Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/105518
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Type: Journal article
Title: Temperatures in transient climates: improved methods for simulations with evolving temporal covariances
Author: Poppick, A.
McInerney, D.
Moyer, E.
Stein, M.
Citation: Annals of Applied Statistics, 2016; 10(1):477-505
Publisher: The Institute of Mathematical Statistics
Issue Date: 2016
ISSN: 1932-6157
1941-7330
Statement of
Responsibility: 
Andrew Poppick, David J. McInerney, Elisabeth J. Moyer and Michael L. Stein
Abstract: Future climate change impacts depend on temperatures not only through changes in their means but also through changes in their variability. General circulation models (GCMs) predict changes in both means and variability; however, GCM output should not be used directly as simulations for impacts assessments because GCMs do not fully reproduce present-day temperature distributions. This paper addresses an ensuing need for simulations of future temperatures that combine both the observational record and GCM projections of changes in means and temporal covariances. Our perspective is that such simulations should be based on transforming observations to account for GCM projected changes, in contrast to methods that transform GCM output to account for discrepancies with observations. Our methodology is designed for simulating transient (nonstationary) climates, which are evolving in response to changes in CO2 concentrations (as is the Earth at present). This work builds on previously described methods for simulating equilibrium (stationary) climates. Since the proposed simulation relies on GCM projected changes in covariance, we describe a statistical model for the evolution of temporal covariances in a GCM under future forcing scenarios, and apply this model to an ensemble of runs from one GCM, CCSM3. We find that, at least in CCSM3, changes in the local covariance structure can be explained as a function of the regional mean change in temperature and the rate of change of warming. This feature means that the statistical model can be used to emulate the evolving covariance structure of GCM temperatures under scenarios for which the GCM has not been run. When combined with an emulator for mean temperature, our methodology can simulate evolving temperatures under such scenarios, in a way that accounts for projections of changes while still retaining fidelity with the observational record. The emulator for variability changes is also of interest on its own as a summary of GCM projections of variability changes.
Keywords: Climate change; climate variability; transient climate; observation-driven simulation; nonstationary processes; evolutionary spectrum
Rights: Copyright Status Unknown
RMID: 0030047934
DOI: 10.1214/16-AOAS903
Appears in Collections:Civil and Environmental Engineering publications

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