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Science 14 November 1997: Vol. 278. no. 5341, pp. 1251 - 1256 DOI: 10.1126/science.278.5341.1251
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Articles
Arctic Environmental Change of the Last Four Centuries
J. Overpeck,
*
K. Hughen,
D. Hardy,
R. Bradley,
R. Case,
M. Douglas,
B. Finney,
K. Gajewski,
G. Jacoby,
A. Jennings,
S. Lamoureux,
A. Lasca,
G. MacDonald,
J. Moore,
M. Retelle,
S. Smith,
A. Wolfe,
G. Zielinski
A compilation of paleoclimate records from lake sediments, trees,
glaciers, and marine sediments provides a view of circum-Arctic environmental variability over the last 400 years. From 1840 to the
mid-20th century, the Arctic warmed to the highest temperatures in four
centuries. This warming ended the Little Ice Age in the Arctic and has
caused retreats of glaciers, melting of permafrost and sea ice, and
alteration of terrestrial and lake ecosystems. Although warming,
particularly after 1920, was likely caused by increases in atmospheric
trace gases, the initiation of the warming in the mid-19th century
suggests that increased solar irradiance, decreased volcanic activity,
and feedbacks internal to the climate system played roles.
J. Overpeck is at the National Oceanographic and Atmospheric
Administration (NOAA)-National Geophysical Data Center (NGDC)
Paleoclimatology Program, 325 Broadway, Boulder, CO 80303, USA, and
Institute of Arctic and Alpine Research (INSTAAR), University of
Colorado, Boulder, CO 80309, USA. K. Hughen, A. Jennings, J. Moore, and A. Wolfe are at INSTAAR, University of Colorado, Boulder, CO
80309, USA. D. Hardy, R. Bradley, and S. Smith are in the Department of
Geosciences, University of Massachusetts, Amherst, MA 01003, USA.
R. Case and G. MacDonald are in the Department of Geography, University
of California, Los Angeles, CA 90095, USA. M. Douglas is in the
Department of Geology, University of Toronto, Toronto, Ontario M5S 3B1,
Canada. B. Finney is at the Institute of Marine Science, University of
Alaska, Fairbanks, AK 99775, USA. K. Gajewski is in the Department
of Geography, University of Ottawa, Ottawa, Ontario K1N 6N5, Canada. G. Jacoby is at the Lamont-Doherty Earth Observatory, Columbia University,
Palisades, NY 10964, USA. S. Lamoureux is in the Department of
Earth and Atmospheric Sciences, University of Alberta, Edmonton,
Alberta T6G 2H3, Canada. A. Lasca and M. Retelle are in the Geology
Department, Bates College, Lewiston, ME 04204, USA. G. Zielinski
is at the Climate Change Research Center, University of New Hampshire,
Durham, NH 03824, USA.
*
To whom correspondence should be addressed. E-mail:
jto{at}ngdc.noaa.gov
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