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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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References

Biondi, F., and Waikul, K. DENDROCLIM2002: a C++ program for statistical calibration of climate signals in tree-ring chronologies. Computers and Geosciences 30, (2004). 303–311.Google Scholar
Brunstein, F.C., and Yamaguchi, D.K. The oldest known Rocky Mountain bristlecone pines (Pinus aristata Engelm.). Arctic and Alpine Research 24, (1992). 252–256.Google Scholar
Cook, E.R., and Peters, K. Calculating unbiased tree-ring indices for the study of climatic and environmental change. Holocene 7, (1997). 361–370.Google Scholar
Cook, E.R., Briffa, K.R., Meko, D.M., Graybill, D.S., and Funkhouser, G. The ‘segment length curse’ in long tree-ring chronology development for paleoclimatic studies. Holocene 5, (1995). 229–237.Google Scholar
Cook, E.R., Woodhouse, C.A., Eakin, C.M., Meko, D.M., and Stahle, D.W. Long-term aridity changes in the western United States. Science 306, (2004). 1015–1018.Google Scholar
Cook, E.R., Seager, R., Heim, R.R., Vose, R.S., Herweijer, C., and Woodhouse, C.A. Megadroughts in North America: placing IPCC projections of hydroclimatic change in a long term paleoclimate context. Journal of Quaternary Science 25, (2009). 48–61. http://dx.doi.org/10.1002/jqs.1303CrossRefGoogle Scholar
Daly, C., Gibson, W.P., Taylor, G.H., Johnson, G.L., and Pasteris, P. A knowledge-based approach to the statistical mapping of climate. Climate Research 22, (2002). 99–113.Google Scholar
Dean, J.S., Euler, R.C., Gumerman, G.J., Plog, F.R., Hevly, R.H., and Karlstrom, T.N.V. Human behavior, demography, and paleoenvironment on the Colorado Plateau. American Antiquities 50, (1985). 537–554.Google Scholar
Euler, R.C., Gumerman, G.J., Karlstrom, T.N.V., Dean, J.S., and Hevly, R.H. The Colorado Plateaus: cultural dynamics and paleoenvironments. Science 205, (1979). 1089–1100.Google Scholar
Feng, S., Oglesby, R.J., Rowe, C.M., Loope, D.B., and Hu, Q. Atlantic and Pacific SST influences on Medieval drought in North America simulated by the Community Atmospheric Model. Journal of Geophysical Research 113, (2008). D11101 http://dx.doi.org/10.1029/2007JD009347Google Scholar
Fritts, H.C., Guiot, J., and Gordon, G.A. Verification. Cook, E.R., and Kairiukstis, L.A. Methods of Dendrochronology, Applications in the Environmental Sciences. (1990). Kluwer Academic Publishers, Dordrecht. 178–185.Google Scholar
Graham, N.E., Hughes, M.K., Ammann, C.M., Cobb, K.C., Hoerling, M.P., Kennett, D.J., Kennett, J.P., Rein, B., Stott, L., Wigand, P.E., and Xu, T. Tropical Pacific–mid latitude teleconnections in medieval times. Climatic Change 83, (2007). 241–285.Google Scholar
Gray, S.T., Betancourt, J.L., Fastie, C.L., and Jackson, S.T. Patterns and sources of multidecadal oscillations in drought-sensitive tree-ring records from the central and southern Rocky Mountains. Geophysical Research Letters 30, (2003). 491–494. http://dx.doi.org/10.1029/2002GL016154Google Scholar
Gray, S.T., Fastie, C., Jackson, S.T., and Betancourt, J.L. Tree-ring based reconstructions of precipitation in the Bighorn Basin, Wyoming since A.D. 1260. Journal of Climate 17, (2004). 3855–3865.Google Scholar
Gray, S.T., Jackson, S.T., and Betancourt, J.L. Tree-ring based reconstructions of interannual to decadal-scale precipitation variability for northeastern Utah. Journal of the American Water Resources Association 40, (2004). 947–960.Google Scholar
Gray, S.T., Graumlich, L.J., and Betancourt, J.L. Annual precipitation in the Yellowstone National Park Region since A.D. 1173. Quaternary Research 68, (2007). 18–27.Google Scholar
