夏季夜間における山麓冷気流の集積・流出過程に関する研究

書誌事項

タイトル別名
  • FILLING PROCESS IN A VALLEY AND OUTFLOW PROCESS INTO A BUILT-UP AREA OF COLD AIR DRAINAGE ON SUMMER NIGHT
  • カキ ヤカン ニ オケル サンロク レイキリュウ ノ シュウセキ リュウシュツ カテイ ニ カンスル ケンキュウ

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抄録

Filling process in a valley and outflow process into a built-up area of cold air drainage are examined by a measurement and a model calculation. The valley faces a built-up area in Kobe city. Air temperature in the bottom of the valley is the lowest. This can be thought to reflect on the filling process of cold air drainage in a valley. When wide area land and sea breezes blow in this area, the cold air filled in the bottom of the valley is mixed, and it is blown away by wide area land and sea breezes. From the vertical potential temperature profile, the thickness of the cold air in the bottom of the valley is thicker than that of previous study on the slope.

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