Hostname: page-component-cd9895bd7-p9bg8 Total loading time: 0 Render date: 2024-12-25T18:28:29.443Z Has data issue: false hasContentIssue false
  • English
  • Français

Paleoclimatic Research: Status and Opportunities

Published online by Cambridge University Press:  20 January 2017

Alan D. Hecht ,
Roger Barry ,
Harold Fritts ,
John Imbrie ,
John Kutzbach ,
J.Murray Mitchell  and
Samuel M. Savin
Alan D. Hecht
Affiliation:
Institute of Arctic and Alpine Research, University of Colorado, Boulder, Colorado
Roger Barry
Affiliation:
Institute of Arctic and Alpine Research, University of Colorado, Boulder, Colorado
Harold Fritts
Affiliation:
Laboratory of Tree-Ring Research, University of Arizona, Tucson, Arizona
John Imbrie
Affiliation:
Department of Geological Sciences, Brown University, Providence, Rhode Island
John Kutzbach
Affiliation:
Center for Climatic Research, University of Wisconsin, Madison, Wisconsin
J.Murray Mitchell
Affiliation:
Environmental Data Service, NOAA, Washington, D.C.
Samuel M. Savin
Affiliation:
Department of Earth Sciences, Case Western Reserve University, Cleveland, Ohio
Get access Rights & Permissions [Opens in a new window]

Abstract

This report considers the scientific opportunities and problems for paleoclimatic research for three time intervals, 0-1000 yr, 0-30,000 yr, and 0-1 my. Each of these intervals is appropriate to understanding different parts of the climate problem. The most recent interval is one for which there exists the possibility of determining year-by-year changes in certain parts of the climatic system over a time span which overlaps the instrumental record. The interval 0 to 30,000 yr is one for which the response of many parts of the climate system during a major change in climate can be examined, and for which laC dating provides good chronological control. The interval 0 to 1.000,000 yr is one for which there is reasonably good chronological control. a well-developed global record of changes in the ocean, and the opportunity of investigating glacial-interglacial changes in global climate which appear to have a cyclic or quasi-cyclic component.

Type
Research Article
Information
Quaternary Research , Volume 12 , Issue 1 , July 1979 , pp. 6 - 17
Copyright
University of Washington

