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bn:16649800n
Noun Concept
JA
大気の対流
EN
Atmospheric convection is the result of a parcel-environment instability in the atmosphere. Wikipedia
Relations
Sources
IS A
対流
HAS KIND
EN
snow squall
EN
flanking line
HAS INSTANCE
雷雨
俄雨
EN
April shower
FACET OF
気象学
Wikidata
JA
大気の対流

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