-
1
-
-
0002329078
-
-
J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge)
-
J. A. Church et al., in Climate Change 2001: The Scientific Basis, J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge, 2001), pp. 639-693.
-
(2001)
Climate Change 2001: The Scientific Basis
, pp. 639-693
-
-
Church, J.A.1
-
4
-
-
0000212834
-
-
J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge)
-
F. P. Bretherton et al., in Climate Change: The IPCC Scientific Assessment, J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge, 1990), pp. 173-194.
-
(1990)
Climate Change: The IPCC Scientific Assessment
, pp. 173-194
-
-
Bretherton, F.P.1
-
5
-
-
0000704981
-
-
J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge)
-
A. Kattenberg et al., in Climate Change 1995: The Science of Climate Change, J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge, 1995), pp. 285-357.
-
(1995)
Climate Change 1995: The Science of Climate Change
, pp. 285-357
-
-
Kattenberg, A.1
-
6
-
-
0002289566
-
-
J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge)
-
U. Cubasch et al., in Climate Change 2001: The Scientific Basis, J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge, 2001), pp. 525-582.
-
(2001)
Climate Change 2001: The Scientific Basis
, pp. 525-582
-
-
Cubasch, U.1
-
8
-
-
84905428558
-
-
R. A. Warrick et al., Eds. (Cambridge Univ. Press, Cambridge)
-
T. M. L. Wigley, S. Raper, in Climate and Sea Level Change: Observations, Projections and Implications, R. A. Warrick et al., Eds. (Cambridge Univ. Press, Cambridge, 2003), pp. 111-133.
-
(2003)
Climate and Sea Level Change: Observations, Projections and Implications
, pp. 111-133
-
-
Wigley, T.M.L.1
Raper, S.2
-
12
-
-
2042527678
-
-
G. A. Meehl et al., J. Clim. 17, 1584 (2004).
-
(2004)
J. Clim.
, vol.17
, pp. 1584
-
-
Meehl, G.A.1
-
14
-
-
7744219639
-
-
G. A. Meehl et al., J. Clim. 17, 3721 (2004).
-
(2004)
J. Clim.
, vol.17
, pp. 3721
-
-
Meehl, G.A.1
-
16
-
-
15244356414
-
-
For a description of the CCSM3, see www.ccsm.ucar.edu.
-
-
-
-
17
-
-
0042867240
-
-
B. D. Santer et al., Science 301, 479 (2003).
-
(2003)
Science
, vol.301
, pp. 479
-
-
Santer, B.D.1
-
18
-
-
15244360332
-
-
note
-
The 20th-century solar forcing in the PCM is from (33). The 20th-century solar forcing in the CCSM3 is from (34).
-
-
-
-
19
-
-
0001886562
-
-
J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge)
-
C. K. Folland et al., in Climate Change 2001: The Scientific Basis, J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge, 2001), pp. 99-181.
-
(2001)
Climate Change 2001: The Scientific Basis
, pp. 99-181
-
-
Folland, C.K.1
-
21
-
-
3042856775
-
-
J. A. Church et al., J. Clim. 17, 2609 (2004).
-
(2004)
J. Clim.
, vol.17
, pp. 2609
-
-
Church, J.A.1
-
22
-
-
0002155033
-
-
J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge)
-
V. Ramaswamy, in Climate Change 2001: The Scientific Basis, J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge, 2001), pp. 349-416.
-
(2001)
Climate Change 2001: The Scientific Basis
, pp. 349-416
-
-
Ramaswamy, V.1
-
23
-
-
0001272853
-
-
J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge)
-
I. C. Prentice et al., in Climate Change 2001: The Scientific Basis, J. T. Houghton et al., Eds. (Cambridge Univ. Press, Cambridge, 2001), pp. 183-237.
-
(2001)
Climate Change 2001: The Scientific Basis
, pp. 183-237
-
-
Prentice, I.C.1
-
29
-
-
2042475909
-
-
A. Hu et al., J. Clim. 17, 4267 (2004).
-
(2004)
J. Clim.
, vol.17
, pp. 4267
-
-
Hu, A.1
-
31
-
-
0034210146
-
-
G. A. Meehl et al., J. Clim. 13, 1879 (2000).
-
(2000)
J. Clim.
, vol.13
, pp. 1879
-
-
Meehl, G.A.1
-
32
-
-
15244344567
-
-
note
-
The sea level rise at the year 2100 in the 20th-century stabilization experiment is greater in the CCSM3 than in the PCM in Fig. 1C relative to the 1980-1999 base period, but they both have about the same percentage increase as compared to the total sea level rise that occurred during the 20th century in the respective models as depicted in Fig. 3. This is because the CCSM3 has greater total sea level rise during the 20th century than does the PCM (4.5 cm compared to 3.0 cm, respectively), partly due to the higher sensitivity of the CCSM3 as well as the comparative meridional overturning circulation processes discussed in the text.
-
-
-
-
34
-
-
33646500082
-
-
10.1029/2001JD001143
-
J. Lean et al., Geophys. Res. Lett. 107, 10.1029/2001JD001143 (1995).
-
(1995)
Geophys. Res. Lett.
, vol.107
-
-
Lean, J.1
-
35
-
-
15244346351
-
-
note
-
We acknowledge the efforts of a large group of scientists at the National Center for Atmospheric Research (NCAR), at several U.S. Department of Energy (DOE) and National Oceanic and Atmospheric Administration labs, and at universities across the United States who contributed to the development of the CCSM3 and who participated in formulating the 20th-century and future climate change simulations through the CCSM working groups on atmosphere, ocean, land surface, polar climate, climate change, climate variability, paleoclimate, biogeochemistry, and software engineering. In particular, we thank A. Middleton and V. Wayland from NCAR and M. Wehner at the National Energy Research Scientific Computing Center (NERSC) for their work in either running the model experiments or managing the massive amount of model data. The formidable quantity of supercomputer resources required for this ambitious modeling effort was made available at NCAR through the initiative Nodes and the Climate System laboratory and through DOE as part of its Advanced Scientific Research (ASCR). ASCR provides computing facilities at NERSC, Los Alamos National Laboratory (LANL), and the Oak Ridge National Laboratory (ORNL) Center for Computational Science. Additional simulations with the CCSM3 were performed by the Central Research Institute for the Electric Power Industry (CRIEPI), using the Earth Simulator in Japan through the international research consortium of CRIEPI, NCAR, and LANL under the Project for Sustainable Coexistence of Human Nature and the Earth of the Japanese Ministry of Education, Culture, Sports, Science and Technology. Portions of this study were supported by the Office of Biological and Environmental Research, DOE, as part of its Climate Change Prediction Program; and by the National Center for Atmospheric Research. This work was also supported in part by the Weather and Climate Impact Assessment Initiative at NCAR. NCAR is sponsored by NSF.
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