When air is warmed up, its molecules move faster and faster and as a result they move further from each other. They still have the same mass, but they now occupy a larger volume. This means that its density is smaller.
The opposite when air is cooled off. The molecules slow down, get closer together, occupy a smaller volume and therefore its density is bigger.
When air is warmed up, it goes up. Once it's up there, is cools off and goes back down. Near the heated surface the air gets warmed up again, goes up, cools down, goes back down, and again and again.
That's called a convection cell.
Air above a heated surface expands and rises.
When air is warmed up, its molecules move faster and faster and as a result they move further from each other. They still have the same mass, but they now occupy a larger volume. This means that its density is smaller.
The opposite when air is cooled off. The molecules slow down, get closer together, occupy a smaller volume and therefore its density is bigger.
When air is warmed up, it goes up. Once it's up there, is cools off and goes back down. Near the heated surface the air gets warmed up again, goes up, cools down, goes back down, and again and again.
That's called a convection cell.
When the sunlight strikes the snow, the surface of the snow is heated above the air temperature and some melting and evaporation occur.
Convectional precipitation is the type of precipitation caused by air being heated at the surface of the earth. Convectional precipitation can fall anywhere on earth.
because warm air move upwards and cool air due to gravity move closer to the earth surface
In the atmosphere, warm surfaces can heat the air above them. High pressure in the atmosphere is what causes the air to rapidly heat.
when land is heated, the air above it also gets heated, which makes it to start rising. This is due to the fact dat hot air is lighter dan cold one. this gives rise to a phenomenon nwn as convection current. this is the reason of presence of moderate climate in coastal areas.
in a upward motion
how does air above cold surface move
Air above a cold or cooled surface contracts and falls.
Sunlight is absorbed by the surface of the desert and the surface is heated. The surface, in turn, heats the air above the desert.
POOOOOOP
The air is thinner the higher you go.
The air is thinner the higher you go.
1000
Sunlight is absorbed by the surface of the soil which is heated. The soil then radiates that heat to the air above it, raising the temperature of the desert.
When air is warmed up, its molecules move faster and faster and as a result they move further from each other. They still have the same mass, but they now occupy a larger volume. This means that its density is smaller.The opposite when air is cooled off. The molecules slow down, get closer together, occupy a smaller volume and therefore its density is bigger.When air is warmed up, it goes up. Once it's up there, is cools off and goes back down. Near the heated surface the air gets warmed up again, goes up, cools down, goes back down, and again and again.That's called a convection cell.
When the sunlight strikes the snow, the surface of the snow is heated above the air temperature and some melting and evaporation occur.
It moves up because therefore hot air rises and cold air sinks... it would be like evaporation except not because its air.