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An 1800-yr record of decadal-scale hydroclimatic variability in the upper Arkansas River basin from bristlecone pine

Published online by Cambridge University Press:  20 January 2017

Connie A. Woodhouse ,
Gregory T. Pederson  and
Stephen T. Gray
Connie A. Woodhouse*
Affiliation:
School of Geography and Development, University of Arizona, Tucson, AZ 85721, USA
Gregory T. Pederson
Affiliation:
U.S. Geological Survey, Northern Rocky Mountain Science Center, Bozeman, MT 59715, USA School of Natural Resources, University of Arizona, AZ 85721, USA
Stephen T. Gray
Affiliation:
Water Resources Data System, University of Wyoming, Laramie, WY 82071, USA Department of Civil and Architectural Engineering, University of Wyoming, Laramie, WY 82071, USA
*
⁎Corresponding author. The University of Arizona, School Geography and Development, 1103 E. 2nd Street, Room 409, Tucson, AZ 85721, USA. Fax: +1 520 621 2889.
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Abstract

Bristlecone pine trees are exceptionally long-lived, and with the incorporation of remnant material have been used to construct multi-millennial length ring–width chronologies. These chronologies can provide valuable information about past temperature and moisture variability. In this study, we outline a method to build a moisture-sensitive bristlecone chronology and assess the robustness and consistency of this sensitivity over the past 1200 yr using new reconstructions of Arkansas River flow (AD 1275–2002 and 1577–2002) and the summer Palmer Drought Sensitivity Index. The chronology, a composite built from parts of three collections in the central Rocky Mountains, is a proxy for decadal-scale moisture variability for the past 18 centuries. Since the sample size is small in some portions of the time series, the chronology should be considered preliminary; the timing and duration of drought events are likely the most robust characteristics. This chronology suggests that the region experienced increased aridity during the medieval period, as did much of western North America, but that the timing and duration of drought episodes within this period were somewhat different from those in other western locations, such as the upper Colorado River basin.

Keywords

PaleoclimatologyDendrochronologyDroughtBristlecone pineCentral Colorado
Type
Research Article
Information
Quaternary Research , Volume 75 , Issue 3 , May 2011 , pp. 483 - 490
Copyright
University of Washington

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