在夏天臺北盆地的早晨，熱力作用引發的環流會將潮濕的海風從淡水河口、基隆河谷和大漢溪谷引進盆地內。對流藉著高溫潮濕的空氣逐漸成長茁壯，直到下午時成長成巨大的積雨雲，並造成局部的大雨及雷擊出現。影片記錄了 2024 年 7 月 10 日在臺灣大學發生的午後雷雨，可以看到積雲由小而大、對流降水發生時的複雜過程。
In summer mornings, the sea breeze brings moisture into the Taipei Basin from the Tamsui River mouth, Keelung River Valley, and Dahan River Valley. With the hot and humid air, convections develop into massive cumulonimbus clouds by the afternoon, causing heavy rain and thunderstorms. This video captures the afternoon thunderstorm on July 10, 2024, at National Taiwan University, showing the development of convection and precipitation.
22 авг 2024
