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From
•>>July 2002 Professor Michael E. Mann
answers a few questions about about this month's fast moving
front in Geosciences. Field:
Geosciences
Title: "Global-scale temperature patterns and climate forcing over the past six centuries"
Authors: Mann,
ME;Bradley, RS;Hughes, MK
Journal: NATURE, 392: (6678) 779-787 APR 23 1998
Addresses: Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA.
Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA.
Univ Arizona, Tree Ring Res Lab, Tucson, AZ 85721 USA.
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Why do you think your paper is highly cited?
I believe our '98 Nature article is highly cited because it
establishes a new line of evidence, independent of the predictions of
theoretical climate models, for the assertion that human beings are
responsible in large part for 20th century global warming.
Does it describe a new discovery or new methodology that's useful to
others?
Our paper presented a novel multivariate statistical approach for
assimilating the information contained in disparate "proxy"
indicators of past climate change (natural archives such as tree
rings, corals, and ice cores, which by their very nature record past
climate changes at the annual timescale). Our methodology allowed this
information to be synthesized and compared to modern instrumental
climate records, allowing us to reconstruct large-scale patterns of
surface temperature changes in the past, and, importantly, providing
an estimate of the uncertainties inherent in the reconstructions.
Could you summarize the significance of your paper in layman's
terms?
Our paper established that the large-scale global warming which
took place in the latter part of the 20th century is unprecedented
over a fairly long period of geological time. The now oft-cited
assertion that "the 1990s are the warmest decade of at least the
past 1000 years" is attributable to our '98 Nature article
(which established the result for the last 600 years) along with an
extension of our work (which extended this conclusion to the past 1000
years) which we published in the journal "Geophysical Research
Letters" in 1999. Our Nature article established that
the warmth of the 1990s was outside the range of variability as
indicated in our reconstruction of past Northern Hemisphere
temperature variations, taking the uncertainties in the reconstruction
into account. The paper also showed, from a statistical point of view,
that the recent warming could not be explained in terms of
"natural" influences (such as changes in solar output or
explosive volcanic activity), but could only be explained in terms of
anthropogenic factors (specifically, the increase of greenhouse gas
concentrations due to modern industrial activity).
How did you become involved in this research?
My Ph.D. dissertation (Department of Geology & Geophysics,
Yale University) involved the development of statistical
techniques for detecting "signals" in climate data. This
work was limited to an analysis of the instrumental record, which only
provides widespread spatial coverage over the globe for roughly the
past century. My interest in extending such analyses to longer
timescales inevitably led me to seek other sources of climate
information, namely, "proxy" climate data sources of the
sort discussed above. As I began to seek out scientists with expertise
in this area to collaborate with in this undertaking, I had the good
fortune to meet up with two top-notch paleoclimatogists in particular:
Professor Raymond Bradley at the University of Massachusetts,
and Professor Malcolm Hughes at the University of Arizona.
Supported by a postdoctoral fellowship from the Department of
Energy, and a grant from the National Science Foundation
"Earth Systems Research" program, I collaborated with
Bradley and Hughes on the scientific problem of reconstructing past
climate changes from "proxy" climate data, for my
postdoctoral research.
Professor Michael E. Mann,
Department of Environmental Sciences,
Clark Hall, University of Virginia,
Charlottesville, VA 22903
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