Dynamic Processes of the Arctic Stratosphere in the 2020–2021 Winter

dc.contributor.author	Vargin P.N.
dc.contributor.author	Guryanov V.V.
dc.contributor.author	Lukyanov A.N.
dc.contributor.author	Vyzankin A.S.
dc.date.accessioned	2022-02-09T20:30:23Z
dc.date.available	2022-02-09T20:30:23Z
dc.date.issued	2021
dc.identifier.issn	0001-4338
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/168618
dc.description.abstract	Abstract: The Arctic stratosphere winter season of 2020–2021 was characterized by a weakened stratospheric polar vortex as a result of a major sudden stratospheric warming (SSW) in early January. After the SSW, which persisted for about 3 weeks, and until the end of the winter season, the lower stratosphere temperature inside the stratospheric polar vortex remained higher than required for the formation of polar stratospheric clouds.
dc.relation.ispartofseries	Izvestiya - Atmospheric and Ocean Physics
dc.subject	Arctic stratosphere
dc.subject	planetary waves
dc.subject	sudden stratospheric warming
dc.subject	trajectory modeling
dc.title	Dynamic Processes of the Arctic Stratosphere in the 2020–2021 Winter
dc.type	Article
dc.relation.ispartofseries-issue	6
dc.relation.ispartofseries-volume	57
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	568
dc.source.id	SCOPUS00014338-2021-57-6-SID85121772830

Files in this item

Name: SCOPUS00014338-20 ...

Size: 52.24Kb

Format: PDF

Публикации сотрудников КФУ Scopus [24551]
Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.