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  2. Weather front - Wikipedia

    en.wikipedia.org/wiki/Weather_front

    Stationary fronts either dissipate after several days or devolve into shear lines, but they can transform into a cold or warm front if the conditions aloft change. Stationary fronts are marked on weather maps with alternating red half-circles and blue spikes pointing opposite to each other, indicating no significant movement.

  3. Surface weather analysis - Wikipedia

    en.wikipedia.org/wiki/Surface_weather_analysis

    Occluded fronts usually form around low pressure systems in the mature or late stages of their life cycle, but some continue to deepen after occlusion, and some do not form occluded fronts at all. The weather associated with an occluded front includes a variety of cloud and precipitation patterns, including dry slots and banded precipitation.

  4. 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.

  5. Stationary front - Wikipedia

    en.wikipedia.org/wiki/Stationary_front

    Stationary front symbol: solid line of alternating blue spikes pointing to the warmer air mass and red domes pointing to the colder air mass. A stationary front (or quasi-stationary front) is a weather front or transition zone between two air masses when each air mass is advancing into the other at speeds less than 5 knots (about 6 miles per hour or about 9 kilometers per hour) at the ground ...

  6. Cold front - Wikipedia

    en.wikipedia.org/wiki/Cold_front

    Occluded fronts have an area of warm air aloft. When such a feature forms poleward of an extratropical cyclone, it is known as a trowal, which is short for TRough Of Warm Air aLoft. [14] A cold front is re-designated a warm front if it begins to retreat ahead of the next extratropical cyclone along the frontal boundary, and called a stationary ...

  7. Synoptic scale meteorology - Wikipedia

    en.wikipedia.org/wiki/Synoptic_scale_meteorology

    Warm fronts are usually preceded by stratiform precipitation and fog. The weather usually clears quickly after a front's passage. Some fronts produce no precipitation and little cloudiness, although there is invariably a wind shift. [19] Cold fronts and occluded fronts generally move from west to east, while warm fronts move poleward. Because ...

  8. Portal:Weather/Selected article/8 - Wikipedia

    en.wikipedia.org/wiki/Portal:Weather/Selected...

    Warm fronts are usually preceded by stratiform precipitation and fog. The weather usually clears quickly after a front's passage. Some fronts produce no precipitation and little cloudiness, although there is invariably a wind shift. Cold fronts and occluded fronts generally move from west to east, while warm fronts move poleward. Because of the ...

  9. Surface map - Wikipedia

    en.wikipedia.org/wiki/Surface_map

    Include warm fronts, cold fronts, stationary fronts, and occluded fronts. Represented with specific symbols (e.g., triangles for cold fronts, semicircles for warm ...