Source: wikibot/brewer-dobson-circulation
= Brewer–Dobson circulation
{wiki=Brewer–Dobson_circulation}
Brewer–Dobson circulation is a large-scale atmospheric circulation pattern in the stratosphere, primarily occurring in the tropical regions and influencing the distribution of ozone in the atmosphere. This circulation is named after two scientists, Sir Gordon Brewer and John Dobson, who contributed to the understanding of stratospheric processes.