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The process when air lifts into the atmosphere after multiple horizontal air currents contact one another is called
convection
temperature rising
rain shadow
When mountains cause humidity and weather to differ on either side
a group of thunderstorms along a cold front
supercells
sun heating the earth and the air above the ground warming as a result
source region
Characteristics of a cold front passing through an area include:
convection
temperature rising
rain shadow
When mountains cause humidity and weather to differ on either side
a group of thunderstorms along a cold front
supercells
sun heating the earth and the air above the ground warming as a result
source region
What is orographic lifting?
convection
temperature rising
rain shadow
When mountains cause humidity and weather to differ on either side
a group of thunderstorms along a cold front
supercells
sun heating the earth and the air above the ground warming as a result
source region
Large rotating storm systems are known as
convection
temperature rising
rain shadow
When mountains cause humidity and weather to differ on either side
a group of thunderstorms along a cold front
supercells
sun heating the earth and the air above the ground warming as a result
source region
Convection works by:
convection
temperature rising
rain shadow
When mountains cause humidity and weather to differ on either side
a group of thunderstorms along a cold front
supercells
sun heating the earth and the air above the ground warming as a result
source region
What is a squall line?
convection
temperature rising
rain shadow
When mountains cause humidity and weather to differ on either side
a group of thunderstorms along a cold front
supercells
sun heating the earth and the air above the ground warming as a result
source region
The area that gives an air mass its characteristics is called a
convection
temperature rising
rain shadow
When mountains cause humidity and weather to differ on either side
a group of thunderstorms along a cold front
supercells
sun heating the earth and the air above the ground warming as a result
source region
The effect where a windy side of a mountain is different (drier)than the non-windy side is called the
convection
temperature rising
rain shadow
When mountains cause humidity and weather to differ on either side
a group of thunderstorms along a cold front
supercells
sun heating the earth and the air above the ground warming as a result
source region
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