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? PowerPoint PPT Presentation


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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.

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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

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

Meridional Radiation Balance and Transfer


How does this balance between insolation and outgoing longwave radiation manifest itself globally

Annual Radiation

90°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

Insolation

Annual Radiation

Insolation

90°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

Insolation

Outgoing

Outgoing

Annual Radiation

Insolation

90°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

Insolation

Surplus

Outgoing

Outgoing

Annual Radiation

Insolation

90°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

Insolation

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

90°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

Insolation = Outgoing

Balance equals zero

Insolation

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

Insolation

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

Insolation

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Maximum Poleward

Energy Transfer

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

90°

~35°

Latitude


How does this balance between insolation and outgoing longwave radiation manifest itself globally

50% Surface Area

50% Surface Area

Insolation

Transfer

Surplus

Outgoing

Outgoing

Annual Radiation

Annual Poleward Transfer

Deficit

Insolation

Poleward Energy

Transfer

90°

~35°

Latitude


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