Stratospheric tropical warming event and its impact on the polar and tropical troposphere

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Kodera, Kunihiko, Eguchi, Nawo, Mukougawa, Hitoshi, Nasuno, Tomoe, Hirooka, Toshihiko
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2017
• Subjects: article; Verlagsveröffentlichung; polar night
• Online Access: https://doi.org/10.5194/acp-17-615-2017; https://noa.gwlb.de/receive/cop_mods_00042824; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00042444/acp-17-615-2017.pdf; https://acp.copernicus.org/articles/17/615/2017/acp-17-615-2017.pdf

Stratosphere–troposphere coupling is investigated in relation to middle atmospheric subtropical jet (MASTJ) variations in boreal winter. An exceptional strengthening of the MASTJ occurred in association with a sudden equatorward shift of the stratospheric polar night jet (PNJ) in early December 2011. This abrupt transformation of the MASTJ and PNJ had no apparent relation to the upward propagation of planetary waves from the troposphere. The impact of this stratospheric event penetrated into the troposphere in two regions: in the northern polar region and the tropics. Due to the strong MASTJ, planetary waves at higher latitudes were deflected and trapped in the northern polar region. Trapping of the planetary waves resulted in amplification of zonal wave number 1 component, which appeared in the troposphere as the development of a trough over the Atlantic sector and a ridge over the Eurasian sector. A strong MASTJ also suppressed the equatorward propagation of planetary waves, which resulted in weaker tropical stratospheric upwelling and produced anomalous warming in the tropical stratosphere. In the tropical tropopause layer (TTL), however, sublimation of ice clouds kept the temperature change minor. In the troposphere, an abrupt termination of a Madden–Julian Oscillation (MJO) event occurred following the static stability increase in the TTL. This termination suggests that the stratospheric event affected the convective episode in the troposphere.