Articles | Volume 17, issue 3
Atmos. Chem. Phys., 17, 2437–2458, 2017
Atmos. Chem. Phys., 17, 2437–2458, 2017

Research article 15 Feb 2017

Research article | 15 Feb 2017

How does downward planetary wave coupling affect polar stratospheric ozone in the Arctic winter stratosphere?

Sandro W. Lubis1,a, Vered Silverman2, Katja Matthes1,3, Nili Harnik2,4, Nour-Eddine Omrani5, and Sebastian Wahl1 Sandro W. Lubis et al.
  • 1GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
  • 2Department of Geophysical, Atmospheric and Planetary Sciences, Tel Aviv University, Tel Aviv, Israel
  • 3Christian-Albrechts Universität zu Kiel, Kiel, Germany
  • 4Department of Meteorology, University of Stockholm, Stockholm, Sweden
  • 5Geophysical Institute, University of Bergen and Bjerknes Centre for Climate Research, Bergen, Norway
  • aCurrent affiliation: Department of Geophysical Sciences, University of Chicago, Chicago, Illinois, USA

Abstract. It is well established that variable wintertime planetary wave forcing in the stratosphere controls the variability of Arctic stratospheric ozone through changes in the strength of the polar vortex and the residual circulation. While previous studies focused on the variations in upward wave flux entering the lower stratosphere, here the impact of downward planetary wave reflection on ozone is investigated for the first time. Utilizing the MERRA2 reanalysis and a fully coupled chemistry–climate simulation with the Community Earth System Model (CESM1(WACCM)) of the National Center for Atmospheric Research (NCAR), we find two downward wave reflection effects on ozone: (1) the direct effect in which the residual circulation is weakened during winter, reducing the typical increase of ozone due to upward planetary wave events and (2) the indirect effect in which the modification of polar temperature during winter affects the amount of ozone destruction in spring.

Winter seasons dominated by downward wave reflection events (i.e., reflective winters) are characterized by lower Arctic ozone concentration, while seasons dominated by increased upward wave events (i.e., absorptive winters) are characterized by relatively higher ozone concentration. This behavior is consistent with the cumulative effects of downward and upward planetary wave events on polar stratospheric ozone via the residual circulation and the polar temperature in winter. The results establish a new perspective on dynamical processes controlling stratospheric ozone variability in the Arctic by highlighting the key role of wave reflection.

Short summary
Downward wave coupling (DWC) events impact high-latitude stratospheric ozone in two ways: (1) reduced dynamical transport of ozone from low to high latitudes during individual events and (2) enhanced springtime chemical destruction of ozone via the cumulative impact of DWC events on polar stratospheric temperatures. The results presented here broaden the scope of the impact of wave–mean flow interaction on stratospheric ozone by highlighting the key role of wave reflection.
Final-revised paper