In: Other
Match the general circulation component with the correct description.
Group of answer choices
ITCZ
[ Choose ] between the ITCZ and about 30 degrees north and south; surface winds that flow towards the equator zones at about 30 degrees north and south where cool air from altitude descends creating high pressure where the westerlies and polar easterlies converge; mild rising of air masses produces low pressure descendiung air over the poles that produces persistent high pressure surface wind traveling from pole towards equator Intertropical convergence zone at about 5 degrees north where warm air rises surface winds traveling poleward from about 30 to 60 degrees
Trade winds
[ Choose ] between the ITCZ and about 30 degrees north and south; surface winds that flow towards the equator zones at about 30 degrees north and south where cool air from altitude descends creating high pressure where the westerlies and polar easterlies converge; mild rising of air masses produces low pressure descendiung air over the poles that produces persistent high pressure surface wind traveling from pole towards equator Intertropical convergence zone at about 5 degrees north where warm air rises surface winds traveling poleward from about 30 to 60 degrees
Subtropical highs
[ Choose ] between the ITCZ and about 30 degrees north and south; surface winds that flow towards the equator zones at about 30 degrees north and south where cool air from altitude descends creating high pressure where the westerlies and polar easterlies converge; mild rising of air masses produces low pressure descendiung air over the poles that produces persistent high pressure surface wind traveling from pole towards equator Intertropical convergence zone at about 5 degrees north where warm air rises surface winds traveling poleward from about 30 to 60 degrees
Westerlies
[ Choose ] between the ITCZ and about 30 degrees north and south; surface winds that flow towards the equator zones at about 30 degrees north and south where cool air from altitude descends creating high pressure where the westerlies and polar easterlies converge; mild rising of air masses produces low pressure descendiung air over the poles that produces persistent high pressure surface wind traveling from pole towards equator Intertropical convergence zone at about 5 degrees north where warm air rises surface winds traveling poleward from about 30 to 60 degrees
Polar fronts
[ Choose ] between the ITCZ and about 30 degrees north and south; surface winds that flow towards the equator zones at about 30 degrees north and south where cool air from altitude descends creating high pressure where the westerlies and polar easterlies converge; mild rising of air masses produces low pressure descendiung air over the poles that produces persistent high pressure surface wind traveling from pole towards equator Intertropical convergence zone at about 5 degrees north where warm air rises surface winds traveling poleward from about 30 to 60 degrees
Polar easterlies
[ Choose ] between the ITCZ and about 30 degrees north and south; surface winds that flow towards the equator zones at about 30 degrees north and south where cool air from altitude descends creating high pressure where the westerlies and polar easterlies converge; mild rising of air masses produces low pressure descendiung air over the poles that produces persistent high pressure surface wind traveling from pole towards equator Intertropical convergence zone at about 5 degrees north where warm air rises surface winds traveling poleward from about 30 to 60 degrees
Polar highs
[ Choose ] between the ITCZ and about 30 degrees north and south; surface winds that flow towards the equator zones at about 30 degrees north and south where cool air from altitude descends creating high pressure where the westerlies and polar easterlies converge; mild rising of air masses produces low pressure descendiung air over the poles that produces persistent high pressure surface wind traveling from pole towards equator Intertropical convergence zone at about 5 degrees north where warm air rises surface winds traveling poleward from about 30 to 60 degrees
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TRADE WINDS between ITCZ and about 30 degrees north and south; surface winds that flow towards the equator ITCZ zones at about 30 degrees north and south where cool air from altitude descends creating high pressure POLAR FRONTS where the westerlies and polar easterlies converge; mild rising of air masses produces low pressure POLAR HIGHS descendiung air over the poles that produces persistent high pressure POLAR EASTERLIES surface wind traveling from pole towards equator SUBTROPICAL HIGHS Intertropical convergence zone at about 5 degrees north where warm air rises WESTERLIES surface winds traveling poleward from about 30 to 60 degrees.
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