HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

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HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

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HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

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HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Meridional Radiation Balance and Transfer

Annual Radiation

0°

90°

Latitude

Insolation

Annual Radiation

Insolation

0°

90°

Latitude

Insolation

Outgoing

Outgoing

Annual Radiation

Insolation

0°

90°

Latitude

Insolation

Surplus

Outgoing

Outgoing

Annual Radiation

Insolation

0°

90°

Latitude

Insolation

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

0°

90°

Latitude

Insolation = Outgoing

Balance equals zero

Insolation

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

0°

90°

~35°

Latitude

Insolation

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

0°

90°

~35°

Latitude

Insolation

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

0°

90°

~35°

Latitude

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Maximum Poleward

Energy Transfer

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

0°

90°

~35°

Latitude

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

Poleward Energy

Transfer

0°

90°

~35°

Latitude