When air becomes warm, it expands and becomes less dense, causing it to rise. This can lead to the formation of clouds and eventually precipitation. In water, warmth can increase its evaporation rate and decrease its density, causing it to rise as well.
The water vapor melts and it goes into the mountain
Air pressure is simply the weight of the air above you. Air pressure falls with height because the higher you go up, the less air there is above you to weigh down on you.
I. The cold air mass is pushed underneath the warm air mass.
The warm air mass
When air is directly over a warm surface, it heats up and becomes less dense. This causes the air to rise, creating an area of low pressure at the surface. As the warm air rises, it cools and condenses, forming clouds and potentially leading to the development of thunderstorms or other weather phenomena.
it becomes water vapour in the air
it becomes a warm front
stuff
have less weight
It condenses and it becomes liquid
Cold air is more dense than warm air
As warm air rises, it expands and becomes less dense. This causes it to cool down, leading to the formation of clouds and potentially precipitation. The movement of warm air rising is part of the process known as convection.
Condensation occurs on cans when the cold surface of the can comes into contact with warm, moist air. The warm air cools upon contact with the cold surface of the can, causing the moisture in the air to condense into water droplets.
The water vapor melts and it goes into the mountain
Cool breeze flows when this happens. The water vapor then condenses.
It's the other way round - when air becomes warm, it rises.
Warm air and warm water. Cold air and cold water keep ice cooler longer.