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Recent Evolution of the Intertidal Sand Ridge Lines of the Dongsha Shoal in the Modern Radial Sand Ridges, East China

Bibliographic Data

ID15468147
AuthorsBinglin Liu (0000-0002-8376-1694, Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application), Haotian Wu (0000-0002-6271-0249, Nanjing University), Zhenke Zhang (0000-0003-2751-1153, Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, corresponding author), Guoen Wei (0000-0002-2054-7623, Nanjing University), Yue Wang (0000-0001-8527-9175, Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application), Wen Zhu (0000-0001-7224-6729, Nanjing University), Jie Zheng (0009-0002-7853-6721, Nanjing Forestry University), Xuepeng Ji (0000-0002-3959-4059, Nanjing University), Shengnan Jiang (0000-0001-7083-595X, Nanjing University)
Year2021
Volume18
Issue4
Pages1573-1573
Publication date2021-02-07
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueInternational Journal of Environmental Research and Public Health (JOURNAL)
Journal identifiersISSN: 1661-7827 • E-ISSN: 1660-4601
PublisherMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/ijerph18041573
PMID33562304
OpenAlexW3127111905
LanguageEN
References cited57

The Dongsha Shoal is one of the largest shoals in the South Yellow Sea and has important marine ecological value. The shoal extends in a south-north direction and is controlled by the regional dominating tidal currents. Recently, due to human activities and some natural factors, the geomorphic dynamics of the Dongsha Shoal has undergone drastic changes. However, few people have proposed quantitative research on the changes of tidal flat morphology, let alone the long-term sequence analysis of sand ridge lines. Hence, we attempt to take the Dongsha Shoal in the Radial Sand Ridges as the research area, and analyze the trends of the long-term morphological evolution of the sand ridge lines over the period 1973-2016 based on a high-density time series of medium-resolution satellite images. The sand ridge line generally moves from southeast to northwest, and the position distribution of the sand ridge line from north to south has gradually changed from compact to scattered. We also found that the geomorphological dynamics at different positions of the sand ridge line are inconsistent. The north and south wings are eroded on the west side, while the central area is eroded on the east side. Most of the sand ridge line is moving eastward. In addition, the change of sand ridge line is affected by multiple factors such as sediment supply, typhoon, reclamation and laver cultivation

Geomorphology · Intertidal zone · Ridge · Shoal · Typhoon · Coastal and Marine Dynamics · Coastal wetland ecosystem dynamics · Geology and Paleoclimatology Research · Geology · Oceanography · Paleontology

  • Rapid Loss of Tidal Flats in the Yangtze River Delta since 1974

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  • Recent Evolution of Coastal Tidal Flats and the Impacts of Intensified Human Activities in the Modern Radial Sand Ridges, East China

    Open Access•Yifei Zhao, Qing Liu et al.•International Journal of…•2020

Citation velocityhistorical
Highly citedNo

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