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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. - 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
0° 90°Latitude
Annu
al R
adia
tion
Insolation
Insolation
0° 90°Latitude
Annu
al R
adia
tion
Insolation
Insolation
OutgoingOutgoing
0° 90°Latitude
Annu
al R
adia
tion
Insolation
Insolation
OutgoingOutgoing
0° 90°Latitude
Surplus
Annu
al R
adia
tion
Insolation
Insolation
OutgoingOutgoing
0° 90°Latitude
Deficit
Surplus
Annu
al R
adia
tion
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°Latitude
Deficit
Surplus
Annu
al R
adia
tion
Insolation = OutgoingBalance equals zero
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°Latitude
Deficit
Surplus
Annu
al R
adia
tion
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°Latitude
Deficit
Surplus
Annu
al R
adia
tion
What can you see?
Annual differences in Incoming and outgoing radiation at top of the atmosphere.
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
Annu
al R
adia
tion
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Energy Transfer as Freight Train
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Maximum PolewardEnergy Transfer
Insolation
Insolation
OutgoingOutgoing
~35°0° 90°
Transfer
Latitude
Deficit
Surplus
50% Surface Area 50% Surface Area
Annu
al R
adia
tion
Annu
al P
olew
ard
Tran
sfer
Poleward Energy Transfer