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Nearly all chemistry–climate models (CCMs) have a systematic bias of a delayed springtime breakdown of the Southern Hemisphere (SH) stratospheric polar vortex, implying insufficient stratospheric wave drag. In this study the Canadian Middle Atmosph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::89f0fd993bf9a182f7dc820858f842d3
https://centaur.reading.ac.uk/31545/1/McLandress2012JAS.pdf
https://centaur.reading.ac.uk/31545/1/McLandress2012JAS.pdf