary. The results of the bathymetric surveys also suggest that the shoreline of Yilan County tends to accrete in summer because of abundant sediment from the rivers; however, it is eroded in winter, owing to the large waves induced by the northeast monsoon. Additionally, the calculated net volume of erosion and accretion between each pair of cross sections shows that the length of coastline impacted by estuarine sediment transport is approximately 2 km long from north to south along the coastline of the Lanyang River estuary.

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