Most models that investigate increasing
greenhouse gas scenarios predict that the AMOC will slow down as a result of such forcing (Driesschaert et al., 2007; Hodell et al., 2009).
Most models that investigate increasing
greenhouse gas scenarios predict that the AMOC will slow down as a result of such forcing (Driesschaert et al., 2007; Meehl et al., 2007).
Not exact matches
«This is worrisome given that the temperature in the study region is
predicted to rise by as much as 2 degrees by midcentury under the range of plausible
greenhouse gas emissions
scenarios,» said Avery Cohn, aassistant professor of environment and resource policy at Tufts, who led the work while he was a visiting researcher at Brown.
Meehl and his colleagues used two sophisticated computer models of global climate to
predict what would happen under various
scenarios for
greenhouse gas emission controls, taking into account the oceanic time lag.
Models
predict that the same summertime temperatures that ranked among the top 5 % in 1950 — 1979 will occur at least 70 % of the time by 2035 — 2064 in the U.S. if global emissions of
greenhouse gases grow at a moderate rate (as modeled under the IPCC SRES A2
scenario).
The IPCC
predicts, as its central estimate, 1.5 K warming by 2100 because of the CO2 we add this century, with another 0.6 K for «already - committed» warming and 0.7 K for warming from non-CO2
greenhouse gases: total 2.8 K (the mean of the predictions on all six emissions
scenarios).
The map (above) shows
predicted changes in the annual number of days of extreme rainfall (defined as rainfall totals in excess of the historic 98th percentile) across the United States by 2041 - 2070 as compared to 1971 - 2000 if
greenhouse gases continue to increase at a high rate (A2
scenario).
A moderate - emission
scenario from the 2007 Intergovernmental Panel on Climate Change (IPCC) report
predicts that the continued addition of
greenhouse gases from fossil...
Meehl and his colleagues used two sophisticated computer models of global climate to
predict what would happen under various
scenarios for
greenhouse gas emission controls, taking into account the oceanic time lag.
In terms of atmospheric chemistry, a strong consensus was reached for the first time that science could
predict the changes in tropospheric ozone in response to
scenarios for CH4 and the indirect
greenhouse gases (CO, NOx, VOC) and that a quantitative GWP for CO could be reported.
Science writer Greg Laden wrote that the Duke study will receive «criticism from climate scientists» because it includes language that suggests it is assessing the likelihood of different warming
scenarios by
predicting the amount of
greenhouse gas emissions that will occur in the future, which it can't possibly know.