Skip to main content Accessibility help
×
Hostname: page-component-cd9895bd7-dk4vv Total loading time: 0 Render date: 2024-12-12T21:49:20.603Z Has data issue: false hasContentIssue false
This chapter is part of a book that is no longer available to purchase from Cambridge Core

8 - Climate change

from Part II - Global Physical Climatology

Gordon B. Bonan
Affiliation:
National Center for Atmospheric Research, Boulder, Colorado
Get access

Summary

Chapter summary

Climate has changed over the course of Earth's history and will change in the future. Just 18 000 years ago, Earth was in the grips of a prolonged cold period in which vast tracts of the Northern Hemisphere were covered with ice. Over the past two million years there have been numerous such ice ages separated by shorter, warm interglacial periods. Our current climate is that of a warm interglacial and history suggests that over the next several thousand years prolonged cooling culminating in another ice age is possible in the absence of human influences. The geologic record also reveals numerous rapid climate changes over periods as short as decades or centuries. Climate change is the result of changes in the external forcing of the climate system by the Sun and internal physical, chemical, and biological feedbacks among the atmospheric, oceanic, and terrestrial components of the climate system. Plate tectonics and changes in the geometry of Earth's orbit around the Sun influence climate at timescales of millennia or longer. Changes in the concentration of greenhouse gases or in the runoff of freshwater to oceans affect climate at timescales of centuries to millennia. Changes in solar irradiance or volcanic eruptions that emit aerosols into the atmosphere influence climate at timescales of years to decades. Climate change over the twentieth century is reviewed in the context of greenhouse gases and anthropogenic influences on climate.

Type
Chapter
Information
Ecological Climatology
Concepts and Applications
, pp. 105 - 128
Publisher: Cambridge University Press
Print publication year: 2008

