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THE NATIONAL ACADEMIES PRESS ● 500 Fifth Street NW ⚫ Washington, DC 20001

NOTICE: The project that is the subject of this report was approved by the Governing Board of
the National Research Council, whose members are drawn from the councils of the National
Academy of Sciences, the National Academy of Engineering, and the Institute of Medicine. The
members of the committee responsible for the report were chosen for their special competences
and with regard for appropriate balance.

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THE NATIONAL ACADEMIES
Advisers to the Nation on Science, Engineering, and Medicine

The National Academy of Sciences is a private, nonprofit, self-perpetuating society of distinguished scholars
engaged in scientific and engineering research, dedicated to the furtherance of science and technology and to their
use for the general welfare. Upon the authority of the charter granted to it by the Congress in 1863, the Academy
has a mandate that requires it to advise the federal government on scientific and technical matters. Dr. Ralph J.
Cicerone is president of the National Academy of Sciences.

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Sciences, as a parallel organization of outstanding engineers. It is autonomous in its administration and in the
selection of its members, sharing with the National Academy of Sciences the responsibility for advising the federal
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needs, encourages education and research, and recognizes the superior achievements of engineers. Dr. Wm. A.
Wulf is president of the National Academy of Engineering.

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eminent members of appropriate professions in the examination of policy matters pertaining to the health of the
public. The Institute acts under the responsibility given to the National Academy of Sciences by its congressional
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research, and education. Dr. Harvey V. Fineberg is president of the Institute of Medicine.

The National Research Council was organized by the National Academy of Sciences in 1916 to associate the broad
community of science and technology with the Academy's purposes of furthering knowledge and advising the
federal government. Functioning in accordance with general policies determined by the Academy, the Council has
become the principal operating agency of both the National Academy of Sciences and the National Academy of
Engineering in providing services to the government, the public, and the scientific and engineering communities.
The Council is administered jointly by both Academies and the Institute of Medicine. Dr. Ralph J. Cicerone and Dr.
Wm. A. Wulf are chair and vice chair, respectively, of the National Research Council.

COMMITTEE ON SURFACE TEMPERATURE RECONSTRUCTIONS
FOR THE LAST 2,000 YEARS

GERALD R. NORTH (Chair), Texas A&M University, College Station

FRANCO BIONDI, University of Nevada, Reno

PETER BLOOMFIELD, North Carolina State University, Raleigh

JOHN R. CHRISTY, University of Alabama, Huntsville

KURT M. CUFFEY, University of California, Berkeley

ROBERT E. DICKINSON, Georgia Institute of Technology, Atlanta

ELLEN R.M. DRUFFEL, University of California, Irvine

DOUGLAS NYCHKA, National Center for Atmospheric Research, Boulder, Colorado BETTE OTTO-BLIESNER, National Center for Atmospheric Research, Boulder, Colorado

NEIL ROBERTS, University of Plymouth, United Kingdom

KARL K. TUREKIAN, Yale University, New Haven, Connecticut

JOHN M. WALLACE, University of Washington, Seattle

NRC Staff

IAN KRAUCUNAS, Study Director

CHRIS ELFRING, Board Director

AMANDA STAUDT, Senior Program Officer
ELIZABETH A. GALINIS, Research Associate

LEAH PROBST, Research Associate

DIANE GUSTAFSON, Administrative Coordinator
NORMAN GROSSBLATT, Senior Editor

BOARD ON ATMOSPHERIC SCIENCES AND CLIMATE

ROBERT J. SERAFIN (Chair), National Center for Atmospheric Research, Boulder, Colorado
M. JOAN ALEXANDER, NorthWest Research Associates/CORA, Boulder, Colorado
FREDERICK R. ANDERSON, McKenna Long & Aldridge LLP, Washington, D.C.
MICHAEL L. BENDER, Princeton University, New Jersey
ROSINA M. BIERBAUM, University of Michigan, Ann Arbor
MARY ANNE CARROLL, University of Michigan, Ann Arbor
CAROL ANNE CLAYSON, Florida State University, Tallahassee
WALTER F. DABBERDT, Vaisala Inc., Boulder, Colorado

KERRY A. EMANUEL, Massachusetts Institute of Technology, Cambridge
DENNIS L. HARTMANN, University of Washington, Seattle

PETER R. LEAVITT, Weather Information Inc., Newton, Massachusetts
JENNIFER A. LOGAN, Harvard University, Cambridge, Massachusetts

VERNON R. MORRIS, Howard University, Washington, D.C.

