R
Raymond S. Bradley
Researcher at University of Massachusetts Amherst
Publications - 300
Citations - 37392
Raymond S. Bradley is an academic researcher from University of Massachusetts Amherst. The author has contributed to research in topics: Climate change & Holocene. The author has an hindex of 83, co-authored 296 publications receiving 34822 citations. Previous affiliations of Raymond S. Bradley include Pennsylvania State University & University of Glasgow.
Papers
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Journal ArticleDOI
Global Signatures and Dynamical Origins of the Little Ice Age and Medieval Climate Anomaly
Michael E. Mann,Zhihua Zhang,Scott Rutherford,Raymond S. Bradley,Malcolm K. Hughes,Drew Shindell,Caspar M. Ammann,Greg Faluvegi,Fenbiao Ni +8 more
TL;DR: The Medieval period is found to display warmth that matches or exceeds that of the past decade in some regions, but which falls well below recent levels globally, and the Little Ice Age is marked by a tendency for La Niña–like conditions in the tropical Pacific.
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Northern Hemisphere Temperatures During the Past Millennium: Inferences, Uncertainties, and Limitations
TL;DR: In this article, the authors attempt hemispheric temperature reconstructions with proxy data networks for the past millennium, focusing not just on the reconstructions, but the uncertainties therein, and important caveats.
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Global-scale temperature patterns and climate forcing over the past six centuries
TL;DR: In this article, a spatially resolved global reconstructions of annual surface temperature patterns over the past six centuries are based on the multivariate calibration of widely distributed high-resolution proxy climate indicators.
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Elevation-dependent warming in mountain regions of the world
Nick Pepin,Raymond S. Bradley,Henry F. Diaz,Michel Baraer,E. B. Caceres,Nathan Forsythe,Hayley J. Fowler,Gregory B. Greenwood,M. Z. Hashmi,Xiaodong Liu,James R. Miller,Liang Ning,A. Ohmura,Elisa Palazzi,Imtiaz Rangwala,Wolfgang Schöner,Igor Severskiy,Maria Shahgedanova,M. B. Wang,Scott N. Williamson,D. Q. Yang +20 more
TL;DR: In this paper, the authors review important mechanisms that contribute towards elevation-dependent warming, such as snow albedo and surface-based feedbacks, water vapour changes and latent heat release, surface water vapours and radiative flux changes, surface heat loss and temperature change; and aerosols.