温带气旋 Extratropical cyclone



温带气旋(英语:Extratropical cyclone)是活跃在温带中纬度地区的天气系统,又称为“温带低气压”或“锋面气旋”。
温带气旋是不同于热带气旋的一种冷心系统,其出现伴随着锋面,尺度一般较热带气旋为大,可达几百乃至数千公里。
单词 | Water cyclone |
释义 |
Water cyclone
中文百科
温带气旋 Extratropical cyclone(重定向自Water cyclone)
![]() ![]() ![]() 温带气旋(英语:Extratropical cyclone)是活跃在温带中纬度地区的天气系统,又称为“温带低气压”或“锋面气旋”。 温带气旋是不同于热带气旋的一种冷心系统,其出现伴随着锋面,尺度一般较热带气旋为大,可达几百乃至数千公里。
英语百科
Extratropical cyclone 温带气旋(重定向自Water cyclone)
![]() ![]() ![]() ![]() Extratropical cyclones, sometimes called mid-latitude cyclones or wave cyclones, are low pressure zones, which along with the anticyclones of high pressure zones, drive the weather over much of the Earth. Extratropical cyclones are capable of producing anything from cloudiness and mild showers to heavy gales and thunderstorms. These types of cyclones are defined as large scale (synoptic) low pressure weather systems that occur in the middle latitudes of the Earth. In contrast with tropical cyclones, they produce rapid changes in temperature and dew point along broad lines about the center of the cyclone called fronts. |
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