This refers to the calm that occurs in coastal areas in the morning. Sea surface temperatures do not change much throughout the day, but land surface temperatures are lower at night and higher during the day. As a result, land breezes blow from the land to the sea at night, and conversely, sea breezes blow from the sea to the land during the day. When the two types of wind change, the wind stops blowing for a while, and the calm in the morning when the land breeze is replaced by the sea breeze is called a morning calm, and the calm in the evening when the sea breeze is replaced by the land breeze is called an evening calm. Land and Sea Breeze [Asai Tomio] Source: Heibonsha World Encyclopedia, 2nd Edition Information |
海岸地域で朝方現れる無風に近い状態をいう。海面水温は1日を通してあまり変わらないが,陸地面温度は夜間に低く,日中高くなる。そのため,夜間,陸から海に向かう陸風が吹き,日中は逆に海から陸に向かう海風が吹く。両者の交代時にしばらく風が吹かなくなり,陸風から海風に交代する朝方の無風状態を朝なぎ,海風から陸風に交代する夕方のそれを夕なぎevening calmと呼んでいる。海陸風【浅井 冨雄】
出典 株式会社平凡社世界大百科事典 第2版について 情報 |
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