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- Q4411671 subject Q7110105.
- Q4411671 abstract "Brewer-Dobson circulation is a model of atmospheric circulation, proposed by Alan Brewer in 1949 and Gordon Dobson in 1956, which attempts to explain why tropical air has less ozone than polar air, even though the tropical stratosphere is where most atmospheric ozone is produced. It is a simple circulation model that posits the existence of a slow current in the winter hemisphere which redistributes air from the tropics to the extratropics. The Brewer-Dobson circulation is driven by atmospheric waves and may be speeding up due to climate change.".
- Q4411671 thumbnail Nimbus_ozone_Brewer-Dobson_circulation.jpg?width=300.
- Q4411671 wikiPageExternalLink index.htm.
- Q4411671 wikiPageWikiLink Q108376.
- Q4411671 wikiPageWikiLink Q12507.
- Q4411671 wikiPageWikiLink Q2623243.
- Q4411671 wikiPageWikiLink Q36933.
- Q4411671 wikiPageWikiLink Q4698318.
- Q4411671 wikiPageWikiLink Q4706240.
- Q4411671 wikiPageWikiLink Q673756.
- Q4411671 wikiPageWikiLink Q709194.
- Q4411671 wikiPageWikiLink Q7110105.
- Q4411671 wikiPageWikiLink Q740585.
- Q4411671 wikiPageWikiLink Q757526.
- Q4411671 comment "Brewer-Dobson circulation is a model of atmospheric circulation, proposed by Alan Brewer in 1949 and Gordon Dobson in 1956, which attempts to explain why tropical air has less ozone than polar air, even though the tropical stratosphere is where most atmospheric ozone is produced. It is a simple circulation model that posits the existence of a slow current in the winter hemisphere which redistributes air from the tropics to the extratropics.".
- Q4411671 label "Brewer-Dobson circulation".
- Q4411671 depiction Nimbus_ozone_Brewer-Dobson_circulation.jpg.