JpGU-AGU Joint Meeting 2020

講演情報

[E] 口頭発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS08] 成層圏―対流圏相互作用

コンビーナ:坂崎 貴俊(京都大学 大学院理学研究科)、木下 武也(海洋研究開発機構)、Pu Lin(Princeton University/NOAA Geophysical Fluid Dynamics Laboratory)、Peter Hitchcock(Cornell University)

[AAS08-11] The Coupling between the Troposphere and Stratosphere at Middle and High Latitudes

★Invited Papers

*Wenshou Tian1Jinlong Huang1Ruhua Zhang1Jiankai Zhang1Shiyan Zhang1 (1. College of Atmospheric Sciences, Lanzhou University,China)

キーワード:stratosphere-troposphere coupling, planetary waves, polar vortex, BD circulation

The stratosphere and the troposphere coupling is a hot topic in recent years while the stratospheric polar vortex plays a critical role in this coupling at middle and high latitudes. Up to date, the underlying mechanisms and key processes involved in this coupling are still under wide debate. In this work, the connections of tropospheric blockings, eddy driven jet, planetary waves with the stratospheric polar vortex strength and position are investigated. In addition, the role of the large scale BD circulation played in the stratosphere troposphere dynamical coupling at middle and high latitudes is also discussed. The analysis reveals that the blocking frequency has a close relationship with the stratospheric polar vortex strength and position. The connections between blockings and the polar vortex are controlled by the linear and nonlinear wave interference effects while the BD circulation induced airmass transport can significantly modulate stratosphere troposphere coupling at high latitudes at relatively longer time scales. The thermal-dynamical anomalies in the polar stratosphere can get into the polar troposphere under favorable conditions and we found that it is the duration of upward propagation of planetary waves in mid-high latitude upper troposphere, rather than the wave strength that controls the downward extension of the stratospheric anomalies.