TY - JOUR
T1 - A comparison of the CCM1-simulated climates for pre-industrial and present-day CO2 levels
AU - Marshall, Susan
AU - Mann, Michael E.
AU - Oglesby, Robert J.
AU - Saltzman, Barry
N1 - Funding Information:
This research has been supported by the Electric Power Research Institute (EPRI), Contract No. 2333-11 at Yale University as part of the Model Evaluation Consortium for Climatic Assessment (MECCA), and by the Department of Energy grant DE-FG02-85ER14144 to W. Prell, J. Kutzbach, R.J. Oglesby and T. Webb. Partial support was also provided by the Climate Dynamics Program of the National Science Foundation under grant ATM-9222591 to Yale University and by the Climate and Global Change Program of the National Oceanic and Atmospheric Administration under grant NA36GP0396 to the University of North Carolina at Charlotte and Scripps Institution of Oceanography. The computations were made at the National Center for Atmospheric Research (NCAR), which is sponsored by the National Science Foundation, with computing grant 36211011 from the NCAR Scientific Computing Division. Additional computational support was provided under the MECCA program. The suggestions of two anonymous reviewers were appreciated.
PY - 1995/4
Y1 - 1995/4
N2 - A comparison is made between the climatic equilibria of the NCAR CCM for a pre-industrial atmospheric CO2 level (265 ppm) and a current (circa 1975) level of 330 ppm, including statistical estimates of the level of confidence in the implied changes. We also compare the model results to observations compiled over the past 100 years, which corresponds to roughly half of the period of change in CO2 from pre-industrial (1800) to current levels. A relatively large model response in surface temperature and a smaller response in the precipitation, surface pressure, and storm track fields is obtained. These results are in accord with previous findings of the climate sensitivity to systematic changes in CO2 forcings. A t-statistic of the model results indicates a significant surface temperature response to a relatively small change in CO2, above the inherent model variability. Observations of global surface temperature anomalies for the period 1890-1990 show some similarities to the model results, especially a warming in regions of the wintertime northern hemisphere of 2-3° C. A point-by-point correlation of the 330 ppm minus 265 ppm model temperature differences to the observed 1980-1890 differences suggests that some of the variance in the observed trends in the surface temperature anomalies may be explained by the model experiments.
AB - A comparison is made between the climatic equilibria of the NCAR CCM for a pre-industrial atmospheric CO2 level (265 ppm) and a current (circa 1975) level of 330 ppm, including statistical estimates of the level of confidence in the implied changes. We also compare the model results to observations compiled over the past 100 years, which corresponds to roughly half of the period of change in CO2 from pre-industrial (1800) to current levels. A relatively large model response in surface temperature and a smaller response in the precipitation, surface pressure, and storm track fields is obtained. These results are in accord with previous findings of the climate sensitivity to systematic changes in CO2 forcings. A t-statistic of the model results indicates a significant surface temperature response to a relatively small change in CO2, above the inherent model variability. Observations of global surface temperature anomalies for the period 1890-1990 show some similarities to the model results, especially a warming in regions of the wintertime northern hemisphere of 2-3° C. A point-by-point correlation of the 330 ppm minus 265 ppm model temperature differences to the observed 1980-1890 differences suggests that some of the variance in the observed trends in the surface temperature anomalies may be explained by the model experiments.
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U2 - 10.1016/0921-8181(94)00024-8
DO - 10.1016/0921-8181(94)00024-8
M3 - Article
AN - SCOPUS:0029503804
SN - 0921-8181
VL - 10
SP - 163
EP - 180
JO - Global and Planetary Change
JF - Global and Planetary Change
IS - 1-4
ER -