ブリューワー・ドブソン循環
1. Brewer-Dobson circulationBrewer-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.
Read “Brewer-Dobson circulation” on English Wikipedia
Read “ブリューワー・ドブソン循環” on Japanese Wikipedia
Read “Brewer-Dobson circulation” on DBpedia
Read “Brewer-Dobson circulation” on English Wikipedia
Read “ブリューワー・ドブソン循環” on Japanese Wikipedia
Read “Brewer-Dobson circulation” on DBpedia
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