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leads to ensemble spread in polar bear outcomes. However,
Amstrup et al. note that these projections may be overly op-
timistic, given Stroeve et al .'s [2007] finding that real-world
Arctic sea ice has declined at almost twice the rate found
in model simulations of the recent past. The USGS efforts
culminated in Amstrup et al.'s synthesis report, which uses
a Bayesian framework to assess the probability of decline
in polar bear population based on consideration of sea ice
decline and other factors. Despite the uncertainties of the re-
search, none of the outcomes were favorable for polar bears;
in effect, they run the gamut from bad to extremely bad.
In May 2008 the polar bear was listed as a threatened spe-
cies under ESA, after considerable delay. It is clear from
the final rule [ U.S. Fish and Wildlife Service , 2008] that
the policy makers understood and considered the scientific
guidance. Consideration of the science is also evident from
the announcement of the decision (www.doi.gov/secretary/
speeches/08405_speech.html), which included a prominent
display of Stroeve et al .'s [200X] work on observed and sim-
ulated sea ice trends, and maps of Arctic sea ice showing
the change in coverage by old (at least 5 years) and new
(less than 5 years old) ice, apparently from the drift model
of Rigor and Wallace [2004]. But while the effort to pro-
vide scientific input for the listing decision was successful
in some sense, it remains to be seen if the listing will have
any direct effect on the status of the polar bear (see analysis
of Revkin [2008]).
Comiso, J. C., C. L. Parkinson, R. Gersten, and L. Stock (2008),
Accelerated decline in the Arctic sea ice cover, Geophys. Res.
Lett ., 35 , L0703, doi:0.029/2007GL03972.
Deser, C., and H. Teng (2008), Recent trends in Arctic sea ice and
the evolving role of atmospheric circulation forcing, 979-2007,
this volume.
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chon (2008), Reconstructing sea-ice conditions in the Arctic and
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surface energy budget, this volume.
Durner, G. M., et al. (2008), Predicting 2st century polar bear
habitat distribution from global climate models, Ecol. Monogr .,
in press.
Gorodetskaya, I. v., and L.-B. Tremblay (2008), Arctic cloud prop-
erties and radiative forcing from observations and their role in
sea ice decline predicted by the NCAR CCSM3 model during the
2st century, this volume.
Holland, M. M., C. M. Bitz, and B. Tremblay (2006), Future abrupt
reductions in the summer Arctic sea ice, Geophys. Res. Lett ., 33 ,
L23503, doi:0.029/2006GL028024.
Holland, M. M., C. M. Bitz, B. Tremblay, and D. A. Bailey (2008),
The role of natural versus forced change in future rapid summer
Arctic ice loss, this volume.
Kay, J. E., T. L'Ecuyer, A. Gettelman, G. Stephens, and C. O'Dell
(2008), The contribution of cloud and radiation anomalies to the
2007 Arctic sea ice extent minimum, Geophys. Res . Lett ., 35 ,
L08503, doi:0.029/2008GL03345.
Kerr, R. A. (2007), Is battered sea ice down for the count?, Science ,
318 , 33-34.
Kizzia, T. (2008), Polar ice pack loss may break 2007 record, An-
chorage Daily News , 2 Feb.
Lindsay, R. W., and J. Zhang (2005), The thinning of Arctic sea
ice, 988-2003: Have we passed a tipping point?, J. Clim ., 18 ,
4879-4894.
Maslanik J. A., C. Fowler, J. Stroeve, S. Drobot, J. Zwally, D. Yi,
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Lett ., 34 , L2450, doi:0.029/2007GL032043.
Meier, W. N., J. Stroeve, and F. Fetterer (2007), Wither Arctic sea
ice? A clear signal of decline, regionally, seasonally, and extend-
ing beyond the satellite record, Ann. Glaciol ., 46 , 428-434.
Merryfield, W. J., M. M. Holland, and A. H. Monahan (2008), Mul-
tiple equilibria and abrupt transitions in Arctic summer sea ice
extent, this volume.
Nghiem, S. v., I. G. Rigor, D. K. Perovich, P. Clemente-Colón,
J. W. Weatherly, and G. Neumann (2007), Rapid reduction
of Arctic perennial sea ice, Geophys. Res. Lett ., 34 , L9504,
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(2008), Sunlight, water, and ice: Extreme Arctic sea ice melt
5. CONCLUSION
The events of 2007 and 2008 highlight the need for im-
proved understanding of sea ice sensitivity and the impacts
of sea ice decline. Perhaps, if we are fortunate, our under-
standing of the Arctic sea ice and climate system can evolve
fast enough to keep pace with the changes occurring there.
Acknowledgments .The author's research is supported by the Of-
fice of Science (BER), U.S. Department of Energy, grant DE-FG02-
03ER63604. I thank Cecilia Bitz, Steven Amstrup and members of
the NCAR Polar Climate Working Group for helpful conversations.
I am indebted to the chapter authors for contributing their best work
to this monograph.
REFERENCES
Amstrup, S. C., B. G. Marcot, and D. C. Douglas (2008), A Baye-
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Bitz, C. M. (2008), Some aspects of uncertainty in predicting sea
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Borenstein, S., and D. Joling (2008), Arctic sea ice drops to 2nd
lowest level on record, San Francisco Chron ., 27 Aug.
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