| Literature DB >> 33935342 |
Chunzai Wang1,2,3, Yulong Yao1,2,3, Haili Wang1,2,3, Xiubao Sun1,2,3, Jiayu Zheng1,2,3.
Abstract
China experienced significant flooding in the summer of 2020 and multiple extreme cold surges during the winter of 2020/21. Additionally, the 2020 typhoon season had below average activity with especially quiet activity during the first half of the season in the western North Pacific (WNP). Sea surface temperature changes in the Pacific, Indian, and Atlantic Oceans all contributed to the heavy rainfall in China, but the Atlantic and Indian Oceans seem to have played dominant roles. Enhancement and movement of the Siberian High caused a wavier pattern in the jet stream that allowed cold polar air to reach southward, inducing cold surges in China. Large vertical wind shear and low humidity in the WNP were responsible for fewer typhoons in the first half of the typhoon season. Although it is known that global warming can increase the frequency of extreme weather and climate events, its influences on individual events still need to be quantified. Additionally, the extreme cold surge during 16-18 February 2021 in the United States shares similar mechanisms with the winter 2020/21 extreme cold surges in China. © Institute of Atmospheric Physics/Chinese Academy of Sciences, and Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2021.Entities:
Keywords: climate change; climate variability; extreme weather and climate events; summer floods; typhoon activity; winter cold surge
Year: 2021 PMID: 33935342 PMCID: PMC8074705 DOI: 10.1007/s00376-021-1094-y
Source DB: PubMed Journal: Adv Atmos Sci ISSN: 0256-1530 Impact factor: 3.158