線状降水帯 / linear rainband
線状降水帯 (senjō kōsuitai) refers to a linear rainband, a weather phenomenon where a line of intense rain clouds forms over the same area, causing prolonged heavy rainfall. This can lead to severe flooding and landslides, especially during Japan’s rainy season and typhoon periods. In recent years, 線状降水帯 has become a key term in weather forecasts and disaster prevention alerts due to its potential for significant damage.
Curious to hear more about it? Want to learn how to pronounce it? Watch or listen to Episode 92 using the below link 