Frontiers Science Center for Deep Ocean Multispheres and Earth System, and Key Laboratory of Marine Environment and Ecology, Ministry of Education of China, Ocean University of China, Qingdao, China
Laboratory for Marine Ecology and Environmental Sciences, Qingdao Marine Science and Technology Center, Qingdao, China
Climatic Research Unit, School of Environmental Sciences, University of East Anglia, Norwich, United Kingdom
Climatic Research Unit, School of Environmental Sciences, University of East Anglia, Norwich, United Kingdom
Xiaokun Ding
School of Ocean, Yantai University, Yantai, China
Xiang Gong
School of Mathematics and Physics, Qingdao University of Science and Technology, Qingdao, China
Qingdao Innovation Center of Artificial Intelligence Ocean Technology, Qingdao, China
Mingliang Gu
Frontiers Science Center for Deep Ocean Multispheres and Earth System, and Key Laboratory of Marine Environment and Ecology, Ministry of Education of China, Ocean University of China, Qingdao, China
Laboratory for Marine Ecology and Environmental Sciences, Qingdao Marine Science and Technology Center, Qingdao, China
Frontiers Science Center for Deep Ocean Multispheres and Earth System, and Key Laboratory of Marine Environment and Ecology, Ministry of Education of China, Ocean University of China, Qingdao, China
Laboratory for Marine Ecology and Environmental Sciences, Qingdao Marine Science and Technology Center, Qingdao, China
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474
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The North Pacific oligotrophic ocean gyre (NPOG), with low phytoplankton biomass, covers about 40 % of the North Pacific. The variations in NPOG seasonal cycle, which have a greater impact than its annual mean changes, are influenced by the El Niño-Southern Oscillation from 1998 to 2021. However, from 2021 to 2100, a weakened NPOG seasonal cycle is expected due to climate change. These changes in NPOG seasonal cycle could affect fisheries and marine ecosystems.
The North Pacific oligotrophic ocean gyre (NPOG), with low phytoplankton biomass, covers about...