たいきじゅんかん
大気循環
1. atmospheric circulation
2. Atmospheric circulationAtmospheric circulation is the large-scale movement of air, and the means (together with the smaller ocean circulation) by which thermal energy is distributed on the surface of the Earth. The large-scale structure of the atmospheric circulation varies from year to year, but the basic climatological structure remains fairly constant.
Read “Atmospheric circulation” on English Wikipedia
Read “大気循環” on Japanese Wikipedia
Read “Atmospheric circulation” on DBpedia
Read “Atmospheric circulation” on English Wikipedia
Read “大気循環” on Japanese Wikipedia
Read “Atmospheric circulation” on DBpedia
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