The impact of sea-level rise on the coast of Tianjin-Hebei, China

ABSTRACT: Bulletins of China’s National Sea Level show that the average rising rate of sea-levels in China is 3.3 mm/a over the past 40 years, with an obviously accelerated rising trend in the last decade. The rate of relative sea-level rise of the Yangtze River Delta reached >10 mm/a after consi...

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Main Authors: Fu Wang, Jian-fen Li, Pei-xin Shi, Zhi-wen Shang, Yong Li, Hong Wang
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2019-03-01
Series:China Geology
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S209651921930103X
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author Fu Wang
Jian-fen Li
Pei-xin Shi
Zhi-wen Shang
Yong Li
Hong Wang
author_facet Fu Wang
Jian-fen Li
Pei-xin Shi
Zhi-wen Shang
Yong Li
Hong Wang
author_sort Fu Wang
collection DOAJ
description ABSTRACT: Bulletins of China’s National Sea Level show that the average rising rate of sea-levels in China is 3.3 mm/a over the past 40 years, with an obviously accelerated rising trend in the last decade. The rate of relative sea-level rise of the Yangtze River Delta reached >10 mm/a after considering the land subsidence, and Bohai Bay is even greater than 25 mm/a. The impact of the sea level rise to the coastal area will be greater in the coming years, so carrying out an assessment of this rising trend is urgent. This paper, taking the coastal area of Tianjin and Hebei as examples, comprehensively evaluates the impact of sea-level rise through multitemporal remote sensing shoreline interpretation, ground survey verification, elevation measurements for both seawall and coastal lowlands. The results show that the average elevation of the measured coastal areas of Tianjin and Hebei is about +4 m, and the total area of >100 km2 is already below the present mean sea level. More than 270 km, ca. 31% of the total length of the seawall, cannot withstand a 1-in-100-year storm surge. Numerical simulations of the storm flooding on the west coast of Bohai Bay, for 1-in-50-years, 1-in-100-years, 1-in-200-years and 1-in-500-years, show that if there were no coastal dykes, the maximum flooding area would exceed 3000 km2, 4000 km2, 5300 km2 and 7200 km2, respectively. The rising sea has a direct and potential impact on the coastal lowlands of Tianjin and Hebei. Based on the latest development in international sea-level rise prediction research, this paper proposes 0.5 m, 1.0 m and 1.5 m as low, middle and high sea level rise scenarios by 2100 for the study area, and combines the land subsidence and other factors to the elevation of the existing seawall. Comprehensive evaluation results indicate that even in the case of a low scenario, the existing seawall will not be able to withstand a 1-in-100-years storm surge in 2030, and the potential flooding areas predicted by the model will become a reality in the near future. Therefore, the seawall design in the coastal areas of Tianjin and Hebei must consider the combined effects of land subsidence, sea level rise and the extreme storm surges caused by it.©2019 China Geology Editorial Office.
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spelling doaj.art-9159f082d3ab4161bda970a25819793f2023-02-07T04:21:49ZengKeAi Communications Co., Ltd.China Geology2096-51922019-03-01212639The impact of sea-level rise on the coast of Tianjin-Hebei, ChinaFu Wang0Jian-fen Li1Pei-xin Shi2Zhi-wen Shang3Yong Li4Hong Wang5Tianjin Center, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, China; Key Laboratory of Muddy Coast Geo-Environment, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, China; Corresponding author: E-mail address: wfu@cgs.cn (Fu Wang); whong@cgs.cn (Hong Wang).Tianjin Center, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, China; Key Laboratory of Muddy Coast Geo-Environment, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, ChinaTianjin Center, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, China; Key Laboratory of Muddy Coast Geo-Environment, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, ChinaTianjin Center, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, China; Key Laboratory of Muddy Coast Geo-Environment, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, ChinaTianjin Center, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, China; Key Laboratory of Muddy Coast Geo-Environment, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, ChinaTianjin Center, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, China; Key Laboratory of Muddy Coast Geo-Environment, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, China; Corresponding author: E-mail address: wfu@cgs.cn (Fu Wang); whong@cgs.cn (Hong Wang).ABSTRACT: Bulletins of China’s National Sea Level show that the average rising rate of sea-levels in China is 3.3 mm/a over the past 40 years, with an obviously accelerated rising trend in the last decade. The rate of relative sea-level rise of the Yangtze River Delta reached >10 mm/a after considering the land subsidence, and Bohai Bay is even greater than 25 mm/a. The impact of the sea level rise to the coastal area will be greater in the coming years, so carrying out an assessment of this rising trend is urgent. This paper, taking the coastal area of Tianjin and Hebei as examples, comprehensively evaluates the impact of sea-level rise through multitemporal remote sensing shoreline interpretation, ground survey verification, elevation measurements for both seawall and coastal lowlands. The results show that the average elevation of the measured coastal areas of Tianjin and Hebei is about +4 m, and the total area of >100 km2 is already below the present mean sea level. More than 270 km, ca. 31% of the total length of the seawall, cannot withstand a 1-in-100-year storm surge. Numerical simulations of the storm flooding on the west coast of Bohai Bay, for 1-in-50-years, 1-in-100-years, 1-in-200-years and 1-in-500-years, show that if there were no coastal dykes, the maximum flooding area would exceed 3000 km2, 4000 km2, 5300 km2 and 7200 km2, respectively. The rising sea has a direct and potential impact on the coastal lowlands of Tianjin and Hebei. Based on the latest development in international sea-level rise prediction research, this paper proposes 0.5 m, 1.0 m and 1.5 m as low, middle and high sea level rise scenarios by 2100 for the study area, and combines the land subsidence and other factors to the elevation of the existing seawall. Comprehensive evaluation results indicate that even in the case of a low scenario, the existing seawall will not be able to withstand a 1-in-100-years storm surge in 2030, and the potential flooding areas predicted by the model will become a reality in the near future. Therefore, the seawall design in the coastal areas of Tianjin and Hebei must consider the combined effects of land subsidence, sea level rise and the extreme storm surges caused by it.©2019 China Geology Editorial Office.http://www.sciencedirect.com/science/article/pii/S209651921930103XSea level riseElevationSeawallShorelineTianjin-Hebei (Jin-Ji) coast
spellingShingle Fu Wang
Jian-fen Li
Pei-xin Shi
Zhi-wen Shang
Yong Li
Hong Wang
The impact of sea-level rise on the coast of Tianjin-Hebei, China
China Geology
Sea level rise
Elevation
Seawall
Shoreline
Tianjin-Hebei (Jin-Ji) coast
title The impact of sea-level rise on the coast of Tianjin-Hebei, China
title_full The impact of sea-level rise on the coast of Tianjin-Hebei, China
title_fullStr The impact of sea-level rise on the coast of Tianjin-Hebei, China
title_full_unstemmed The impact of sea-level rise on the coast of Tianjin-Hebei, China
title_short The impact of sea-level rise on the coast of Tianjin-Hebei, China
title_sort impact of sea level rise on the coast of tianjin hebei china
topic Sea level rise
Elevation
Seawall
Shoreline
Tianjin-Hebei (Jin-Ji) coast
url http://www.sciencedirect.com/science/article/pii/S209651921930103X
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