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                                                                         VOLCANOES AND CLIMATE   181


                                                                                                  10



                                                     Agung  Hekla  Katmai  Krakatau  Tambora  Laki  Katla  Lanzarote  Pacaya  Komagatake  Unknown  8 6 4

                                                                                                  2
                                                                                                  0
                                                  2000  1950  1900  1850  1800  1750  1700  1650  1600  1550  1500


                                                                                                  10
                                                                       Unknown  Katla  Hekla      8 6  Acidity





                                                                                                  2 4
                                                                                                  0
                                                  1500  1450  1400  1350  1300  1250  1200  1150  1100  1050  1000



                 Fig. 12.1 Occurrences of sudden                                                  10
                 increases (spikes) of acidity in polar-  Eldgja                                  8
                 ice cores marking known eruptions
                 over the past 1500 years. (Adapted by                                            6
                 permission from Macmillan Publishers                                             4
                 Ltd: Nature, Hammer, C.U., Clausen,
                                                                                                  2
                  H.B. and Dansgaard, W., Greenland
                  ice sheet evidence of post-glacial                                              0
                  volcanism and its climatic impact,   1000  950  900  850  800  750  700  650  600  550  AD
                  288, 230–235, copyright (1980).)

                  eruption to affect climate (e.g., Hekla, 1947 and  eruption. The difficulty of proving such a link
                  Katla, 1755).                               comes in part from the limitations of available data
                  • Frost rings are formed in years in which no known  sets, and partly because the effects we are trying to
                  eruption is evident in either the ice-core records or  detect are subtle and often complex, e.g., cooling
                  in historical records. It is unlikely therefore that the  may occur in one region but warming in another.
                  cold conditions which generated these frost rings  Our appreciation of the complexity of the effects
                  were caused by a volcanic eruption.         of volcanic eruptions on climate has developed
                  • Overall the comparison suggests that, in some  tremendously as the result of the new opportu-
                  instances, volcanic eruptions may have been respon-  nities for detailed study offered with the advent of
                  sible for cooling which was severe enough to gen-  satellite monitoring.
                  erate frost rings but that not all eruptions cause
                  cooling and not all frost rings are the result of
                                                              12.3 Satellite monitoring of climate change
                  volcanic activity.
                                                              after volcanic eruptions
                   Though individual studies, such as the one just
                  discussed, are not always conclusive, through a  Until relatively recently our understanding of
                  range of different studies it has become evident that  whether volcanic eruptions affect climate was
                  volcanic eruptions can induce mild climate change,  based on historical records and studies such as
                  usually cooling, for a period of 2–3 years after an  those just described. With the advent of the space
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