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Adams, J. B., Mann, M. E., and Ammann, C. M., 2003. Proxy evidence for an El Niño-like response to volcanic forcing. Nature, 426, 274–8.CrossRefGoogle Scholar
Alley, R. B., 2000. Ice-core evidence of abrupt climate changes. Proceedings of the National Academy of Sciences, USA, 97, 1331–4.CrossRefGoogle ScholarPubMed
Alley, R. B. and Ágústsdóttir, A. M., 2005. The 8k event: cause and consequences of a major Holocene abrupt climate change. Quaternary Science Reviews, 24, 1123–49.CrossRefGoogle Scholar
Alley, R. B. and Clark, P. U., 1999. The deglaciation of the Northern Hemisphere: a global perspective. Annual Review of Earth and Planetary Sciences, 27, 149–82.CrossRefGoogle Scholar
Alley, R. B., Marotzke, J., Nordhaus, W., et al., 2002. Abrupt Climate Change: Inevitable Surprises. The National Academies Press, 238 pp.Google Scholar
Alley, R. B., Marotzke, J., Nordhaus, W. D., et al., 2003. Abrupt climate change. Science, 299, 2005–10.CrossRefGoogle ScholarPubMed
Ammann, C. M., Joos, F., Schimel, D. S., Otto-Bliesner, B. L., and Tomas, R. A., 2007. Solar influence on climate during the past millennium: results from transient simulations with the NCAR Climate System Model. Proceedings of the National Academy of Sciences, USA, 104, 3713–18.CrossRefGoogle ScholarPubMed
Andres, R. J., Marland, G., Fung, I., and Matthews, E., 1996. A one degree by one degree distribution of carbon dioxide emissions from fossil fuel consumption and cement manufacture, 1950–1990. Global Biogeochemical Cycles, 10, 419–29.CrossRefGoogle Scholar
Andres, R. J., Fielding, D. J., Marland, G., et al., 1999. Carbon dioxide emissions from fossil-fuel use, 1751–1950. Tellus, 51B, 759–65.CrossRefGoogle Scholar
Barber, D. C., Dyke, A., Hillaire-Marcel, C., et al., 1999. Forcing of the cold event of 8,200 years ago by catastrophic drainage of Laurentide lakes. Nature, 400, 344–8.CrossRefGoogle Scholar
Barnola, J. M., Raynaud, D., Korotkevich, Y. S., and Lorius, C., 1987. Vostok ice core provides 160,000-year record of atmospheric CO2. Nature, 329, 408–14.CrossRefGoogle Scholar
Barron, E. J. and Peterson, W. H., 1989. Model simulation of the Cretaceous ocean circulation. Science, 244, 684–6.CrossRefGoogle ScholarPubMed
Beerling, D. J. and Berner, R. A., 2005. Feedbacks and the coevolution of plants and atmospheric CO2. Proceedings of the National Academy of Sciences, USA, 102, 1302–5.CrossRefGoogle ScholarPubMed
Berger, A. L., 1978. Long-term variations of daily insolation and Quaternary climatic changes. Journal of the Atmospheric Sciences, 35, 2362–7.2.0.CO;2>CrossRefGoogle Scholar
Berger, A. L., 1988. Milankovitch theory and climate. Reviews of Geophysics, 26, 624–57.CrossRefGoogle Scholar
Berger, A. L. and Loutre, M. F., 1991. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews, 10, 297–317.CrossRefGoogle Scholar
Berger, A. L., Loutre, M. F., and Tricot, C., 1993. Insolation and Earth's orbital periods. Journal of Geophysical Research, 98D, 10 341–62.CrossRefGoogle Scholar
Berner, R. A., 1991. A model for atmospheric CO2 over Phanerozoic time. American Journal of Science, 291, 339–76.CrossRefGoogle Scholar
Berner, R. A., 1998. The carbon cycle and CO2 over Phanerozoic time: the role of land plants. Philosophical Transactions of the Royal Society of London, 353B, 75–82.CrossRefGoogle Scholar
Berner, R. A., 2003. The long-term carbon cycle, fossil fuels and atmospheric composition. Nature, 426, 323–6.CrossRefGoogle ScholarPubMed
Berner, R. A. and Lasaga, A. C., 1989. Modeling the geochemical carbon cycle. Scientific American, 260(3), 74–81.CrossRefGoogle Scholar
Bindoff, N. L., Willebrand, J., Artale, V., et al., 2007. Observations: oceanic climate change and sea level. In Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M., et al. Cambridge University Press, pp. 385–432.Google Scholar
