Page 292 - Earth's Climate Past and Future
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268     PART IV • Deglacial Climate Changes


        a range of indicators suggests that millennial oscilla-  Key Terms
        tions in the northern hemisphere were much larger in
        winter than in summer. This pattern is consistent with  millennial oscillations   red noise (p. 262)
        propagation of the millennial oscillation during the  (p. 251)               stochastic resonance
        strong atmospheric flow of winter.                  Dansgaard-Oeschger        (p. 262)
                                                              oscillations (p. 253)  bedrock pinning points
          IN SUMMARY, the origin of millennial climatic     sediment drifts (p. 253)  (p. 265)
          oscillations remains unknown, but considerable    Heinrich events (p. 253)  bipolar seesaw (p. 267)
          progress has been made in defining their time-and-
          space “footprint” in the climate system. The
          oscillations appear to be largely random rather than
          cyclic. Their amplitude is largest when ice sheets are  Review Questions
          present on North America and Eurasia, and the
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          largest oscillations are centered near Greenland and  1. How do the processes that control δ O changes
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          the North Atlantic Ocean. Similar (but smaller)       in ice sheets differ from those that control δ O
          changes with nearly opposite timing occur over        fluctuations in ocean cores?
          Antarctica and in other regions in the southern
          hemisphere, including the southeastern Pacific     2. Why is it difficult to correlate millennial climatic
          Ocean off the coast of Chile. The bipolar seesaw      oscillations in records from different regions?
          is a promising candidate for an internal oscillation  3. What other regions show millennial oscillations
          of natural origin.                                    like those in the North Atlantic and Greenland?
                                                             4. Are millennial oscillations true cycles?
        14-10 Implications for Future Climate                5. How strong is the evidence that solar changes
                                                                drive millennial oscillations?
        Because millennial oscillations occur much faster than
        orbital-scale changes, they have the potential to have a  6. What is the evidence for and against internal ice
        more immediate impact on our climatic future. Scientists  sheet processes causing millennial oscillations?
        and policy planners would like to know whether natural  7. How could ocean flow cause opposite millennial
        oscillations could cause climate to warm or to cool in  oscillations north and south of the equator?
        future decades. Some scientists have speculated that a
        natural millennial-scale warming could be underway
        now. If this view is correct, it means that the observed
        warming of the last century or so could in part be the
        result of natural processes rather than human activities.  Additional Resources
           This claim is unjustifiable for several reasons.
        Because millennial oscillations are either completely  Basic Reading
        random (red noise) or at best quasi-periodic, their pre-  Alley, R. B. 2000. The Two-Mile Time Machine.
        sent and future course cannot be predicted with any   Princeton, NJ: Princeton University Press.
        confidence. More critically, the largest oscillations
        occurred only during glacial climates, whereas the  Advanced Reading
        changes during the past 8000 years of warm interglacial  Beer, J., et al. 1988. “Information on Past Solar
                                                                                           10
        climate have been small and local in scale. This observa-  Activity and Geomagnetism from  Be in the
        tion argues against natural oscillations playing a major  Camp Century Ice Core.” Nature 331: 675–79.
        role in present and future climate change.          Bond, G., W. S. Broecker, S. J. Johnsen, J. McManus,
           Of course, the Greenland and Antarctic ice sheets  L. D. Labeyrie, J. Jouzel, and G. Bonani. 1993.
        are still in place, and they remain susceptible to some  “Correlations Between Climatic Records from
        degree of melting in the warmer climate of the future.  North Atlantic Sediments and Greenland Ice.”
        Because ice sheets appear to have played a role in at  Nature 365:143–47.
        least some of the glacial-age millennial oscillations, par-  Boyle, E. A. 2000. “Is Ocean Thermohaline
        tial melting of today’s ice sheets because of human activ-  Circulation Linked to Abrupt Stadial-Interstadial
        ities could conceivably trigger changes in the climate  Transitions?” Quaternary Science Reviews 19:
        system in the future, even if at a smaller scale. In this  255–72.
        case, however, the cause of these changes will be human  Brook, E. J., et al. 2005. “Timing of Millennial-Scale
        activities, not natural variations in the climate system.  Climate Change at Siple Dome, West Antarctica,
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