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温暖前線
2. Warm frontA warm front is a density discontinuity located at the leading edge of a homogeneous warm air mass, and is typically located on the equator-facing edge of an isotherm gradient. Warm fronts lie within broader troughs of low pressure than cold fronts, and move more slowly than the cold fronts which usually follow because cold air is denser and less easy to remove from the Earth's surface. This also forces temperature differences across warm fronts to be broader in scale.
Read “Warm front” on English Wikipedia
Read “温暖前線” on Japanese Wikipedia
Read “Warm front” on DBpedia
Read “Warm front” on English Wikipedia
Read “温暖前線” on Japanese Wikipedia
Read “Warm front” on DBpedia
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