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regional differences in solar radiationcreateglobal wind belts
This unequal heating also sets the air in motioncreatingglobal wind belts
Air moving at the bases of the three major convection cells in each hemisphere north and south of the equatorcreatesthe global wind belts
The air movement of each large circulation cellcreatesthe major wind belts
Air moving between large high and low pressure systems at the bases of the three major convection cellscreatesthe global wind belts
due to global long term pressure systems(passive) are createdThe global wind belts
Wind energy along with the uneven heating of the earth ’s surfacecreatesglobal wind belts
Air blowing at the base of the circulation cells , from high pressure to low pressurecreatesthe global wind belts
when the earth receives an unequal amount of heat from sunlight and the spinning of the earth(passive) are createdGlobal wind belts
Surface currents(passive) are caused bySurface currents
the surface ocean currents(passive) set bythe surface ocean currents
the wet and dry seasons in this area ( Figure 17.4 ) pdfcausesthe wet and dry seasons in this area ( Figure 17.4 ) pdf
the wet and dry seasons in this area At about 30 degrees N and 30 degrees Scausesthe wet and dry seasons in this area At about 30 degrees N and 30 degrees S
global patterns of air flowcreateglobal patterns of air flow
wind belts Subtropical high - pressure zones Areas of dry , bright sunshineresultingwind belts Subtropical high - pressure zones Areas of dry , bright sunshine
from this balance of energy at the Earth ’s surfaceresultfrom this balance of energy at the Earth ’s surface
from the tendency of air to flow from high to low pressureresultfrom the tendency of air to flow from high to low pressure