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As air moves it becomes

this question is about science ( Circulating air ) .

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Aija Sawyer

Lvl 2
5y ago
Updated: 2/27/2020

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Aija Sawyer

Lvl 2
5y ago

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Related Questions

When air moves away from the tropics and toward the poles it becomes .?

cool and dry


When air moves slowly it takes on the temperature and humidity of its region becomes an?

Stagnant.


When the air moves away from the tropics and towards the poles it becomes?

cool and dry


How does air become wind?

Air becomes a wind when it moves from one place to another. The movement is driven by the heat from the Sun.


When water from the earth's surface moves into the air what does it become?

* It stays water, it leeches through the ground or evaporates always staying as water.


Why does convection in air occur?

Convection in air occurs because as air is heated, it becomes less dense and rises, while cooler, denser air sinks. This creates a cycle of circulation where warmer air moves upwards and cooler air moves downwards, transferring heat in the process.


What happens to a maritime Pacific air mass over the North Pacific as it moves inland over the Pacific ocean?

It mixes with continental air and gradually becomes a continental air mass


What is it called when warm air moves up?

convetion currents


You get wind because?

We get wind because:Some places are warmer than othersThe warm air heats up becomes light and risesThe cool air moves in to replace it


How does the air around us moves?

how does the air around us moves?


Which air mass often originates as a different air mass in Siberia and is subsequently altered?

The Siberian air mass often originates as a continental polar air mass. As it moves over the Siberian landmass, it becomes extremely cold and dry due to frigid temperatures. This Siberian air mass can then be altered by interactions with other air masses as it moves, shaping weather conditions in different regions.


As the atmosphere heats the air it becomes?

less dense and rises, creating areas of low pressure. This leads to the formation of convection currents as the warm air expands and moves upwards.