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  2. Occluded front - Wikipedia

    en.wikipedia.org/wiki/Occluded_front

    Occluded fronts usually form around mature low pressure areas.There are two types of front occlusions, warm and cold, depending on the temperature contrast: . In a cold occlusion, the cold air mass that overtakes the warm air mass ahead is colder than the cool air at the very front and plows under both air masses, and often has the characteristics of a cold front.

  3. Weather front - Wikipedia

    en.wikipedia.org/wiki/Weather_front

    Occluded front depiction for the Northern Hemisphere. An occluded front is formed when a cold front overtakes a warm front, [10] and usually forms around mature low-pressure areas, including cyclones. [2] The cold and warm fronts curve naturally poleward into the point of occlusion, which is also known as the triple point. [11]

  4. Surface weather analysis - Wikipedia

    en.wikipedia.org/wiki/Surface_weather_analysis

    The weather associated with an occluded front includes a variety of cloud and precipitation patterns, including dry slots and banded precipitation. Cold, warm and occluded fronts often meet at the point of occlusion or triple point. [28] A guide to the symbols for weather fronts that may be found on a weather map: 1. cold front 2. warm front

  5. Frontogenesis - Wikipedia

    en.wikipedia.org/wiki/Frontogenesis

    Frontogenesis is a meteorological process of tightening of horizontal temperature gradients to produce fronts. In the end, two types of fronts form: cold fronts and warm fronts. A cold front is a narrow line where temperature decreases rapidly. A warm front is a narrow line of warmer temperatures and essentially where much of the precipitation ...

  6. Cold front - Wikipedia

    en.wikipedia.org/wiki/Cold_front

    The triple point is the intersection of the cold, warm, and occluded fronts. Cold fronts form when a cooler air mass moves into an area of warmer air in the wake of a developing extratropical cyclone. The warmer air interacts with the cooler air mass along the boundary, and usually produces precipitation. Cold fronts often follow a warm front ...

  7. Warm front - Wikipedia

    en.wikipedia.org/wiki/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 ...

  8. Cold hands are common in winter. When are they a sign of a ...

    www.aol.com/lifestyle/cold-hands-common-winter...

    The most effective ways to warm up cold hands. It sounds obvious, but if cold hands are a problem, limiting how much time you spend in chilly environments — whether that’s outdoors in the ...

  9. Air mass - Wikipedia

    en.wikipedia.org/wiki/Air_mass

    Some fronts produce no precipitation and little cloudiness, although there is invariably a wind shift. [10] Cold fronts and occluded fronts generally move from west to east, while warm fronts move poleward. Because of the greater density of air in their wake, cold fronts and cold occlusions move faster than warm fronts and warm occlusions.