Jiangsu Key Laboratory of Marine Bioresources and Environment/Jiangsu Key Laboratory of Marine Biotechnology, Jiangsu Ocean University, Lianyungang, Jiangsu Province, China
School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu Province, China
Linfei Bai
Lianyungang Meteorological Bureau, Lianyungang, Jiangsu Province, China
School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu Province, China
Hao Shen
School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu Province, China
Xiaoqi Ding
Lianyungang Meteorological Bureau, Lianyungang, Jiangsu Province, China
School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu Province, China
Rui Wang
Lianyungang Meteorological Bureau, Lianyungang, Jiangsu Province, China
School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu Province, China
Jiangsu Key Laboratory of Marine Bioresources and Environment/Jiangsu Key Laboratory of Marine Biotechnology, Jiangsu Ocean University, Lianyungang, Jiangsu Province, China
Co-Innovation Center of Jiangsu Marine Bio-industry Technology,
Jiangsu Ocean University, Lianyungang, Jiangsu Province, China
School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu Province, China
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The super cyclonic storm Amphan occurred in the central Bay of Bengal in May 2020, and a phytoplankton bloom occurred. Its dynamic mechanism was first researched. An inertial oscillation with a 2 d period appeared and lasted for approximately 2 weeks. With the weakened thermocline and thinner barrier layer thickness, nitrate and Chl a were uplifted to the upper ocean by upwelling. With the high photosynthetically available radiation, a phytoplankton bloom occurred.
The super cyclonic storm Amphan occurred in the central Bay of Bengal in May 2020, and a...
