Journal
ATMOSPHERIC SCIENCE LETTERS
Volume 12, Issue 2, Pages 228-232Publisher
WILEY-BLACKWELL
DOI: 10.1002/asl.318
Keywords
El Nino; STE; tropospheric ozone; stratospheric ozone
Funding
- NERC
- NCAS (UK)
- IKY (Greece)
- Natural Environment Research Council [ncas10009] Funding Source: researchfish
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The stratosphere can strongly influence the interannual variability of tropospheric ozone. It has been discussed previously that tropospheric ozone can increase following an El Nino event, due to enhanced stratosphere/troposphere exchange (STE) of ozone. Here, we run a chemical-transport model for 5 years, covering a period including a strong El Nino event (1997-1998), and find that variability of ozone in the stratosphere is an almost negligible driver of modelled post-El Nino increases of ozone STE and tropospheric ozone abundances. Changes in the dynamics, affecting the cross-tropopause air-mass flux, may be far more important in driving these anomalies. Copyright. (C) 2011 Royal Meteorological Society
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