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Air heating and rising over the land and circulating back in from the ocean is an example of a
Convection
True
Visible light
True
Conduction
True
Coriolis Effect
Sea Breeze
Heat transfer through fluids (air or water) is called
Convection
True
Visible light
True
Conduction
True
Coriolis Effect
Sea Breeze
Cold air is more dense than warm air
Convection
True
Visible light
True
Conduction
True
Coriolis Effect
Sea Breeze
ROY G BIV represents all the colors of
Convection
True
Visible light
True
Conduction
True
Coriolis Effect
Sea Breeze
Warm air is less dense and causes air pressure to decrease
Convection
True
Visible light
True
Conduction
True
Coriolis Effect
Sea Breeze
There is low pressure at the equator because it is warm
Convection
True
Visible light
True
Conduction
True
Coriolis Effect
Sea Breeze
A spoon heating on a hot stove demonstrates
Convection
True
Visible light
True
Conduction
True
Coriolis Effect
Sea Breeze
The deflection or cuving of global winds due to the Earth's rotation is called
Convection
True
Visible light
True
Conduction
True
Coriolis Effect
Sea Breeze
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