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The radiative forcing due to a doubling of CO alone is 3.70 (w/m^2) Due the planetary albedo was about 1% higher at the LGM than the present. Solar output was the same between the two periods. LGM was 5 C colder Compare to the value of the climate sensitivity in the absence of climate feedbacks and estimates the differences in Ts and F between the current climate and the climate at the time of the (LGM).

The radiative forcing due to a doubling of CO alone is 3.70 (w/m^2) Due the planetary albedo was about 1% higher at the LGM than the present. Solar output was the same between the two periods. LGM was 5 C colder Compare to the value of the climate sensitivity in the absence of climate feedbacks and estimates the differences in Ts and F between the current climate and the climate at the time of the (LGM).

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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The radiative forcing due to a doubling of CO alone is 3.70 (w/m^2) Due the planetary albedo was about 1% higher at the LGM than the present. Solar output was the same between the two periods. LGM was 5 C colder Compare to the value of the climate sensitivity in the absence of climate feedbacks and estimates the differences in Ts and F between the current climate and the climate at the time of the (LGM) .
Transcribed Image Text:The radiative forcing due to a doubling of CO alone is 3.70 (w/m^2) Due the planetary albedo was about 1% higher at the LGM than the present. Solar output was the same between the two periods. LGM was 5 C colder Compare to the value of the climate sensitivity in the absence of climate feedbacks and estimates the differences in Ts and F between the current climate and the climate at the time of the (LGM) .
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