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'Tis the seasonal

Anthropogenic climate change has become clearly observable through many metrics. These include an increase in global annual temperatures, growing heat content of the oceans, and sea level rise owing to the melting of the polar ice sheets and glaciers. Now, Santer et al. report that a human-caused signal in the seasonal cycle of tropospheric temperature can also be measured (see the Perspective by Randel). They use satellite data and the anthropogenic “fingerprint” predicted by climate models to show the extent of the effects and discuss how these changes have been caused.
Science, this issue p. eaas8806; see also p. 227

Structured Abstract

INTRODUCTION

Fingerprint studies use pattern information to separate human and natural influences on climate. Most fingerprint research relies on patterns of climate change that are averaged over years or decades. Few studies probe shorter time scales. We consider here whether human influences are identifiable in the changing seasonal cycle. We focus on Earth’s troposphere, which extends from the surface to roughly 16 km at the tropics and 13 km at the poles. Our interest is in TAC, the geographical pattern of the amplitude of the annual cycle of tropospheric temperature. Information on how TAC has changed over time is available from satellite retrievals and from large multimodel ensembles of simulations.

RATIONALE

At least three lines of evidence suggest that human activities have affected the seasonal cycle. First, there are seasonal signals in certain human-caused external forcings, such as stratospheric ozone depletion and particulate pollution. Second, there is seasonality in some of the climate feedbacks triggered by external forcings. Third, there are widespread signals of seasonal changes in the distributions and abundances of plant and animal species. These biological signals are in part mediated by seasonal climate changes arising from global warming. All three lines of evidence provide scientific justification for performing fingerprint studies with the seasonal cycle.

RESULTS

The simulated response of the seasonal cycle to historical changes in human and natural factors has prominent mid-latitude increases in the amplitude of TAC. These features arise from larger mid-latitude warming in the summer hemisphere, which appears to be partly attributable to continental drying. Because of land-ocean differences in heat capacity and hemispheric asymmetry in land fraction, mid-latitude increases in TAC are greater in the Northern Hemisphere than in the Southern Hemisphere. Qualitatively similar large-scale patterns of annual cycle change occur in satellite tropospheric temperature data.
We applied a standard fingerprint method to determine (i) whether the pattern similarity between the model “human influence” fingerprint and satellite temperature data increases with time, and (ii) whether such an increase is significant relative to random changes in similarity between the fingerprint and patterns of natural internal variability. This method yields signal-to-noise (S/N) ratios as a function of increasing satellite record length. Fingerprint detection occurs when S/N exceeds and remains above the 1% significance threshold.
We find that the model fingerprint of externally forced seasonal cycle changes is identifiable with high statistical confidence in five out of six satellite temperature datasets. In these five datasets, S/N ratios for the 38-year satellite record vary from 2.7 to 5.8. Our positive fingerprint detection results are unaffected by the removal of all global mean information and by the exclusion of sea ice regions. On time scales for which meaningful tests are possible (one to two decades), there is no evidence that S/N ratios are spuriously inflated by a systematic model underestimate of the amplitude of observed tropospheric temperature variability.

CONCLUSION

Our results suggest that attribution studies with the seasonal cycle of tropospheric temperature provide powerful and novel evidence for a statistically significant human effect on Earth’s climate. We hope that this finding will stimulate more detailed exploration of the seasonal signals caused by anthropogenic forcing.
Trends in the amplitude of the annual cycle of tropospheric temperature.
Trends are calculated over 1979 to 2016 and are averages from a large multimodel ensemble of historical simulations. The most prominent features are pronounced mid-latitude increases in annual cycle amplitude (shown in red) in both hemispheres. Similar mid-latitude increases occur in satellite temperature data. Trends are superimposed on NASA’s “blue marble” image.

