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At night, when the air over land cools more quickly than the air over water, it results in a
land breeze.
insolation.
water vapor.
precipitation.
cirrus clouds.
convection cell.
evaporation.
condensation.
The Sun continually turns ocean water into vapor through the process of
land breeze.
insolation.
water vapor.
precipitation.
cirrus clouds.
convection cell.
evaporation.
condensation.
On a humid day, the air is full of
land breeze.
insolation.
water vapor.
precipitation.
cirrus clouds.
convection cell.
evaporation.
condensation.
Water droplets may form on the outside of a glass of water as a result of
land breeze.
insolation.
water vapor.
precipitation.
cirrus clouds.
convection cell.
evaporation.
condensation.
The position of the Sun directly affects the angle of
land breeze.
insolation.
water vapor.
precipitation.
cirrus clouds.
convection cell.
evaporation.
condensation.
On a foggy, rainy day, it would be unlikely for you to see
land breeze.
insolation.
water vapor.
precipitation.
cirrus clouds.
convection cell.
evaporation.
condensation.
Sleet is a form of
land breeze.
insolation.
water vapor.
precipitation.
cirrus clouds.
convection cell.
evaporation.
condensation.
Unequal heating and cooling in the atmosphere can result in a(n)
land breeze.
insolation.
water vapor.
precipitation.
cirrus clouds.
convection cell.
evaporation.
condensation.
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