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

Bernabo, J.C., Webb, T.C., (1977). Changing patterns in the Holocene pollen records of northeastern N. America: A Mapped Summary. Quaternary Research. 8, 64–96.CrossRefGoogle Scholar
Batten, E.S., (1975). The effects of a stratospheric dust cloud as simulated by a general circulation model. Weller, G., Bowling, S.A., Proceedings of the 24th Alaska Scientific Conference. University of Alaska 150–158.Google Scholar
Berger, A., (1977). Power and limitation of an energy-balance climate model as applied to the astronomical theory of paleoclimates. Palaeography, Palaeoclimatology, Palaeoecology. 21, 227–236.CrossRefGoogle Scholar
Blasing, T.J., Fritts, H.C., (1976). Reconstructing Past Climatic Anomalies in the North Pacific and Western North Africa from Tree Ring Data. Quaternary Research. 6, 563–580.CrossRefGoogle Scholar
Bryson, R.A., Wendland, W.M., Ives, J.D., Andrews, J.T., (1969). Radiocarbon isochromes on the disintegration of the Laurentide ice sheet. Arctic and Alpine Research. 1, 1–14.CrossRefGoogle Scholar
Charney, J., Quirk, W.J., Chow, S., Kornfield, J., (1977). A comparative study of the effects of albedo change on drought in semi-arid regions. Journal of Atmospheric Sciences. 34, 1366–1385.2.0.CO;2>CrossRefGoogle Scholar
Cline, R.M., Hays, J., (1976) Investigation of Late Quaternary Paleogeography and Paleoclimatology. Geological Society America Memoir 145, Boulder, Colo..Google Scholar
Coope, G.R., (1975). Climate Fluctuations in Northwest Europe since the last interglacial, indicated by fossil assemblages of Coleoptera. Ice Age, Ancient and Modern. House Press, Liverpool. Google Scholar
Denton, G.M., Karlen, W., (1973). Holocene climatic variations—their patterns and possible causes. Quaternary Research. 3, 155–206.CrossRefGoogle Scholar
Eddy, J.A., (1977). The case of the missing sunspots. Scientific American. 236, 80–92.CrossRefGoogle Scholar
Epstein, S., Yapp, C., (1976). Climatic implications of the D/H ratio of hydrogen in CH groups in tree cellulose. Earth and Planetary Science Letters. 30, 252–261.CrossRefGoogle Scholar
Fletcher, J.O., Mintz, Y., Arakawa, A., Fox, T., (1973). Numerical Simulation of the Influence of Arctic Sea Ice on Climate. WHO Technical Note No. 129. W.M.O, Geneva, 181–218.Google Scholar
Frankignoul, C., Hasselmann, K., (1977). Stochastic climate models, Part II. Application to sea surface temperature anomalies. Tellus. 28, 473–485.Google Scholar
Fritts, H.C., Blasing, T.J., Mayden, B.P., Kutzbach, J.E., (1971). Multivariate techniques for specifying tree growth and climate relationships and for reconstructing anomalies in paleotemperature. Journal of Applied Meteorology. 10, 845–864.2.0.CO;2>CrossRefGoogle Scholar
Fritts, H.C., (1976) Tree Rings and Climate. Academic Press, London. Google Scholar
Gates, W.L., (1976a). Modeling the ice-age climate. Science. 191, 1131–1144.CrossRefGoogle ScholarPubMed
Gates, W.L., (1976b). The numerical simulation of ice-age climate with a global general circulation model. Journal of Atmospheric Science. 33, 1844–1873.2.0.CO;2>CrossRefGoogle Scholar
Hasselmann, K., (1976). Stochastic climate models, Part I. Theory. Tellus. 28, 473–484.Google Scholar
Hays, B.D., Imbrie, J., Shackleton, N.J., (1976). Variations in the earth's orbit: Pacemaker of the Ice Ages. Science. 194, 1121–1132.CrossRefGoogle ScholarPubMed
Hughes, T., Denton, G.H., Grosswald, M.G., (1977). Was there a late-warm Arctic ice sheet?. Nature (London). 266, 596–602.CrossRefGoogle Scholar
Hunt, B.G., (1976). A simulation of the possible consequences of a volcanic eruption on the general circulation of the atmosphere. Monthly Weather Review. 165, 247–260.Google Scholar
Kukla, G.J., (1975). Missing link between Milankovitch and climate. Nature (London). 253, 600–603.CrossRefGoogle Scholar
Kutzbach, J.E., Chervin, R.M., Houghton, D.D., (1977). Response of the NCAR GCM to prescribed changes in ocean surface temperature. Part I: Mid-latitude changes. Journal of Atmospheric Sciences. 34, 1200–1213.2.0.CO;2>CrossRefGoogle Scholar
Ladurie, E.L., (1971) Times of Feast. Times of Famine: A History of Climate Since the Year 1,000. Doubleday, New York. Google Scholar
Lamb, H.H., Johnson, A.I., (1966) Secular Variations of the Atmospheric-Circulation since AD 1750. Geophysical Memoir, London No. 110.Google Scholar
