| Literature DB >> 32742282 |
Blanca Ayarzagüena1,2, Lorenzo M Polvani3, Ulrike Langematz4, Hideharu Akiyoshi5, Slimane Bekki6, Neal Butchart7, Martin Dameris8, Makoto Deushi9, Steven C Hardiman7, Patrick Jöckel8, Andrew Klekociuk10, Marion Marchand6, Martine Michou11, Olaf Morgenstern12, Fiona M O'Connor7, Luke D Oman13, David A Plummer14, Laura Revell15,16, Eugene Rozanov15, David Saint-Martin11, John Scinocca14, Andrea Stenke15, Kane Stone17,18, Yousuke Yamashita5, Kohei Yoshida9, Guang Zeng12.
Abstract
Major stratospheric sudden warmings (SSWs) are the largest instance of wintertime variability in the Arctic stratosphere. Due to their relevance for the troposphere-stratosphere system, several previous studies have focused on their potential response to anthropogenic forcings. However, a wide range of results have been reported, from a future increase in the frequency of SSWs to a decrease. Several factors might explain these contradictory results, notably the use of different metrics for the identification of SSWs, and the impact of large climatological biases in single-model studies. Here we revisit the question of future SSWs changes, using an identical set of metrics applied consistently across 12 different models participating in the Chemistry Climate Model Initiative. From analyzing future integrations we find no statistically significant change in the frequency of SSWs over the 21st century, irrespective of the metric used for the identification of SSWs. Changes in other SSWs characteristics, such as their duration and the tropospheric forcing, are also assessed: again, we find no evidence of future changes over the 21st century.Year: 2018 PMID: 32742282 PMCID: PMC7394248
Source DB: PubMed Journal: Atmos Chem Phys ISSN: 1680-7316 Impact factor: 6.133