Question: Using the simplified model of Earths atmosphere as in Example 34.1, with no absorption, no meridional energy transport, and an albedo of 0.16, use the

Using the simplified model of Earth’s atmosphere as in Example 34.1, with no absorption, no meridional energy transport, and an albedo of 0.16, use the yearly average integrated insolation computed in §23.3 to compute the temperature in radiative equilibrium on the equator and at the poles.

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From Figure 236 the hours of perpendicular sunshine average about 73 hd at the equator and about ... View full answer

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