Bradley, R. S. and Jones, P. D. (eds.), 1992. Climate since A.D. 1500. Routledge, 679 pp.Google Scholar
Brady, E. C., DeConto, R. M., and Thompson, S. L., 1998. Deep water formation and poleward ocean heat transport in the warm climate extreme of the Cretaceous (80 Ma). Geophysical Research Letters, 25, 4205–8.CrossRefGoogle Scholar
Briffa, K. R., Jones, P. D., Schweingruber, F. H., and Osborn, T. J., 1998. Influence of volcanic eruptions on Northern Hemisphere summer temperature over the past 600 years. Nature, 393, 450–5.CrossRefGoogle Scholar
Broecker, W. S., 1997. Thermohaline circulation, the Achilles heel of our climate system: will man-made CO2 upset the current balance?Science, 278, 1582–8.CrossRefGoogle ScholarPubMed
Broecker, W. S., 2000. Was a change in thermohaline circulation responsible for the Little Ice Age?Proceedings of the National Academy of Sciences, USA, 97, 1339–42.CrossRefGoogle ScholarPubMed
Broecker, W. S., 2003. Does the trigger for abrupt climate change reside in the ocean or in the atmosphere?Science, 300, 1519–22.CrossRefGoogle ScholarPubMed
Broecker, W. S., 2006. Abrupt climate change revisited. Global and Planetary Change, 54, 211–15.CrossRefGoogle Scholar
Broecker, W. S., Peteet, D. M., and Rind, D., 1985. Does the ocean–atmosphere system have more than one stable mode of operation?Nature, 315, 21–6.CrossRefGoogle Scholar
Broecker, W. S., Kennett, J. P., Flower, B. P., et al., 1989. Routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode. Nature, 341, 318–21.CrossRefGoogle Scholar
Brohan, P., Kennedy, J. J., Harris, I., Tett, S. F. B., and Jones, P. D., 2006. Uncertainty estimates in regional and global observed temperature changes: a new data set from 1850. Journal of Geophysical Research, 111D, D12106, doi:10.1029/2005JD006548.Google Scholar
Burroughs, W. J., 1997. Does the Weather Really Matter? The Social Implications of Climate Change. Cambridge University Press, 230 pp.CrossRefGoogle Scholar
Cane, M. A. and Molnar, P., 2001. Closing of the Indonesian seaway as a precursor to east African aridification around 3–4 million years ago. Nature, 411, 157–62.CrossRefGoogle ScholarPubMed
Chappellaz, J., Barnola, J. M., Raynaud, D., Korotkevich, Y. S., and Lorius, C., 1990. Ice-core record of atmospheric methane over the past 160,000 years. Nature, 345, 127–31.CrossRefGoogle Scholar
Charlson, R. J., Lovelock, J. E., Andreae, M. O., and Warren, S. G., 1987. Oceanic phytoplankton, atmospheric sulfur, cloud albedo and climate. Nature, 326, 655–61.CrossRefGoogle Scholar
Clark, P. U., Marshall, S. J., Clarke, G. K. C., et al., 2001. Freshwater forcing of abrupt climate change during the last glaciation. Science, 293, 283–7.CrossRefGoogle ScholarPubMed
Clark, P. U., Pisias, N. G., Stocker, T. F., and Weaver, A. J., 2002. The role of the thermohaline circulation in abrupt climate change. Nature, 415, 863–9.CrossRefGoogle ScholarPubMed
Clarke, G. K. C., Leverington, D. W., Teller, J. T., and Dyke, A. S., 2004. Paleohydraulics of the last outburst flood from glacial Lake Agassiz and the 8200 BP cold event. Quaternary Science Reviews, 23, 389–407.CrossRefGoogle Scholar
,COHMAP, 1988. Climatic changes of the last 18,000 years: observations and model simulations. Science, 241, 1043–52.CrossRefGoogle Scholar
Crowley, T. J. and North, G. R., 1991. Paleoclimatology. Oxford University Press, 339 pp.Google Scholar
DeConto, R. M. and Pollard, D., 2003. Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2. Nature, 421, 245–9.CrossRefGoogle ScholarPubMed
Denman, K. L., Brasseur, G., Chidthaisong, A., et al., 2007. Couplings between changes in the climate system and biogeochemistry. In Climate Change 2007: the Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M., et al. Cambridge University Press, pp. 499–587.Google Scholar
Driscoll, N. W. and Haug, G. H., 1998. A short circuit in thermohaline circulation: a cause for Northern Hemisphere glaciation?Science, 282, 436–8.CrossRefGoogle Scholar
