A cold air mass moves underneath a warm air mass causing the warm air to rise. This brings showers or thunderstorms, followed by cooler weather this event can be identified as-

This event can be identified as a cold front.

The event you are referring to is called an "occluded front." An occluded front occurs when a cold air mass catches up and overtakes a warm air mass. This typically happens in a complex weather system, such as a mid-latitude cyclone.

To identify an occluded front, you can follow these steps:

1. Look for a low-pressure system on a weather map: Occluded fronts often form within the circulation of a low-pressure system, which is represented by a closed isobar (line of constant pressure) contour.

2. Look for a cold front and a warm front converging: An occluded front forms when a cold front catches up with a warm front. On a weather map, a cold front is represented by a solid blue line with blue triangles pointing towards the warm air, while a warm front is represented by a solid red line with red semicircles pointing towards the cold air.

3. Look for a purple line with alternating semicircles and triangles: An occluded front is depicted on weather maps as a purple line with alternating red semicircles and blue triangles. The semicircles and triangles indicate the motion of warm air rising and cool air sinking.

So, by identifying a low-pressure system, a cold front, a warm front, and a purple line with alternating semicircles and triangles on a weather map, you can recognize an occluded front. This weather phenomenon often brings showers or thunderstorms followed by cooler weather due to the mixing of different air masses.

This event can be identified as a cold front. A cold front occurs when a cold air mass moves beneath a warm air mass, causing the warm air to rise rapidly. As the warm air rises, it cools and condenses, forming clouds and leading to the development of showers or thunderstorms. Once the cold front passes, cooler weather typically follows due to the colder air replacing the warmer air mass.