Consider a planet where Solar constant = 1360 W /m2 and albedo =0.30. If n=0, what is the equilibrium surface temperature of the planet? If S increases to 1370 W/m2 and n remains zero, what is the new equilibrium surface temperature?
Consider a planet where Solar constant = 1360 W /m2 and albedo =0.30. If n=0, what is the equilibrium surface temperature of the planet? If S increases to 1370 W/m2 and n remains zero, what is the new equilibrium surface temperature?
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Consider a planet where Solar constant = 1360 W /m2 and albedo =0.30.
- If n=0, what is the equilibrium surface temperature of the planet? If S increases to 1370 W/m2 and n remains zero, what is the new equilibrium surface temperature?
- If the planet has a water vapor feedback so that the number of layers n is a function of surface temperature nT = (T – 254.5)/100, what is the equilibrium surface temperature?
- Considering the answers above, calculate the climate feedback factor g for this planet.
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