Stratospheric warming in Southern Hemisphere high latitudes since 1979

• Main Authors: Hu, Y., Fu, Q.
• Other Authors: Hu, Y (reprint author), Peking Univ, Dept Atmospher Sci, Beijing 100871, Peoples R China., Peking Univ, Dept Atmospher Sci, Beijing 100871, Peoples R China., Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA.
• Format: Journal/Newspaper
• Language: English
• Published: atmospheric chemistry and physics 2009
• Subjects: PLANETARY WAVE ACTIVITY; ATLANTIC CLIMATE-CHANGE; OZONE DEPLETION; TEMPERATURE TRENDS; MSU CHANNEL-2; TROPOSPHERE; REANALYSIS; OCEAN; SIMULATIONS; EXCHANGE; Antarctic; The Antarctic; Antarc*
• Online Access: https://hdl.handle.net/20.500.11897/396751

In the present study, we show evidence of significant stratospheric warming over Southern Hemisphere high latitudes and large portions of the Antarctic polar region in winter and spring seasons, with a maximum warming of 7-8 degrees C in September and October, using satellite Microwave Sounding Unit observations for 1979-2006. It is found that this warming is associated with increasing wave activity from the troposphere into the stratosphere, suggesting that the warming is caused by enhanced wave-driven adiabatic heating. We show that the stratospheric warming in Southern Hemisphere high latitudes has close correlations with sea surface temperature (SST) increases, and that general circulation model simulations forced with observed time-varying SSTs reproduce similar warming trend patterns in the Antarctic stratosphere. The simulated stratospheric warming is closely related to increasing wave activity in the Southern Hemisphere. These findings suggest that the stratospheric warming is likely induced by SST warming. As SST warming continues as a consequence of greenhouse gas increases due to anthropogenic activity, the stratospheric warming would also continue, which has important implications to the recovery of the Antarctic ozone hole. Meteorology & Atmospheric Sciences SCI(E) 0 ARTICLE 13 4329-4340 9