an occluded front.
When a warm air mass is trapped between two cool air masses, it creates a weather pattern known as a frontal boundary. This can lead to the development of thunderstorms, strong winds, and other types of severe weather as the warm air tries to move over the denser cool air masses. Ultimately, the interaction of these air masses can lead to the formation of cold and warm fronts.
when to air masses meet it's called a front.
A front. There are several kinds of fronts, depending upon the conditions in which the air clashes. Some are Warm fronts, Cold fronts, Occluded fronts, and Stationary fronts.
No, as cold air is denser.
im cool
No
When two cool air masses cut off a warm air mass from the ground, a stationary front forms. Stationary fronts occur when the boundary between two air masses stalls and neither one advances. This can lead to prolonged periods of cloudy, rainy weather.
A stationary front typically involves three air masses of different temperatures - warm air, cold air, and cool air. This front occurs when a warm air mass is positioned between a cold air mass and a cool air mass, leading to little to no horizontal movement of the air masses.
The cool air sinks, while the warm air rises. If it does so with enough force and torque, a tornado or hurricane will form.
Maritime polar air masses have more effect on the west coast due to the prevailing westerly winds that bring these air masses from the Pacific Ocean. The west coast is more influenced by these moist and cool air masses, leading to more precipitation and cooler temperatures. In contrast, the east coast is shielded by the Appalachian Mountains, which hinder the penetration of maritime polar air masses from the Atlantic Ocean.
The upward movement of warm air is called convection, while the downward movement of cool air is called subsidence. This process occurs due to differences in temperature, density, and pressure in the atmosphere, leading to the circulation of air masses.
Cold dry air masses are typically referred to as continental polar (cP) air masses. These air masses originate over cold, dry land areas and tend to bring cool temperatures and low humidity to the regions they affect.