Eddy, J. A., 1976. The Maunder Minimum. Science, 192, 1189–202.CrossRefGoogle ScholarPubMed
,EPICA, 2004. Eight glacial cycles from an Antarctic ice core. Nature, 429, 623–8.CrossRefGoogle Scholar
Fiocco, G., Fuà, D., and Visconti, G. (eds.), 1996. The Mount Pinatubo Eruption: Effects on the Atmosphere and Climate. Springer-Verlag, 310 pp.CrossRefGoogle Scholar
Forster, P., Ramaswamy, V., Artaxo, P., et al., 2007. Changes in atmospheric constituents and in radiative forcing. Climate Change 2007: the Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M., et al. Cambridge University Press, pp. 129–234.Google Scholar
Foukal, P., Fröhlich, C., Spruit, H., and Wigley, T. M. L., 2006. Variations in solar luminosity and their effect on the Earth's climate. Science, 443, 161–6.Google ScholarPubMed
Free, M. and Robock, A., 1999. Global warming in the context of the Little Ice Age. Journal of Geophysical Research, 104D, 19 057–70.CrossRefGoogle Scholar
Hansen, J. and Sato, M., 2004. Greenhouse gas growth rates. Proceedings of the National Academy of Sciences, USA, 101, 16 109–14.CrossRefGoogle ScholarPubMed
Hansen, J., Lacis, A., Ruedy, R., and Sato, M., 1992. Potential climate impact of Mount Pinatubo eruption. Geophysical Research Letters, 19, 215–18.CrossRefGoogle Scholar
Hansen, J., Sato, M., Ruedy, R., et al., 1996. A Pinatubo climate modeling investigation. In The Mount Pinatubo Eruption: Effects on the Atmosphere and Climate, ed. Fiocco, G., Fuà, D., and Visconti, G.. Springer-Verlag, pp. 233–72.CrossRefGoogle Scholar
Hansen, J. E., Sato, M., Lacis, A., et al., 1998. Climate forcings in the Industrial era. Proceedings of the National Academy of Sciences, USA, 95, 12 753–8.CrossRefGoogle ScholarPubMed
Hansen, J., Nazarenko, L., Ruedy, R., et al., 2005. Earth's energy imbalance: confirmation and implications. Science, 308, 1431–5.CrossRefGoogle ScholarPubMed
Hansen, J., Sato, M., Ruedy, R., et al., 2006. Global temperature change. Proceedings of the National Academy of Sciences, USA, 103, 14 288–93.CrossRefGoogle ScholarPubMed
Haug, G. H. and Tiedemann, R., 1998. Effect of the formation of the Isthmus of Panama on Atlantic Ocean thermohaline circulation. Nature, 393, 673–6.CrossRefGoogle Scholar
Hay, W. W., DeConto, R. M., Wold, C. N., et al., 1999. Alternative global Cretaceous paleogeography. In Evolution of the Cretaceous Ocean–Climate System, ed. Barrera, E. and Johnson, C. C.. Geological Society of America, pp. 1–47.Google Scholar
Hays, J. D., Imbrie, J., and Shackleton, N. J., 1976. Variations in the Earth's orbit: pacemaker of the Ice Ages. Science, 194, 1121–32.CrossRefGoogle ScholarPubMed
Hegerl, G. C., Zwiers, F. W., Braconnot, P., et al., 2007. Understanding and attributing climate change. Climate Change 2007: the Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M., et al., Cambridge University Press, pp. 663–745.Google Scholar
Hoyt, D. V. and Schatten, K. H., 1993. A discussion of plausible solar irradiance variations, 1700–1992. Journal of Geophysical Research, 98A, 18 895–906.CrossRefGoogle Scholar
Hughes, P., 1976. American Weather Stories. U.S. Department of Commerce, National Ocean and Atmospheric Administration, 116 pp.Google Scholar
Huntley, B. J. and Webb, III T. (eds.), 1988. Vegetation History. Kluwer Academic Publishers, 803 pp.CrossRefGoogle Scholar
Jansen, E., Overpeck, J., Briffa, K. R., et al., 2007. Palaeoclimate. Climate Change 2007: the Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M., et al., Cambridge University Press, pp. 433–97.Google Scholar
Jones, P. D. and Kelly, P. M., 1996. The effect of tropical explosive volcanic eruptions on surface air temperature. In The Mount Pinatubo Eruption: Effects on the Atmosphere and Climate, ed. Fiocco, G., Fuà, D., and Visconti, G.. Springer-Verlag, pp. 95–111.CrossRefGoogle Scholar
