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Study on the non-stationary characteristics of extreme storm surges along the Changjiang River Estuary
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Dongmei Xie1, 2, 3, Yongping Chen2, 3, *, Qianqian Yu2, 3, Li Sun4, Chonglun Pan4
Haiyang Xuebao | 2023, 45(7) : 25 - 39
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Haiyang Xuebao | 2023, 45(7): 25-39
Article
Study on the non-stationary characteristics of extreme storm surges along the Changjiang River Estuary
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Dongmei Xie1, 2, 3, Yongping Chen2, 3, *, Qianqian Yu2, 3, Li Sun4, Chonglun Pan4
Affiliations
  • 1River and Harbor Engineering Department, Nanjing Hydraulic Research Institute, Nanjing 210029, China
  • 2State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China
  • 3College of Harbour, Coastal and Offshore Engineering, Hohai University, Nanjing 210098, China
  • 4Shanghai Flood and Drought Disaster Prevention Technology Center, Shanghai 200050, China
Published: 2023-07-01 doi: 10.12284/hyxb2023099
Outline
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Under the background of global climate change, the extreme storm surge events caused by tropical cyclones in the Changjiang River Estuary and adjacent coastal area present non-stationary feature. In this study, a storm surge model for the Changjiang River Estuary was constructed using the ADCIRC model to reproduce the storm surges during 241 tropical cyclones affecting the Changjiang River Estuary from 1979 to 2019. By combining the non-stationary generalized extreme value distribution with the state space approach, a statistical model for capturing the non-stationarity of extreme storm surges was built to investigate the spatiotemporal variability of the extreme storm surges in the Changjiang River Estuary and its adjacent coastal area. The statistical model can well reproduce the non-stationary feature of extreme storm surges, which was mainly represented by the time-dependent location parameter. The time-dependent location parameters at the tidal gauge stations were stationary before 2008 and presented increasing trends afterwards, which was mainly caused by the increase of the annual second- and third-largest storm surges. The reoccurrence period of storm surge event with 100-year return period under the stationary assumption was reduced to around 40–80 years, indicating an increased flood risk in the Changjiang River Estuary. Combined with the changes in the intensity and path of the tropical cyclones that caused the annual second- and third-largest storm surges, it was concluded that the increasing trends of extreme storm surges were mainly caused by the increase in the intensity of the tropical cyclone that tracking northward to the offshore of the Changjiang River Estuary and veering eastwards.

the Changjiang River Estuary  /  extreme storm surges  /  non-stationary variation  /  extreme value statistics  /  state space model
Dongmei Xie, Yongping Chen, Qianqian Yu, Li Sun, Chonglun Pan. Study on the non-stationary characteristics of extreme storm surges along the Changjiang River Estuary[J]. Haiyang Xuebao, 2023 , 45 (7) : 25 -39 . DOI: 10.12284/hyxb2023099
Year 2023 volume 45 Issue 7
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Article Info
doi: 10.12284/hyxb2023099
  • Receive Date:2022-06-23
  • Online Date:2025-12-28
  • Published:2023-07-01
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History
  • Received:2022-06-23
  • Revised:2023-02-08
Funding
Affiliations
    1River and Harbor Engineering Department, Nanjing Hydraulic Research Institute, Nanjing 210029, China
    2State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China
    3College of Harbour, Coastal and Offshore Engineering, Hohai University, Nanjing 210098, China
    4Shanghai Flood and Drought Disaster Prevention Technology Center, Shanghai 200050, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
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Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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