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Autor:
S. Bahramvash Shams, V. P. Walden, J. W. Hannigan, W. J. Randel, I. V. Petropavlovskikh, A. H. Butler, A. de la Cámara
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 5435-5458 (2022)
Stratospheric circulation is a critical part of the Arctic ozone cycle. Sudden stratospheric warming events (SSWs) manifest the strongest alteration of stratospheric dynamics. During SSWs, changes in planetary wave propagation vigorously influence zo
Externí odkaz:
https://doaj.org/article/0bfad23abb8543ed90d2b052353217bd
