High and Low Pressure
Warm air rises at the equator and cold air sinks at the poles. Warm air expands and cool air contracts and compresses.
When it is heated it becomes less dense (i.e. lighter). The more dense (i.e. heavier) magma sinks while the less dense magma rises to the top. It will eventually cool again causing a convection current within the mantle.
Warm water expands and rises, cool water contracts and sinks.
Helium is a gas that is less dense than air. This is why a balloon filled with helium rises when released.
yes the cool denser air sink while the warm less dense rises
It expands, rises, and becomes less dense.
Hot air expands. When it expands, it becomes less dense and rises.
RAIN
precipitation (rain)
This creates clouds and, if there is enough moisture, precipitation.
It expands, rises, and becomes less dense.
Warm air rises at the equator and cold air sinks at the poles. Warm air expands and cool air contracts and compresses.
Water that is heated expands and rises to the surface of the tray. Similarly, the magma expands and rises to the surface of the tray. Similarly, the magma nearer the core expands and rises to top of the mantle.
It expands and cools
Air expands as it is heated, hence, hot air is less dense than cool air. Hence it rises in a surrounding environment of cooler air.
Fluids rise and sink in a convection current due to differences in temperature and density. When a fluid is heated, it becomes less dense and rises, creating an upward flow. As it cools, it becomes more dense and sinks, creating a downward flow. This continuous cycle of heating and cooling drives the convection current.
rising air expands then cools and condenses