寒冷低気圧
1. Cold-core lowA cold-core low, also known as a cold low or cold-core cyclone, is a cyclone aloft which has an associated cold pool of air residing at high altitude within the Earth's troposphere. It is a low pressure system which strengthens with height in accordance with the thermal wind relationship. These systems can be referred to as upper level lows.
Read “Cold-core low” on English Wikipedia
Read “寒冷低気圧” on Japanese Wikipedia
Read “Cold-core low” on DBpedia
Read “Cold-core low” on English Wikipedia
Read “寒冷低気圧” on Japanese Wikipedia
Read “Cold-core low” on DBpedia
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