Lamb, H.H., (1970). Volcanic dust in the atmosphere; with a chronology and an assessment of its meteorological significance. Philosophical Transactions of the Royal Society, London, A. 266, 425–533.Google Scholar
Lamb, H.H., (1977) Climate: Present, Past and Future. Vol. 2, Methuen, London. Google Scholar
Livingstone, D.A., (1975). Late Quaternary Climatic Change in Africa. Annual Review of Ecology and Systematics. 6, 249–280.CrossRefGoogle Scholar
MacCracken, M.C., (1970) Test of Ice Theories Using a Zonal Atmsopheric Model. Lawrence Radiation Lab, Livermore, Calif, URCL 72803.Google Scholar
Manabe, S., Wetherald, R.T., (1975). The effects of doubling the CO2 concentrations on the climate of a general circulation model. Journal of Atmsopheric Sciences. 32, 3–15.2.0.CO;2>CrossRefGoogle Scholar
Manabe, S., Hahn, D.G., (1977). Simulation of the tropical climate of an ice age. Journal of Geophysical Research. 82, 3889–3911.CrossRefGoogle Scholar
Mass, C., Schneider, S.H., (1977). Statistical evidence on the influence of sunspots and volcanic dust on long term temperature records. Journal of Atmsopheric Science. 34, 1995–2004.Google Scholar
Mitchell, J.M., (1963). On the worldwide pattern of secular temperature change. Changes of Climate, Arid Zone Research. Vol. 20, Unesco, Paris, 161–181.Google Scholar
Newson, R., (1973). Response of a general circulation model of the atmosphere to removal of the Arctic ice-cap. Nature (London). 241, 39–40.CrossRefGoogle Scholar
Rognon, P., Williams, M.A.J., (1977). Late Quaternary climatic changes in Australia and N. Africa: A preliminary interpretation. Paleogeography, Paleoclimatology, Paleoecology. 21, 285–327.CrossRefGoogle Scholar
Roundtree, P.R., (1972). The influence of tropical east Pacific Ocean temperatures in the atmosphere. Quaternary Journal Royal Meteorological Society. 98, 290–321.Google Scholar
Saltzman, B., Vernekar, A.D., (1971). Note on the effect of earth orbital variations on climate. Journal of Geophysical Research. 76, 4195–4197.CrossRefGoogle Scholar
Saltzman, B., Vernekar, A.D., (1975). A solution for the Northern Hemisphere climatic zonation during a glacial maximum. Quaternary Research. 5, 307–320.CrossRefGoogle Scholar
Schneider, S.H., Gal-Chen, T., (1973). Numerical experiments in climatic stability. Journal of Geophysical Research. 78, 27 6182–6194.CrossRefGoogle Scholar
Sellers, W.D., (1974). Climate models and variations in the solar constant. Geofisica International. 14, 303–315.CrossRefGoogle Scholar
Shaw, D.M., Donn, W.L., (1971). A thermodynaic study of arctic paleoclimatology. Quaternary Research. 1, 175–187.CrossRefGoogle Scholar
Suarez, M.J., Held, I.M., (1976). Modelling climatic response to orbital parameter variations. Nature (London). 263, 46–47.CrossRefGoogle Scholar
Van Loon, H., Williams, J., (1976). The connection between trends of mean temperature and circulation at the surface. Winter Monthly Review. 104, 365–380 Part I.2.0.CO;2>CrossRefGoogle Scholar
Warshaw, M., Rapp, R.R., (1973). An experiment on the sensitivity of global circulation model. Journal Applied Meteorology. 12, 43–49.2.0.CO;2>CrossRefGoogle Scholar
Washington, W.M., (1972). Numerical climatic change experiments: The effect of man's production of thermal energy. Journal of Applied Meteorology. 11, 768–772.2.0.CO;2>CrossRefGoogle Scholar
Wetherald, R.T., Manabe, S., (1975). The effects of changing the solar constant on the climate of a general circulation model. Journal of Atmospheric Sciences. 32, 2044–2059.2.0.CO;2>CrossRefGoogle Scholar
Williams, J., (1975). The influence of snowcover on the atmospheric circulation and its role in climatic change: An analysis based on results from the NCAR global circulation model. Journal of Applied Meteorology. 14, 137–152.2.0.CO;2>CrossRefGoogle Scholar
Williams, J., Barry, R.G., Washington, W.M., (1974). Simulation of the atmospheric circulation using the NCAR global circulation model with ice age boundary conditions. Journal of Applied Meteorology. 13, 3 305–317.2.0.CO;2>CrossRefGoogle Scholar
Yapp, C., Epstein, S., (1977). Climatic implications of D/H ratios of Meteoric waters over North America (9500-22,000 B.P.) as inferred from ancient wood cellulose CH hydrogen. Earth and Planetary Science Letters. 34, 333–350.CrossRefGoogle Scholar