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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. 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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  1. HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY? Meridional Radiation Balance and Transfer

  2. Annual Radiation 0° 90° Latitude

  3. Insolation Annual Radiation Insolation 0° 90° Latitude

  4. Insolation Outgoing Outgoing Annual Radiation Insolation 0° 90° Latitude

  5. Insolation Surplus Outgoing Outgoing Annual Radiation Insolation 0° 90° Latitude

  6. Insolation Surplus Outgoing Outgoing Annual Radiation Deficit Insolation 0° 90° Latitude

  7. Insolation = Outgoing Balance equals zero Insolation Surplus Outgoing Outgoing Annual Radiation Deficit Insolation 0° 90° ~35° Latitude

  8. Insolation Surplus Outgoing Outgoing Annual Radiation Deficit Insolation 0° 90° ~35° Latitude

  9. Insolation Surplus Outgoing Outgoing Annual Radiation Deficit Insolation 0° 90° ~35° Latitude

  10. Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Deficit Insolation 0° 90° ~35° Latitude

  11. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Deficit Insolation 0° 90° ~35° Latitude

  12. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  13. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  14. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  15. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  16. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  17. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  18. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  19. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  20. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  21. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  22. 50% Surface Area 50% Surface Area Insolation Transfer Surplus Outgoing Outgoing Annual Radiation Annual Poleward Transfer Deficit Insolation 0° 90° ~35° Latitude

  23. 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

  24. 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

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