Jones, P. D. and Mann, M. E., 2004. Climate over past millennia. Reviews of Geophysics, 42, RG2002, doi:10.1029/2003RG000143.CrossRefGoogle Scholar
Jones, P. D., Briffa, K. R., Barnett, T. P., and Tett, S. F. B., 1998. High-resolution palaeoclimatic records for the last millennium: Interpretation, integration and comparison with general circulation model control-run temperatures. The Holocene, 8, 455–71.CrossRefGoogle Scholar
Jouzel, J., Barkov, N. I., Barnola, J. M., et al., 1993. Extending the Vostok ice-core record of palaeoclimate to the penultimate glacial period. Nature, 364, 407–12.CrossRefGoogle Scholar
Jouzel, J., Waelbroeck, C., Malaize, B., et al., 1996. Climatic interpretation of the recently extended Vostok ice records. Climate Dynamics, 12, 513–21.CrossRefGoogle Scholar
Keigwin, L. D. and Boyle, E. A., 2000. Detecting Holocene changes in thermohaline circulation. Proceedings of the National Academy of Sciences, USA, 97, 1343–6.CrossRefGoogle ScholarPubMed
Kennett, J. P., 1977. Cenozoic evolution of Antarctic glaciation, the circum-Antarctic ocean, and their impact on global paleoceanography. Journal of Geophysical Research, 82, 3843–60.CrossRefGoogle Scholar
Kirchner, I., Stenchikov, G. L., Graf, H.-F., Robock, A., and Antuña, J. C., 1999. Climate model simulation of winter warming and summer cooling following the 1991 Mount Pinatubo volcanic eruption. Journal of Geophysical Research, 104D, 19 039–55.CrossRefGoogle Scholar
Knutson, T. R., Delworth, T. L., Dixon, K. W., et al., 2006. Assessment of twentieth-century regional surface temperature trends using the GFDL CM2 coupled models. Journal of Climate, 19, 1624–51.CrossRefGoogle Scholar
Knutti, R., Flückiger, J., Stocker, T. F., and Timmermann, A., 2004. Strong hemispheric coupling of glacial climate through freshwater discharge and ocean circulation. Nature, 430, 851–6.CrossRefGoogle ScholarPubMed
Kump, L. R., Kasting, J. F., and Crane, R. G., 1999. The Earth System. Prentice-Hall, 351 pp.Google Scholar
Kutzbach, J. E. and Guetter, P. J., 1986. The influence of changing orbital parameters and surface boundary conditions on climate simulations for the past 18 000 years. Journal of the Atmospheric Sciences, 43, 1726–59.2.0.CO;2>CrossRefGoogle Scholar
Kutzbach, J. E. and Webb, III T., 1993. Conceptual basis for understanding late-Quaternary climates. In Global Climates since the Last Glacial Maximum, ed. Wright, Jr. H. E., Kutzbach, J. E., Webb, III T., et al. University of Minnesota Press, pp. 5–11.Google Scholar
Kutzbach, J. E., Guetter, P. J., Ruddiman, W. F., and Prell, W. L., 1989. Sensitivity of climate to late Cenozoic uplift in southern Asia and the American west: numerical experiments. Journal of Geophysical Research, 94D, 18 393–407.CrossRefGoogle Scholar
Lamb, H. H., 1995. Climate, History and the Modern World, 2nd edn. Routledge, 433 pp.Google Scholar
Lean, J., Beer, J., and Bradley, R., 1995. Reconstruction of solar irradiance since 1610: implications for climate change. Geophysical Research Letters, 22, 3195–8.CrossRefGoogle Scholar
Lean, J. L., Wang, Y.-M., and Sheeley, Jr. N. R., 2002. The effect of increasing solar activity on the Sun's total and open magnetic flux during multiple cycles: implications for solar forcing of climate. Geophysical Research Letters, 29, 2224, doi:10.1029/2002GL015880.CrossRefGoogle Scholar
Lemke, P., Ren, J., Alley, R. B., et al., 2007. Observations: Changes in snow, ice and frozen ground. Climate Change 2007: the Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M., et al. Cambridge University Press, pp. 337–83.Google Scholar
Manabe, S. and Stouffer, R. J., 1999. The role of thermohaline circulation in climate. Tellus, 51A–B, 91–109.Google Scholar
Mann, M. E. and Jones, P. D., 2003. Global surface temperatures over the past two millennia. Geophysical Research Letters, 30, 1820, doi:10.1029/2003GL017814.CrossRefGoogle Scholar
