This figure, based on Meehl et al. (2004), shows the ability of a global climate model (the DOE PCM ) to reconstruct the historical temperature record and the degree to which the associated temperature changes can be decomposed into various forcing factors. The top part of the figure compares a five year average of global temperature measurements (Jones and Moberg 2001) to the Meehl et al. results incorporating the effects of five predetermined forcing factors: greenhouse gases, man-made sulfate emissions, solar variability, ozone changes (both stratospheric and tropospheric), and volcanic emissions (including natural sulfates). The time history and radiative forcing qualities for each of these factors was specified in advance and was not adjusted to specifically match the temperature record.
Also shown are grey bands indicating the 68% and 95% range for natural variability in temperature relative to the climatic expectation as determined from multiple simulations with different initial conditions. In other words, they indicate the estimated size of variations that are expected to occur due to fluctuation in weather rather than changes in climate. Ideally the model should be able to reconstruct temperature variations to within about the tolerance specified by these bands. Some of the remaining misfit may be accounted for by the ~0.05 °C uncertainty in the temperature reconstruction. However, though the model captures the gross features of twentieth century climate change, it remains likely that some of the differences between model and observation still reflect the limitations of the model and/or our understanding of the histories of the observed forcing factors.
In the lower portion of the figure are the results of additional simulations in which the model was operated with only one forcing factor used at a time. A key conclusion of the Meehl et al. (2004) work is that the model response to all factors combined is to a good approximation equal to the sum of the responses to each factor taken individually. This means it is reasonable to talk about the temperature change due to individual aspects of the evolving man-made and natural influences on climate. The zeros on both plots are set equal to 1900 temperatures, and it is apparent that most of the 0.52 °C global warming between 1900 and 1994 should be attributed to a 0.69 °C temperature forcing from greenhouse gases partially offset by a 0.27 °C cooling due to man-made sulfate emissions and with other factors contributing the balance. This contrasts with the warming from 1900 to 1940 for which the model only attributes a net increases of 0.06 °C to the combined effects of greenhouse gases and sulfate emissions.
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Summary This figure, based on Meehl et al. (2004), shows the ability of a global climate model...
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|current||01:22, April 20, 2007||500 × 573 (32 KB)||Eric Wester||This figure, based on Meehl et al. (2004), shows the ability of a global climate model (the DOE PCM ) to reconstruct the historical temperature record and the degree to which the associated temperature changes can be decomposed into various forcing fac|