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2.A lifting actionto causea parcel of air to rise
This change decreases air densitycausinguplift of the air parcels
This difference between ground and high altitude temperaturecreatesan “ uplift of air
Differences in heat and pressure between the surface of the planet and the upper atmospherecreatesan uplift of air
The lay of the landcreatesan uplift of air
Earth 's rotation(passive) caused bya parcel of air
unequal heating of earth 's surface Air flow resulting from heating and cooling of air Amount of precipitation less than .025 cm Increased air temperature over urban regions compared to the surrounding countryside State of the atmosphere at a certain point in time Zonal Wind Flow Wind that has a predominant west to east component(passive) caused bySmall rising parcel of air
Convergencecreatesa focused uplift of air
differences in ( near ) surface temperature(passive) caused initially bya parcel of air Bouyancy
a localized cloud in the beginning stages of a thunderstormcan createa localized cloud in the beginning stages of a thunderstorm
at the surface and being lifted to its level of free convection ( LFCoriginatingat the surface and being lifted to its level of free convection ( LFC
a " hole punch " effect ((passive) caused bya " hole punch " effect (
at the surface and being lifted to the surface 's level of free convection ( LFCoriginatingat the surface and being lifted to the surface 's level of free convection ( LFC
to riseis causedto rise
when a density difference between the environmental air and the parcel existsis createdwhen a density difference between the environmental air and the parcel exists
from between 900 to 800 mbaroriginatingfrom between 900 to 800 mbar
in the stratosphereoriginatingin the stratosphere
the parcel to circle the lowcausingthe parcel to circle the low
it to become satura 21could causeit to become satura 21