Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters (CIC-FEMD), Nanjing University of Information
Science and Technology, Nanjing, 210044, China
Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters (CIC-FEMD), Nanjing University of Information
Science and Technology, Nanjing, 210044, China
Xiaoye Yang
Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters (CIC-FEMD), Nanjing University of Information
Science and Technology, Nanjing, 210044, China
Ruixi Wu
Meteorological Bureau of Jiading District, Shanghai, 201815, China
Zhicong Yin
Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters (CIC-FEMD), Nanjing University of Information
Science and Technology, Nanjing, 210044, China
Southern Marine Science and Engineering Guangdong Laboratory
(Zhuhai), Zhuhai, 519080, China
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2,507
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2,061
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Supplement: 122
BibTeX: 69
EndNote: 94
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446
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10
661
150
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HTML: 446
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Total: 661
Supplement: 150
BibTeX: 6
EndNote: 8
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Total article views: 3,560 (including HTML, PDF, and XML)
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Total article views: 2,899 (including HTML, PDF, and XML)
Thereof 2,870 with geography defined
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Total article views: 661 (including HTML, PDF, and XML)
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This study classified the winter cold surge in eastern China into blocking cold surge and wave-train cold surge and investigated the difference of haze dispersion ability between the two types. The results show that the haze dispersion of blocking cold surge is weaker than that of wave-train cold surge. In the past 4 decades, the frequency of wave-train (blocking) cold surge shows a downward (upward) trend, which means that the ability of cold surge to disperse haze is declining.
This study classified the winter cold surge in eastern China into blocking cold surge and...
