Adaption to environment.
When warm air is lifted up over cold air, it is called "overrunning" or "warm air advection." This process leads to the warm air rising, cooling, and condensing to form clouds and precipitation as it interacts with the cold air at the surface.
When a cold FRONT catches up to a warm FRONT it is called an occluded front.When a cold AIR MASS displaces a warmer AIR MASS it is a cold front.Occluded front
When a cold air mass catches up to a warm air mass, it is called a cold front. At a cold front, the cold air replaces the warm air, creating a boundary between the two air masses. This can result in the formation of clouds, precipitation, and potentially severe weather.
When a cold front overtakes a warm front, it is known as an occluded front. This occurs when the cold air behind the cold front catches up with the warm air ahead of the warm front, forcing the warm air upward.
An occluded front.
When a cold air mass catches up to a warm air mass, it is called a cold front. This phenomenon typically leads to a rapid drop in temperature and often results in precipitation, as the warm air is forced to rise over the denser cold air. Cold fronts are associated with stormy weather and can bring thunderstorms or heavy rainfall.
A warm air mass advancing under a cold air mass is called an occluded front. This occurs when a fast-moving cold front catches up to a slow-moving warm front, lifting the warm air off the ground. The mixing of air masses can lead to cloud formation and precipitation.
Persiptaton
A merging of a cold front and warm front is called an occluded front. This occurs when a fast-moving cold front catches up to a slow-moving warm front, lifting the warm air off the ground and forming a distinct type of front.
The region where a warm front and a cold front meet is called an occluded front. This occurs when a fast-moving cold front catches up to a slower-moving warm front, lifting the warm air mass off the ground. This creates a boundary where three air masses converge.
When a warm air mass catches up with a cold air mass, it is known as an occluded front. At this point, the warm air mass is forced aloft as the faster-moving cold front overtakes the slower-moving warm front. This results in cooler temperatures and often precipitation.
It is called a lower pressure front.