Mann, M. E., Bradley, R. S., and Hughes, M. K., 1998. Global-scale temperature patterns and climate forcing over the past six centuries. Nature, 392, 779–87.CrossRefGoogle Scholar
Mann, M. E., Bradley, R. S., and Hughes, M. K., 1999. Northern Hemisphere temperatures during the past millennium: inferences, uncertainties, and limitations. Geophysical Research Letters, 26, 759–62.CrossRefGoogle Scholar
McCormick, M. P. and Veiga, R. E., 1992. SAGE II measurements of early Pinatubo aerosols. Geophysical Research Letters, 19, 155–8.CrossRefGoogle Scholar
Meehl, G. A., Washington, W. M., Ammann, C. M., et al., 2004. Combinations of natural and anthropogenic forcings in twentieth-century climate. Journal of Climate, 17, 3721–7.2.0.CO;2>CrossRefGoogle Scholar
Meehl, G. A., Washington, W. M., Santer, B. D., et al., 2006. Climate change projections for the twenty-first century and climate change commitment in the CCSM3. Journal of Climate, 19, 2597–616.CrossRefGoogle Scholar
Meehl, G. A., Stocker, T. F., Collins, W. D., et al., 2007. Global climate projections. In Climate Change 2007: the Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M., et al. Cambridge University Press, pp. 747–845.Google Scholar
Meissner, K. J. and Clark, P. U., 2006. Impact of floods versus routing events on the thermohaline circulation. Geophysical Research Letters, 33, L15 704, doi:10.1029/2006GL026705.CrossRefGoogle Scholar
North, G. R., Biondi, F., Bloomfield, P., et al., 2006. Surface Temperature Reconstructions for the Last 2,000 Years. The National Academies Press, 145 pp.Google Scholar
Otto-Bliesner, B. L., Brady, E. C., and Shields, C., 2002. Late Cretaceous ocean: coupled simulations with the National Center for Atmospheric Research Climate System Model. Journal of Geophysical Research, 107D, 4019, 10.1029/2001JD000821.CrossRefGoogle Scholar
Overpeck, J. and Webb, R., 2000. Nonglacial rapid climate events: past and future. Proceedings of the National Academy of Sciences, USA, 97, 1335–8.CrossRefGoogle ScholarPubMed
Peltier, W. R., 1994. Ice age paleotopography. Science, 265, 195–201.CrossRefGoogle ScholarPubMed
Petit, J. R., Mounier, L., Jouzel, J., et al., 1990. Palaeoclimatological and chronological implications of the Vostok core dust record. Nature, 343, 56–8.CrossRefGoogle Scholar
Petit, J. R., Jouzel, J., Raynaud, D., et al., 1999. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature, 399, 429–36.CrossRefGoogle Scholar
Prell, W. L. and Kutzbach, J. E., 1992. Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution. Nature, 360, 647–52.CrossRefGoogle Scholar
Raupach, M. R., Marland, G., Ciais, P., et al., 2007. Global and regional drivers of accelerating CO2 emissions. Proceedings of the National Academy of Sciences, USA, 104, 10 288–93.CrossRefGoogle ScholarPubMed
Renssen, H., Goosse, H., Fichefet, T., and Campin, J.-M., 2001. The 8.2 kyr BP event simulated by a global atmosphere–sea ice–ocean model. Geophysical Research Letters, 28, 1567–70.CrossRefGoogle Scholar
Robock, A. and Mao, J., 1995. The volcanic signal in surface temperature observations. Journal of Climate, 8, 1086–103.2.0.CO;2>CrossRefGoogle Scholar
Robock, A. and Matson, M., 1983. Circumglobal transport of the El Chichón volcanic dust cloud. Science, 221, 195–7.CrossRefGoogle ScholarPubMed
Ruddiman, W. F. and Kutzbach, J. E., 1989. Forcing of late Cenozoic Northern Hemisphere climate by plateau uplift in southern Asia and the American west. Journal of Geophysical Research, 94D, 18 409–27.CrossRefGoogle Scholar
Ruddiman, W. F. and Kutzbach, J. E., 1991. Plateau uplift and climatic change. Scientific American, 264(3), 66–75.CrossRefGoogle Scholar
Ruddiman, W. F., Prell, W. L., and Raymo, M. E., 1989. Late Cenozoic uplift in southern Asia and the American west: rationale for general circulation modeling experiments. Journal of Geophysical Research, 94D, 18 379–91.CrossRefGoogle Scholar
