Global Signatures and Dynamical Origins of the Little Ice Age and Medieval Climate Anomaly

Author:

Mann Michael E.1,Zhang Zhihua1,Rutherford Scott2,Bradley Raymond S.3,Hughes Malcolm K.4,Shindell Drew5,Ammann Caspar6,Faluvegi Greg5,Ni Fenbiao4

Affiliation:

1. Department of Meteorology and Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA 16802, USA.

2. Department of Environmental Science, Roger Williams University, Bristol, RI 02809, USA.

3. Department of Geosciences, University of Massachusetts, Amherst, MA 01003–9298, USA.

4. Laboratory of Tree-Ring Research, University of Arizona, Tucson, AZ 85721, USA.

5. NASA Goddard Institute for Space Studies, New York, NY 10025, USA.

6. Climate Global Dynamics Division, National Center for Atmospheric Research, Boulder, CO 80305, USA.

Abstract

Patterns of Change The global climate record of the past 1500 years shows two long intervals of anomalous temperatures before the obvious anthropogenic warming of the 20th century: the warm Medieval Climate Anomaly between roughly 950 and 1250 A.D. and the Little Ice Age between around 1400 and 1700 A.D. It has become increasingly clear in recent years, however, that climate changes inevitably involve a complex pattern of regional changes, whose inhomogeneities contain valuable insights into the mechanisms that cause them. Mann et al. (p. 1256 ) analyzed proxy records of climate since 500 A.D. and compared their global patterns with model reconstructions. The results identify the large-scale processes—like El Niño and the North Atlantic Oscillation—that can account for the observations and suggest that dynamic responses to variable radiative forcing were their primary causes.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference29 articles.

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4. Low-frequency temperature variations from a northern tree ring density network

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