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global wind patterns

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Q: The tendency for warm air to rise and cool air to sink results in?
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The tendency for warm air to rise and cool air to sink results in what?

The tendency for warm air to rise and cool air to sink results in convection currents. As warm air rises, it cools and then sinks back down in a continuous loop, creating circulation patterns in the atmosphere. This process helps distribute heat and moisture around the Earth.


What is the result in the tendency for warm air to rise and cool air to sink?

The result of warm air rising and cool air sinking is convection currents of air, causing wind. Even hurricanes are caused by this phenomenon.


How does temperature affect air movement?

the hot air will rise and the cool air will sink


Why does got air rise and cold air sink?

Hot air is lighter while cold air is heavier. This results in warm or hot air rising and cool or cold air falls.


Do you use convection when you use heat?

convection is the movement caused within a fluid by the tendency of hotter and therefore less dense material to rise, and colder, denser material to sink under the influence of gravity, which consequently results in transfer of heat


When happens when cooler air and heated air interact?

The cool air will sink and the warm air will rise.


What will rise and what will sink?

a stone will sink and a feather would rise


Why does happen in the atmosphere?

For the same reason that it happens in other fluids. The hot air (in this case) has a tendency to rise, and colder air, to sink, due to differences in density.


Why does convection happen in the atmosphere?

For the same reason that it happens in other fluids. The hot air (in this case) has a tendency to rise, and colder air, to sink, due to differences in density.


Do molecules rise or sink after they are heated?

Rise


Does heated air rise or sink?

rise


What is the opposite of sink?

The opposite reaction of to sink (in liquid) is to float.However the opposite motion sink (move lower) would have the opposite rise.