Abstract

We provide scientific evidence that a human-caused signal in the seasonal cycle of tropospheric temperature has emerged from the background noise of natural variability. Satellite data and the anthropogenic “fingerprint” predicted by climate models show common large-scale changes in geographical patterns of seasonal cycle amplitude. These common features include increases in amplitude at mid-latitudes in both hemispheres, amplitude decreases at high latitudes in the Southern Hemisphere, and small changes in the tropics. Simple physical mechanisms explain these features. The model fingerprint of seasonal cycle changes is identifiable with high statistical confidence in five out of six satellite temperature datasets. Our results suggest that attribution studies with the changing seasonal cycle provide powerful evidence for a significant human effect on Earth’s climate.
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Supplementary Material

Summary

Materials and Methods
Supplementary Text
Figs. S1 to S13
References (120127)

Resources

File (aas8806_santer_sm.pdf)

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Published In

Science
Volume 361 | Issue 6399
20 July 2018

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Received: 8 January 2018
Accepted: 7 June 2018
Published in print: 20 July 2018

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Acknowledgments

We acknowledge the World Climate Research Programme’s Working Group on Coupled Modelling, which is responsible for CMIP, and we thank the climate modeling groups for producing and making available their model output. For CMIP, the U.S. Department of Energy’s Program for Climate Model Diagnosis and Intercomparison (PCMDI) provided coordinating support and led development of software infrastructure in partnership with the Global Organization for Earth System Science Portals. We thank M. MacCracken (Climate Institute) and two reviewers for helpful comments. Funding: Work at LLNL was performed under the auspices of the U.S. Department of Energy under contract DE-AC52-07NA27344 through the Regional and Global Model Analysis Program (B.D.S., S.P.-C., M.D.Z., P.J.D., and J.P.) and the Early Career Research Program Award SCW1295 (I.C., C.B.). Additional support was provided by the LLNL-LDRD Program under project no. 13-ERD-032 (B.D.S., I.C., and C.B.); the Lee and Geraldine Martin Professorship at MIT (S.S.); NASA grant NNH12CF05C (F.J.W. and C.M.); and NASA grant NNX13AN49G (Q.F.). Author contributions: B.D.S., I.C., and C.B. conceived the study; B.D.S., S.P.-C., and I.C. performed statistical analyses; J.P. calculated synthetic satellite temperatures from model simulation output; C.M., F.J.W., and C.-Z.Z. provided satellite temperature data; and all authors contributed to the writing and revision of the manuscript. Competing interests: None. Data and materials availability: All primary satellite and model temperature datasets used here are publicly available. Derived products (synthetic satellite temperatures calculated from model simulations) are provided at https://pcmdi.llnl.gov/research/DandA/. Disclaimer: The views, opinions, and findings contained in this report are those of the authors and should not be construed as a position, policy, or decision of the U.S. Government, the U.S. Department of Energy, or the National Oceanic and Atmospheric Administration.

Authors

Affiliations

Program for Climate Model Diagnosis and Intercomparison (PCMDI), Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
Program for Climate Model Diagnosis and Intercomparison (PCMDI), Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
Mark D. Zelinka
Program for Climate Model Diagnosis and Intercomparison (PCMDI), Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
Program for Climate Model Diagnosis and Intercomparison (PCMDI), Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
Céline Bonfils
Program for Climate Model Diagnosis and Intercomparison (PCMDI), Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
Program for Climate Model Diagnosis and Intercomparison (PCMDI), Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
Qiang Fu
Department of Atmospheric Sciences, University of Washington, Seattle, WA 98195, USA.
Earth and Planetary Sciences, University of California, Santa Cruz, CA 95064, USA.
Remote Sensing Systems, Santa Rosa, CA 95401, USA.
Program for Climate Model Diagnosis and Intercomparison (PCMDI), Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
Program for Climate Model Diagnosis and Intercomparison (PCMDI), Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA.
Frank J. Wentz
Remote Sensing Systems, Santa Rosa, CA 95401, USA.
Center for Satellite Applications and Research, NOAA/NESDIS, College Park, MD 20740, USA.

Funding Information

U.S. Department of Energy: DE-AC52-07NA27344
U.S. Department of Energy: Early Career Research Program Award SCW1295
U.S. Department of Energy: DE-AC52-07NA27344
Lawrence Livermore National Lab LDRD Program: 13-ERD-032
M.I.T. Lee and Geraldine Martin Professorship:
Lawrence Livermore National Laboratory LDRD Program: 18-ERD-054

Notes

*Corresponding author. Email: [email protected]

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