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Science (New York, N.Y.)
|December 24, 1971
PubMed
まとめ

平原の雷雨は,下層平流と上層熱帯圏の水蒸気を大幅に増加させる. 空中での測定は,晴れた天候条件と比較して,水蒸気質量の3倍の増加を明らかにしました.

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