Using the simplified model of Earths atmosphere as in Example 34.1, with no absorption, no meridional energy

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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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The Physics of Energy

ISBN: 978-1107016651

1st edition

Authors: Robert L. Jaffe, Washington Taylor

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