Page 287 - Earth's Climate Past and Future
P. 287

CHAPTER 14 • Millennial Oscillations of Climate  263


                             Climate                        shielding permitted more bombardment by charged
                    Colder              Warmer                                                          14
                                                            cosmic particles (protons) and faster production of  C
        Younger                                             atoms.
                                                               Shorter-term changes in age offsets are also appar-
                                                            ent within the last 10,000 years (Figure 14–14). These
                   1500               Minor ice rafting     discrepancies may also reflect changes in the rate of
                   years                                    production of   14 C atoms in Earth’s atmosphere,
                                                            although in this case the main cause is thought to be
                                                            changes in emissions from the Sun rather than the over-
                                                            print of Earth’s magnetic shielding. Particles streaming
                                                            from the Sun (called the solar wind) deflect some of the
                                                            incoming cosmic rays (protons) that would otherwise
                                                            enter Earth’s atmosphere (Figure 14–15). Changes in
                                    Major ice rafting event  the amount of solar deflection over hundreds of years
                                       at multiples of                   14
                                         1500 years         could alter the  C production rate in the atmosphere
                                                            and explain the short-term differences in ages derived
                                                            from the two dating methods.
                                                                                14
         Older                                                 The major cycle of  C production in this 10,000-
                                                            year record was centered at 420 years, considerably
                                                            shorter than the millennial time scale explored in this
        FIGURE 14-13 Millennial-scale North Atlantic cycles?  chapter. The only evidence of millennial changes was a
        One view of millennial-scale changes in the North Atlantic is
        that short cooling cycles 1500 years in length gradually drift  weak cycle in the band between 2000 and 2500 years
        toward colder conditions and occasionally culminate in major  (~2100 years), and evidence for a cyclic link between
        ice-rafting episodes, followed by an abrupt return to warmer  solar emissions and climate at this period is faint at best.
        conditions.                                         One reconstruction of the timing of mountain glacier
                                                            advances over the last 7000 years shows some indication
                                                            of a response near 2100 years (see Figure 14–11B), but
                                                            the other reconstruction does not (see Figure 14–11A).
        years), they appear to be random (stochastic) but are
        actually an expression of highly irregular cyclic behavior.  A hint of changes at intervals near 2600 years occurs in
                                                            the sea salt signal in Greenland ice (see Figure 14–9),
                                                            but no such response occurs in the ice-rafting signals in
          IN SUMMARY, the evidence that millennial oscillations  the nearby ocean (see Figure 14–10).
          occur at regular cycles is weak. The oscillations seem  The absence of any obvious cycle of  C production
                                                                                              14
          to be largely the product of random behavior (red  at a period of 1500 years weakens the case for a link
          noise) in the climate system. Several explanations for  between solar forcing and climatic responses such as
          their origin are now under active consideration.  North Atlantic ice rafting and Greenland ice δ O. If
                                                                                                     18
                                                            such a link exists, it would require enormous amplifica-
                                                            tion from within the climate system (perhaps by
        14-6 Solar Variability
                                                            stochastic resonance). Still, the evidence against a cyclic
        One possibility is that millennial-scale oscillations are  link between the Sun and Earth’s climate does not
        caused by changes in the amount of solar radiation  eliminate the possibility that a non-cyclic link exists.
                                                                                                10
        arriving on Earth. No direct record exists of past     Another proposed solar proxy is the  Be isotope,
        changes in the amount of incoming radiation at visible  which is produced by collisions with cosmic particles. As
                                                                       14
        or near-visible (infrared or ultraviolet) wavelengths.  in the case of  C, solar emissions can deflect the cosmic
                                                                                              10
        This part of the spectrum contains most of the energy  particles and modulate production of  Be. Ice core
        that Earth receives from the Sun.                   records show large millennial-scale changes in  Be con-
                                                                                                   10
           Instead, several available proxies provide scientists  centration during the interval from 40,000 to 25,000
                                                                                                       10
        with other measures of possible solar fluctuations. As  years ago, with an obvious correlation between  Be
                                                                         18
        noted in Chapter 13, the difference between the ages  maxima and  δ O minima that indicate oscillations
        derived by counting (matching) tree rings and those  toward cold climates. At first, this correlation seems to
        derived by  C dating of the same rings are one index.  point to a clear solar-climate link, but in fact the varia-
                  14
        The gradually increasing discrepancy between the ages  tions in  Be concentration are an artifact of climatic
                                                                    10
        derived from these two methods (see Box 13–1)       changes. During cold oscillations, ice accumulation rates
        indicates that Earth’s magnetic field was weaker near  dropped. With slower ice accumulation, the concentra-
                                                                  10
        15,000 to 20,000 years ago and that the weaker solar  tion of  Be in the ice would have increased even if its
   282   283   284   285   286   287   288   289   290   291   292