Proceedings of the National Academy of Sciences · 2011 · 370 citations · 28 references
Climate SciencesClimatologyFuture Climatic ChangeEngineeringGlobal Surface TemperatureSolar InsolationGreenhouse EffectGeographyGlobal Warming PotentialGlobal WarmingInternal VariabilityGlobal ClimateClimate Change BiologyAnthropogenic Climate ChangeEarth ScienceEarth's ClimateClimate Change
Given the widely noted increase in the warming effects of rising greenhouse gas concentrations, it has been unclear why global surface temperatures did not rise between 1998 and 2008. We find that this hiatus in warming coincides with a period of little increase in the sum of anthropogenic and natural forcings. Declining solar insolation as part of a normal eleven-year cycle, and a cyclical change from an El Nino to a La Nina dominate our measure of anthropogenic effects because rapid growth in short-lived sulfur emissions partially offsets rising greenhouse gas concentrations. As such, we find that recent global temperature records are consistent with the existing understanding of the relationship among global surface temperature, internal variability, and radiative forcing, which includes anthropogenic factors with well known warming and cooling effects.
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Spurious regressions in econometrics
Clive W. J. Granger, Paul Newbold · Journal of Econometrics · 1974 · 6.1K citations
Climate Change: The IPCC Scientific Assessment.
John Bongaarts · Population and Development Review · 1992 · 3.1K citations