When warm air meets moist air, the warm air rises due to being less dense than the cooler moist air. As the warm air rises, it cools and condenses, forming clouds and precipitation. This process of rising warm air creates a region of lower pressure at the surface.
Rain typically occurs when there are clouds in the sky, and the air is moist and unstable. This often happens in regions where warm, moist air rises and cools, leading to condensation and the formation of raindrops.
it gets warmer
When a cyclone forms, warm, moist air over the ocean rises up from the ocean surface. As this warm, moist air rises, it cools off, and the water in the air forms clouds. The cycle keeps going because air rushes in to fill the void left as the warm moist air rises. This new air also becomes warm and moist and so it rises, too. Again, the cycle continues. Warm air rises, the surrounding air swirls in to take its place, and so on. The whole system of clouds and wind spins and grows, because it is being constantly fed by the ocean's heat and water evaporating from the surface. This causes massive rain clouds to develop.
Warm air rises, and cool air sinks.
As warm, moist air rises in the atmosphere, it cools and condenses, forming clouds and eventually leading to the possibility of precipitation such as rain or snow.
Evaporation.
When warm moist air rises, it cools, causing the water vapor it contains to condense and form clouds. As the air continues to rise, this condensation can lead to precipitation such as rain, snow, or hail. This process is known as adiabatic cooling and is responsible for the formation of most weather phenomena.
When warm air meets moist air, the warm air rises due to being less dense than the cooler moist air. As the warm air rises, it cools and condenses, forming clouds and precipitation. This process of rising warm air creates a region of lower pressure at the surface.
it gets warmer as it rises
The warm moist air rises along the western side of the mountain, cools as it gains altitude, and condenses, forming clouds and precipitation. This process is known as orographic lifting, and it leads to increased rainfall on the windward side of the mountain.
Warm moist air rises because it is less dense than the surrounding cool air. As the warm air rises, it expands and cools, leading to condensation and the formation of clouds and precipitation. This process is known as convection.
Warm, humid air which rises in an unstable environment. Often, this happens as a cold front sweeps into a warm, humid region, driving up the warm, moist air into a region where it quickly condenses due to temperature and pressure changes.
Rain typically occurs when there are clouds in the sky, and the air is moist and unstable. This often happens in regions where warm, moist air rises and cools, leading to condensation and the formation of raindrops.
it gets warmer
When a cyclone forms, warm, moist air over the ocean rises up from the ocean surface. As this warm, moist air rises, it cools off, and the water in the air forms clouds. The cycle keeps going because air rushes in to fill the void left as the warm moist air rises. This new air also becomes warm and moist and so it rises, too. Again, the cycle continues. Warm air rises, the surrounding air swirls in to take its place, and so on. The whole system of clouds and wind spins and grows, because it is being constantly fed by the ocean's heat and water evaporating from the surface. This causes massive rain clouds to develop.
it rises