Ruddiman, W. F., Kutzbach, J. E., and Prentice, I. C., 1997. Testing the climatic effects of orography and CO2 with general circulation and biome models. In Tectonic Uplift and Climate Change, ed. Ruddiman, W. F.. Plenum Press, pp. 203–35.CrossRefGoogle Scholar
Schmittner, A., Yoshimori, M., and Weaver, A. J., 2002. Instability of glacial climate in a model of the ocean–atmosphere–cryosphere system. Science, 295, 1489–93.CrossRefGoogle Scholar
Shackleton, N. J., 2000. The 100,000-year ice-age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity. Science, 289, 1897–902.CrossRefGoogle ScholarPubMed
Siegenthaler, U., Stocker, T. F., Monnin, E., et al., 2005. Stable carbon cycle–climate relationship during the late Pleistocene. Science, 310, 1313–17.CrossRefGoogle ScholarPubMed
Spahni, R., Chappellaz, J., Stocker, T. F., et al., 2005. Atmospheric methane and nitrous oxide of the late Pleistocene from Antarctic ice cores. Science, 310, 1317–21.CrossRefGoogle ScholarPubMed
Stenchikov, G. L., Kirchner, I., Robock, A., et al., 1998. Radiative forcing from the 1991 Mount Pinatubo volcanic eruption. Journal of Geophysical Research, 103D, 13 837–57.CrossRefGoogle Scholar
Stommel, H. and Stommel, E., 1979. The year without a summer. Scientific American, 240(6), 176–86.CrossRefGoogle Scholar
Stott, P. A., Jones, G. S., Lowe, J. A., et al., 2006. Transient climate simulations with the HadGEM1 climate model: causes of past warming and future climate change. Journal of Climate, 19, 2763–82.CrossRefGoogle Scholar
Teller, J. T., Leverington, D. W., and Mann, J. D., 2002. Freshwater outbursts to the oceans from glacial Lake Agassiz and their role in climate change during the last deglaciation. Quaternary Science Reviews, 21, 879–87.CrossRefGoogle Scholar
Tett, S. F. B., Jones, G. S., Stott, P. A., et al., 2002. Estimation of natural and anthropogenic contributions to twentieth century temperature change. Journal of Geophysical Research, 107D, 4306, 10.1029/2000JD000028.CrossRefGoogle Scholar
Trenberth, K. E., Jones, P. D., Ambenje, P., et al., 2007. Observations: Surface and atmospheric climate change. In Climate Change 2007: the Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M., et al. Cambridge University Press, pp. 235–336.Google Scholar
Grafenstein, U., Erlenkeuser, H., Müller, J., Jouzel, J., and Johnsen, S., 1998. The cold event 8200 years ago documented in oxygen isotope records of precipitation in Europe and Greenland. Climate Dynamics, 14, 73–81.CrossRefGoogle Scholar
Watson, B. (ed.), 1990. New England's Disastrous Weather. Yankee Books, 228 pp.Google Scholar
Wright, H. E., Kutzbach, J. E., Webb, III T., et al., (eds.) 1993. Global Climates since the Last Glacial Maximum. University of Minnesota Press, 569 pp.Google Scholar
Zhisheng, A., Kutzbach, J. E., Prell, W. L., and Porter, S. C., 2001. Evolution of Asian monsoons and phased uplift of the Himalaya–Tibetan plateau since Late Miocene times. Nature, 411, 62–6.CrossRefGoogle ScholarPubMed

Save book to Kindle

To save this book to your Kindle, first ensure no-reply@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

  • Climate change
  • Gordon B. Bonan, National Center for Atmospheric Research, Boulder, Colorado
  • Book: Ecological Climatology
  • Online publication: 05 April 2013
  • Chapter DOI: https://doi.org/10.1017/CBO9780511805530.009
Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

  • Climate change
  • Gordon B. Bonan, National Center for Atmospheric Research, Boulder, Colorado
  • Book: Ecological Climatology
  • Online publication: 05 April 2013
  • Chapter DOI: https://doi.org/10.1017/CBO9780511805530.009
Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

  • Climate change
  • Gordon B. Bonan, National Center for Atmospheric Research, Boulder, Colorado
  • Book: Ecological Climatology
  • Online publication: 05 April 2013
  • Chapter DOI: https://doi.org/10.1017/CBO9780511805530.009
Available formats
×