Frontiers Science Center for Deep Ocean Multispheres and Earth System and Key Laboratory of Marine Environmental Science and Ecology, Ministry of Education, Ocean University of China, and Laoshan Laboratory, Qingdao, 266100, China
Frontiers Science Center for Deep Ocean Multispheres and Earth System and Key Laboratory of Marine Environmental Science and Ecology, Ministry of Education, Ocean University of China, and Laoshan Laboratory, Qingdao, 266100, China
Dan Tong
Department of Earth System Science, Tsinghua University, Beijing, 100084, China
College of Oceanic and Atmospheric Sciences, Ocean University of China, Qingdao, 266100, China
Wenyu Liu
Department of Earth System Science, Tsinghua University, Beijing, 100084, China
Mengshi Cui
Department of Earth System Science, Tsinghua University, Beijing, 100084, China
Xiuwen Guo
Frontiers Science Center for Deep Ocean Multispheres and Earth System and Key Laboratory of Marine Environmental Science and Ecology, Ministry of Education, Ocean University of China, and Laoshan Laboratory, Qingdao, 266100, China
Shaoqing Zhang
Frontiers Science Center for Deep Ocean Multispheres and Earth System and Key Laboratory of Physical Oceanography, Ministry of Education, College of Oceanic and Atmospheric Sciences, Ocean University of China and Laoshan Laboratory, Qingdao, 266100, China
Frontiers Science Center for Deep Ocean Multispheres and Earth System and Key Laboratory of Marine Environmental Science and Ecology, Ministry of Education, Ocean University of China, and Laoshan Laboratory, Qingdao, 266100, China
Lixin Wu
Frontiers Science Center for Deep Ocean Multispheres and Earth System and Key Laboratory of Physical Oceanography, Ministry of Education, College of Oceanic and Atmospheric Sciences, Ocean University of China and Laoshan Laboratory, Qingdao, 266100, China
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2,606
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Total article views: 4,641 (including HTML, PDF, and XML)
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Total article views: 2,035 (including HTML, PDF, and XML)
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Total article views: 2,606 (including HTML, PDF, and XML)
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Unlike traditional numerical studies, we apply a high-resolution Earth system model, improving simulations of surface ozone and large-scale circulations such as atmospheric blocking. Besides local heat waves, we quantify the impact of atmospheric blocking on downstream ozone concentrations, which is closely associated with the blocking position. We identify three major pathways of Rossby wave propagation, stressing the critical role of large-scale circulation in regional air quality.
Unlike traditional numerical studies, we apply a high-resolution Earth system model, improving...
