Page 179 - Earth's Climate Past and Future
P. 179

CHAPTER 9





                                      Insolation Control



                                      of Ice Sheets








                                      Ice sheets covered northern North America and Europe 20,000 years ago. The
                                      present locations of Toronto, New York, Chicago, Seattle, and London were
                                      buried under hundreds of meters of ice. Later, the ice melted, and the last
                                      remnants disappeared by 6000 years ago, near the time human civilizations
                                      came into existence. The fact that ice sheets first appeared in the northern
                                      hemisphere within the last 3 Myr can be explained by very slow tectonic-scale
                                      cooling (Part II), but the evidence that ice sheets grew and melted over much
                                      shorter intervals of time requires a different explanation.
                                         The driver of these shorter-term variations in the amount of ice is orbitally
                                      driven insolation changes. In this chapter, we investigate how changes in sum-
                                      mer insolation control the size of ice sheets by determining the rate of ice
                                      melting or accumulation. We explore two lags that are important to under-
                                      standing the ice response: the lag of slow-responding ice sheets behind the
                                      insolation changes and the delayed depression of bedrock beneath the weight
                                      of the overlying ice. Both these lags are thousands of years in length. Then we
                                      examine past changes in ice volume based on evidence from oxygen isotopes
                                      and coral reefs. Finally, we analyze how the ice sheet history over the last 3 Myr
                                      compares with predictions from the theory of orbital control of ice volume.
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