Open AccessImpacts of increases in greenhouse gases and ozone recovery on lower stratospheric circulation and the age of air: Chemistry‐climate model simulations up to 2100
Author(s) -
Deushi Makoto,
Shibata Kiyotaka
Publication year - 2011
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2010jd015024
Subject(s) - polar vortex , stratosphere , atmospheric sciences , forcing (mathematics) , climatology , environmental science , ozone , greenhouse gas , ozone layer , sudden stratospheric warming , climate model , atmosphere (unit) , climate change , atmospheric circulation , meteorology , geology , physics , oceanography
Long‐term changes in lower stratospheric wave forcing and the distribution of mean age of air were examined using multidecadal simulations carried out with a chemistry‐climate model in which changes in ozone concentration and the climate of the middle atmosphere were projected through the twenty‐first century. Changes in wave forcing between future (2085–2099) and past (1985–1999) periods show clear seasonal variation in the simulations. In both summer hemispheres, subtropical wave forcing significantly strengthens and extends to the extratropics in the lower stratosphere, with the exception of the Antarctic region where resolved wave forcing is decreased in spring and summer as a result of an earlier breakdown of the polar vortex in the future period. This summer strengthening and extending in wave forcing is likely related to the westerly wind shift of the lower stratospheric easterly wind. In the future period, mean age of air is decreased at all locations and seasons at 50 hPa. However, the decrease is nonuniform in each season and region. A large decrease is simulated over the northern extratropics in summer, in accordance with a strengthened residual circulation. Over the Antarctic, a local maximum decrease appears in December, related to the earlier breakdown of the polar vortex.