occluded front
Quick Summary
In meteorology, an occluded front forms when a faster-moving cold front catches up to and overtakes a slower-moving warm front. This process lifts the warm air mass completely off the ground, creating a boundary between two masses of cold air. Occluded fronts are often associated with cyclonic storms and can bring varied weather conditions. They are a type of front, which is a transition zone between two air masses of different temperatures and densities.12
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front…the end result is an occluded front. Cyclonic storms in high and middle latitudes often start out as an undulation, or wave, on a frontal boundary between warm and cold air masses. If the wave intensifies, the surface atmospheric pressure at the centre of the cyclone falls. Eventually, the advancing…
Read More…the end result is an occluded front. Cyclonic storms in high and middle latitudes often start out as an undulation, or wave, on a frontal boundary between warm and cold air masses. If the wave intensifies, the surface atmospheric pressure at the centre of the cyclone falls. Eventually, the advancing…
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atmospherePolar fronts and the jet stream…frontal intersection is called an occluded front. Without exception, fronts of all types follow the movement of colder air.
Read More…frontal intersection is called an occluded front. Without exception, fronts of all types follow the movement of colder air.
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