Journal cover Journal topic
Advances in Statistical Climatology, Meteorology and Oceanography An international open-access journal on applied statistics
Adv. Stat. Clim. Meteorol. Oceanogr., 3, 33-53, 2017
https://doi.org/10.5194/ascmo-3-33-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
 
09 Jun 2017
Estimating trends in the global mean temperature record
Andrew Poppick1, Elisabeth J. Moyer2, and Michael L. Stein3 1Department of Mathematics and Statistics, Carleton College, Northfield, MN, USA
2Department of the Geophysical Sciences, University of Chicago, Chicago, IL, USA
3Department of Statistics, University of Chicago, Chicago, IL, USA
Abstract. Given uncertainties in physical theory and numerical climate simulations, the historical temperature record is often used as a source of empirical information about climate change. Many historical trend analyses appear to de-emphasize physical and statistical assumptions: examples include regression models that treat time rather than radiative forcing as the relevant covariate, and time series methods that account for internal variability in nonparametric rather than parametric ways. However, given a limited data record and the presence of internal variability, estimating radiatively forced temperature trends in the historical record necessarily requires some assumptions. Ostensibly empirical methods can also involve an inherent conflict in assumptions: they require data records that are short enough for naive trend models to be applicable, but long enough for long-timescale internal variability to be accounted for. In the context of global mean temperatures, empirical methods that appear to de-emphasize assumptions can therefore produce misleading inferences, because the trend over the twentieth century is complex and the scale of temporal correlation is long relative to the length of the data record. We illustrate here how a simple but physically motivated trend model can provide better-fitting and more broadly applicable trend estimates and can allow for a wider array of questions to be addressed. In particular, the model allows one to distinguish, within a single statistical framework, between uncertainties in the shorter-term vs. longer-term response to radiative forcing, with implications not only on historical trends but also on uncertainties in future projections. We also investigate the consequence on inferred uncertainties of the choice of a statistical description of internal variability. While nonparametric methods may seem to avoid making explicit assumptions, we demonstrate how even misspecified parametric statistical methods, if attuned to the important characteristics of internal variability, can result in more accurate uncertainty statements about trends.

Citation: Poppick, A., Moyer, E. J., and Stein, M. L.: Estimating trends in the global mean temperature record, Adv. Stat. Clim. Meteorol. Oceanogr., 3, 33-53, https://doi.org/10.5194/ascmo-3-33-2017, 2017.
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We show that ostensibly empirical methods of analyzing trends in the global mean temperature record, which appear to de-emphasize assumptions, can nevertheless produce misleading inferences about trends and associated uncertainty. We illustrate how a simple but physically motivated trend model can provide better-fitting and more broadly applicable results, and show the importance of adequately characterizing internal variability for estimating trend uncertainty.
We show that ostensibly empirical methods of analyzing trends in the global mean temperature...
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