Page 273 - Earth's Climate Past and Future

CHAPTER 13 • Climate During and Since the Last Deglaciation 249

2. To what degree does the timing of ice sheet www.classzone.com/book/earth_science/terc/content/
melting support the Milankovitch theory visualization (Chapter15).
that orbital insolation controls the size of ice
sheets?
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Fairbanks, R. G. 1989. “A 17,000-Year Glacio-eustatic
5. Describe how and why proglacial lakes travel slowly Sea Level Record: Influence of Glacial Melting on
across the landscape behind melting ice sheets. the Younger Dryas Event and Deep-Ocean

6. Why were summer temperatures at high northern Circulation.” Nature 342: 637–42.
latitudes warmer 6000 years ago than they are Teller, J. T. 1987. “Proglacial Lakes and the Southern
today? Would they also have been warmer at high Margin of the Laurentide Ice Sheet.” In North
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in monsoons and northern ice sheets? Geological Society of America.
Webb, T., III. 1998. “Late Quaternary Climates: Data
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Last 18,000 Years: Observations and Model from Pollen Percentages: The Use of Regression
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Roberts, N. 1998. The Holocene. Oxford: Blackwell. Minneapolis: University of Minnesota Press.