WARMFRONT
Warm front
A 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.The above text is a snippet from Wikipedia: Warm front
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warm front
Noun
- A warm front is the trailing edge of a retreating mass of cold air.
The above text is a snippet from Wiktionary: warm front
and as such is available under the Creative Commons Attribution/Share-Alike License.