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

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 jett...

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Main Authors: Ting-Yu Liang, Chih-Hsin Chang, Shih-Chun Hsiao, Wei-Po Huang, Tzu-Yin Chang, Wen-Dar Guo, Che-Hsin Liu, Jui-Yi Ho, Wei-Bo Chen
Format: Article
Language:English
Published: MDPI AG 2022-02-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/10/2/282
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author Ting-Yu Liang
Chih-Hsin Chang
Shih-Chun Hsiao
Wei-Po Huang
Tzu-Yin Chang
Wen-Dar Guo
Che-Hsin Liu
Jui-Yi Ho
Wei-Bo Chen
author_facet Ting-Yu Liang
Chih-Hsin Chang
Shih-Chun Hsiao
Wei-Po Huang
Tzu-Yin Chang
Wen-Dar Guo
Che-Hsin Liu
Jui-Yi Ho
Wei-Bo Chen
author_sort Ting-Yu Liang
collection DOAJ
description 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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spelling doaj.art-c97410c4021e442d82c7f6b5bafd7d482023-11-23T20:36:26ZengMDPI AGJournal of Marine Science and Engineering2077-13122022-02-0110228210.3390/jmse10020282On-Site Investigations of Coastal Erosion and Accretion for the Northeast of TaiwanTing-Yu Liang0Chih-Hsin Chang1Shih-Chun Hsiao2Wei-Po Huang3Tzu-Yin Chang4Wen-Dar Guo5Che-Hsin Liu6Jui-Yi Ho7Wei-Bo Chen8National Science and Technology Center for Disaster Reduction, New Taipei City 23143, TaiwanNational Science and Technology Center for Disaster Reduction, New Taipei City 23143, TaiwanDepartment of Hydraulic and Ocean Engineering, National Cheng Kung University, Tainan City 70101, TaiwanDepartment of Harbor and River Engineering, National Taiwan Ocean University, Keelung City 202301, TaiwanNational Science and Technology Center for Disaster Reduction, New Taipei City 23143, TaiwanNational Science and Technology Center for Disaster Reduction, New Taipei City 23143, TaiwanNational Science and Technology Center for Disaster Reduction, New Taipei City 23143, TaiwanNational Science and Technology Center for Disaster Reduction, New Taipei City 23143, TaiwanNational Science and Technology Center for Disaster Reduction, New Taipei City 23143, TaiwanCoastal 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.https://www.mdpi.com/2077-1312/10/2/282erosion and accretioncross-shore profile evolutionLanyang River estuarylimit of estuarine sediment transportnortheastern coastal waters of Taiwan
spellingShingle Ting-Yu Liang
Chih-Hsin Chang
Shih-Chun Hsiao
Wei-Po Huang
Tzu-Yin Chang
Wen-Dar Guo
Che-Hsin Liu
Jui-Yi Ho
Wei-Bo Chen
On-Site Investigations of Coastal Erosion and Accretion for the Northeast of Taiwan
Journal of Marine Science and Engineering
erosion and accretion
cross-shore profile evolution
Lanyang River estuary
limit of estuarine sediment transport
northeastern coastal waters of Taiwan
title On-Site Investigations of Coastal Erosion and Accretion for the Northeast of Taiwan
title_full On-Site Investigations of Coastal Erosion and Accretion for the Northeast of Taiwan
title_fullStr On-Site Investigations of Coastal Erosion and Accretion for the Northeast of Taiwan
title_full_unstemmed On-Site Investigations of Coastal Erosion and Accretion for the Northeast of Taiwan
title_short On-Site Investigations of Coastal Erosion and Accretion for the Northeast of Taiwan
title_sort on site investigations of coastal erosion and accretion for the northeast of taiwan
topic erosion and accretion
cross-shore profile evolution
Lanyang River estuary
limit of estuarine sediment transport
northeastern coastal waters of Taiwan
url https://www.mdpi.com/2077-1312/10/2/282
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