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Hui Wu

isobaths in ~60-km distance. The inner shelf slope was formed by the past sediments deposition from the Changjiang River ( Liu et al. 2018 ). Given this origin, it is conventionally called the Mud Belt. The AVISO data were again used to look at the MADT in the ECS, but for the February (winter) and July (summer) separately ( Figs. 9a,b ). The overlays show the monthly mean (in 2003–16) sea surface temperature (SST) derived from the Moderate Resolution Imaging Spectroradiometer (MODIS) Level-3 data, and

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Madeleine M. Hamann, Matthew H. Alford, Andrew J. Lucas, Amy F. Waterhouse, and Gunnar Voet

Canyon, Taiwan . J. Mar. Syst. , 76 , 383 – 396 , https://doi.org/10.1016/j.jmarsys.2007.08.005 . 10.1016/j.jmarsys.2007.08.005 Lentz , S. J. , and C. Winant , 1986 : Subinertial currents on the Southern California Shelf . J. Phys. Oceanogr. , 16 , 1737 – 1750 , https://doi.org/10.1175/1520-0485(1986)016<1737:SCOTSC>2.0.CO;2 . 10.1175/1520-0485(1986)016<1737:SCOTSC>2.0.CO;2 Liu , J. T. , K.-j. Liu , and J. C. Huang , 2002 : The effect of a submarine canyon on the river sediment

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