F. SHERWOOD ROWLAND, University of California, Irvine

THOMAS H. VONDER HAAR, Colorado State University/CIRA, Fort Collins

ROGER M. WAKIMOTO, National Center for Atmospheric Research, Boulder, Colorado

Ex Officio Members

ANTONIO J. BUSALACCHI, JR., University of Maryland, College Park

ERIC F. WOOD, Princeton University, New Jersey

NRC Staff

CHRIS ELFRING, Director

PAUL CUTLER, Senior Program Officer

AMANDA STAUDT, Senior Program Officer
MARIA UHLE, Program Officer

IAN KRAUCUNAS, Associate Program Officer
CLAUDIA MENGELT, Associate Program Officer
ELIZABETH A. GALINIS, Research Associate
LEAH PROBST, Research Associate

ROB GREENWAY, Senior Program Assistant
DIANE GUSTAFSON, Administrative Coordinator
ANDREAS SOHRE, Financial Associate

Foreword

Our understanding of climate and how it has varied over time are advancing rapidly as new data are acquired and new investigative instruments and methods are employed. Thus in 2005, I suggested to the U. S. Congress that the National Research Council (NRC) could help to answer questions about the data and methods that have been used in constructing records of Earth's surface temperatures from times when there were no scientific instruments, using proxy indicators. How has temperature varied over the last 2,000 years? How certain is the answer to this question?

Subsequently, this study was requested by Representative Sherwood Boehlert, Chairman of the Committee on Science, U.S. House of Representatives. Chairman Boehlert asked for a clear and concise report in a relatively short period of time, and the NRC agreed to undertake the study quickly. An ad hoc committee was formed, with the group carefully composed to include the breadth and depth of expertise and perspectives needed to analyze all aspects of how surface temperatures are estimated and interpreted, and to comment generally on climate science. The NRC asked the committee to summarize current scientific information on the temperature record for the past two millennia, describe the main areas of uncertainty and how significant they are, describe the principal methodologies used and any problems with these approaches, and explain how central is the debate over the paleoclimate temperature record to the state of scientific knowledge on global climate change.

The committee has prepared a report that, in my view, provides policy makers and the scientific community with a critical view of surface temperature reconstructions and how they are evolving over time, as well as a good sense of how important our understanding of the paleoclimate temperature record is within the overall state of scientific knowledge on global climate change. The report does not make policy recommendations.

I thank the members of the committee, who worked intensely to produce this careful report in a short period of time and contributed much personal time, insight, and energy. The NRC staff, and all those who contributed papers, data, graphics, and other information, as well as the independent experts who participated in the rigorous review process, were essential participants.

Ralph J. Cicerone, President National Academy of Sciences Chair, National Research Council

Preface

This committee was asked to describe and assess the state of scientific efforts to reconstruct surface temperature records for the Earth over approximately the last 2,000 years. (The full Statement of Task appears in Appendix A.) Normally, a technical issue such as surface temperature reconstructions might not generate widespread attention, but this case brings interesting lessons about how science works and how science, especially climate science, is communicated to policy makers and the public. The debate began in 1998 when a paper by Michael Mann, Raymond Bradley and Malcolm Hughes was published in the journal Nature. The authors used a new methodology to combine data from a number of sources to estimate temperatures in the Northern Hemisphere for the last six centuries, and later for the last 1,000 years. This research received wide attention, in part because it was illustrated with a simple graphic, the so-called hockey stick curve, that many interpreted as definitive evidence of anthropogenic causes of recent climate change. The research was given prominence in the 2001 report of the Intergovernmental Panel on Climate Change, and then picked up by many in the wider science community and by the popular media.

Science is a process of exploration of ideas-hypotheses are proposed and research is conducted to investigate. Other scientists work on the issue, producing supporting or negating evidence, and each hypothesis either survives for another round, evolves into other ideas, or is proven false and rejected. In the case of the hockey stick, the scientific process has proceeded for the last few years with many researchers testing and debating the results. Critics of the original papers have argued that the statistical methods were flawed, that the choice of data was biased, and that the data and procedures used were not shared so others could verify the work. This report is an opportunity to examine the strengths and limitations of surface temperature reconstructions and the role that they play in improving our understanding of climate. The reconstruction produced by Dr. Mann and his colleagues was just one step in a long process of research, and it is not (as sometimes presented) a clinching argument for anthropogenic global warming, but rather one of many independent lines of research on global climate change.

Using multiple types of proxy data to infer temperature time series over large geographic regions is a relatively new area of scientific research, although it builds upon the considerable progress that has been made in deducing past temperature variations at single sites and local regions. Surface temperature reconstructions often combine data from a number of specialized disciplines, and few individuals have expertise in all aspects of the work. The procedures for dealing with these data are evolving—there is no one "right" way to proceed. It is my opinion that this field is progressing in a healthy manner. As in all scientific endeavors, research reported in the scientific literature is often "work in progress" aimed at other investigators, not always to be taken as individual calls for action in the policy community.

With this as context, the committee considered the voluminous literature pertinent to its charge and received briefings and written contributions from more than two dozen people. We have organized our report knowing that we have at least two different audiences-the science community and the policy community. The principal conclusions of the committee are listed in the Summary and explained in the Overview using nontechnical language. More extensive

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