JpGU-AGU Joint Meeting 2020

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS08] Stratosphere-troposphere interaction

convener:Takatoshi Sakazaki(Graduate School of Science, Kyoto University), Takenari Kinoshita(Japan Agency for Marine-Earth Science and Technology), Pu Lin(Princeton University/NOAA Geophysical Fluid Dynamics Laboratory), Peter Hitchcock(Cornell University)

[AAS08-12] A pause in Southern Hemisphere circulation trends due to the Montreal Protocol

★Invited Papers

*Antara Banerjee1,2, John C. Fyfe3, Lorenzo M. Polvani4, Darryn Waugh5,6, Kai-Lan Chang1,2 (1.Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, USA, 2.Chemical Sciences Division, National Oceanic and Atmospheric Administration/Earth System Research Laboratory, Boulder, Colorado, USA, 3.Canadian Centre for Climate Modelling and Analysis, Environment and Climate Change Canada, Victoria, British Columbia, Canada, 4.Department of Applied Physics and Applied Mathematics, Columbia University, New York, NY, USA, 5.Department of Earth and Planetary Sciences, The John Hopkins University, Baltimore, Maryland, USA., 6.School of Mathematics and Statistics, University of New South Wales, Sydney, New South Wales, Australia)

Keywords:Atmospheric Dynamics, Chemistry-Climate Interactions, Stratosphere-Troposphere Interactions, Detection and Attribution

Observations show robust near-surface trends in the Southern Hemisphere tropospheric circulation towards the end of the 20th century, including a poleward shift in the midlatitude jet, a positive trend in the Southern Annular Mode, and an expansion of the Hadley cell. It is established that these trends have been driven by ozone depletion in the Antarctic stratosphere due to emissions of ozone-depleting substances. Here we show that these widely reported circulation trends have, in fact, paused, or slightly reversed, around the year 2000. Using a pattern-based detection and attribution analysis of atmospheric zonal wind, we show that the pause in circulation trends is forced by human activities, and has not occurred simply due to internal or natural variability of the climate system. Further, we demonstrate the essential role of stratospheric ozone recovery as a result of the Montreal Protocol in driving the pause through stratosphere-troposphere coupling. Since the pre-2000 circulation trends have impacted precipitation, and potentially, the ocean circulation and salinity, we anticipate that a pause in these trends will have wider impacts on the Earth system. Signatures of the Montreal Protocol and the associated stratospheric ozone recovery might therefore manifest, or might have already manifested, in other aspects of the Earth system.