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Speeding extreme cold events under global warming
Regional anthropogenic warming caused stronger and shorter cold events in the winter (December–February) of 2020–21, with the strongest cooling of −10 °C covering an area of 1.63 × 10 ^7 km ^2 over East Asia. In contrast to previous cold events, the extreme cold events in 2020–21 were a result of meridional circulation change due to stronger regional anthropogenic warming. Our results show a multi-aspect anthropogenic effect in the process of cold events, and illustrate that anthropogenic effect played a role not only in the thermodynamic process but also in the dynamic process. The exchange of equilibrium from low to high index does not take fewer cold events anymore; new principles on equilibrium have appeared and will soon play an effect in more fields of climate change.
Speeding extreme cold events under global warming
Regional anthropogenic warming caused stronger and shorter cold events in the winter (December–February) of 2020–21, with the strongest cooling of −10 °C covering an area of 1.63 × 10 ^7 km ^2 over East Asia. In contrast to previous cold events, the extreme cold events in 2020–21 were a result of meridional circulation change due to stronger regional anthropogenic warming. Our results show a multi-aspect anthropogenic effect in the process of cold events, and illustrate that anthropogenic effect played a role not only in the thermodynamic process but also in the dynamic process. The exchange of equilibrium from low to high index does not take fewer cold events anymore; new principles on equilibrium have appeared and will soon play an effect in more fields of climate change.
Speeding extreme cold events under global warming
Xiaodan Guan (author) / Zhaokui Gao (author) / Jianping Huang (author) / Chenyu Cao (author) / Kaiwei Zhu (author) / Jiamin Wang (author)
2022
Article (Journal)
Electronic Resource
Unknown
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