4.7 Article

HY-1C Observations of the Impacts of Islands on Suspended Sediment Distribution in Zhoushan Coastal Waters, China

期刊

REMOTE SENSING
卷 12, 期 11, 页码 -

出版社

MDPI
DOI: 10.3390/rs12111766

关键词

HY-1C; suspended sediment concentration; islands; vortex street

资金

  1. Planning Program of Science and Technology of Zhoushan [2016C41018]
  2. Research Project of Zhejiang Department of Education [Y201840279]
  3. Guangdong Key Laboratory of Ocean Remote Sensing (South China Sea Institute of Oceanology Chinese Academy of Sciences) [2017B030301005-LORS2001, 2019BT2H594]
  4. open Foundation from Marine Sciences in the First-Class Subjects of Zhejiang Province [11104060218]
  5. National Natural Science Foundation of China [41776183]
  6. National Key Project of Research and Development Plan of China Research and Development of Ocean Big Data Analysis and Forecast Technology, three-dimensional temperature and salinity prediction by big data analysis technology for marine dynamic environme [2016YFC1401904]

向作者/读者索取更多资源

We analyzed the impacts of islands on suspended sediment concentration (SSC) in Zhoushan Coastal waters based on data from HY-1C, which was launched in September 2018 in China, carrying Coastal Zone Imager (CZI) and Chinese Ocean Color and Temperature Scanner (COCTS) on it for offshore observation. A new SSC retrieved model was established based on the relationship between in situ SSC and the reflectance in red and near infrared bands of CZI image. Fifteen CZI images obtained from October to December 2019 were applied to retrieve SSC in Zhoushan coastal waters. The results show that SSC in study area is 100-1600 mgL(-1). The SSC near islands changes obviously. Upstream of the islands, SSC is lower than downstream. During the flood and ebb, when the current passes through the islands, circumfluence will appear, under certain geophysical factors, generating Karman vortex streets downstream of the islands. The sediments were stirred by the fast speed current at the outer side of vortex street to the sea surface inducing higher SSC at the outer side of the vortex street, while the central sediments of the vortex street were lower. In the direction of ocean currents, the SSC of the vortex street downstream of islands is changing regularly, i.e., increasing, then decreasing and increasing again and then decreasing in a snaking vortex street whose length downstream is between 1000 and 8000 m long.

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