Grissino-Mayer, H.D. A 2129-year reconstruction of precipitation for northwestern New Mexico, U.S.A.. Dean, J.S., Meko, D.M., and Swetnam, T.W. Tree Rings, Environment, and Humanity, Radiocarbon. (1996). 191–204.Google Scholar
Hughes, M.K., and Brown, P.M. Drought frequency in central California since 101 B.C. recorded in giant sequoia tree rings. Climate Dynamics 6, (1992). 161–167.Google Scholar
Hughes, M.K., and Graumlich, L.J. Climatic variations and forcing mechanisms of the last 2000 years. Multi-millennial dendroclimatic studies from the western United States. NATO ASI Series vol. 141, (1996). 109–124.Google Scholar
Kipfmueller, K.F., and Salzer, M.W. Linear trend and climate response of five-needle pines in the western United States related to treeline proximity. Canadian Journal of Forest Research 40, (2010). 134–142.Google Scholar
Laird, K.R., Fritz, S.C., Maasch, K.A., and Cumming, B.F. Greater drought intensity and frequency before A.D. 1200 in the northern Great Plains, U.S.A.. Nature 384, (1996). 552–554.Google Scholar
Laird, K.R., Fritz, S.C., and Cumming, B.F. A diatom-based reconstruction of drought intensity, duration, and frequency from Moon Lake, North Dakota: a sub-decadal record of the last 2300 years. Journal of Paleolimnology 19, (1998). 161–179.CrossRefGoogle Scholar
LaMarche, V.C. Jr. Environment in relation to the age of bristlecone pines. Ecology 50, (1969). 53–59.CrossRefGoogle Scholar
Meko, D.M., Stockton, C.W., and Boggess, W.R. The tree-ring record of severe sustained drought. Water Resources Bulletin 31, (1995). 789–801.Google Scholar
Meko, D.M., Therrell, M.D., Baisan, C.H., and Hughes, M.K. Sacramento River flow — reconstructed to A.D. 869 from tree rings. Journal of the American Water Resources Association 37, (2001). 1029–1040.CrossRefGoogle Scholar
Meko, D.M., Woodhouse, C.A., Baisan, C.A., Knight, T., Lukas, J.L., Hughes, M.K., and Salzer, M.W. Medieval drought in the upper Colorado River Basin. Geophysical Research Letters 34, (2007). L10705 Google Scholar
Michaelsen, J. Cross-validation in statistical climate forecast models. Journal of Climate and Applied Meteorology 26, (1987). 1589–1600.Google Scholar
Mock, C.J. Climatic controls and spatial variations of precipitation in the western United States. Journal of Climate 9, (1996). 1111–1125.2.0.CO;2>CrossRefGoogle Scholar
National Academies of Science Colorado River Basin Water Management: Evaluating and Adjusting to Hydroclimatic Variability. Committee on the Scientific Bases of Colorado River Basin Water Management, National Research Council. (2007). The National Academies Press, Washington DC.Google Scholar
NOAA National Climate Data Center Median COFECHA Chronology Statistics by Species. http://www.ncdc.noaa.gov/paleo/treering/cofecha/speciesdata.html (2009). accessed 03/31/10 Google Scholar
Pederson, G.T., Gray, S.T., Fagre, D.B., and Graumlich, L.J. Long-duration drought variability and impacts on ecosystem services: a case study from Glacier National Park, Montana. Earth Interactions 10, (2006). 1–28.Google Scholar
>Salida Mail http://salida.com/history/ranching.htm Ranching and Agriculture of Chaffee County. (1929). accessed 03/31/10. Salida+Mail+http://salida.com/history/ranching.htm+Ranching+and+Agriculture+of+Chaffee+County.+(1929).+accessed+03/31/10.>Google Scholar
Salzer, M.W., and Kipfmueller, K.F. Reconstructed temperature and precipitation on a millennial timescale from tree rings in the southern Colorado Plateau, USA. Climatic Change 70, (2005). 465–487.Google Scholar
Salzer, M.W., Hughes, M.K., Bunn, A.G., and Kipfmueller, K.F. Recent unprecedented tree-ring growth in bristlecone pine at the highest elevations and possible causes. Proceedings of the National Academy of Sciences 106, (2009). 20348–20353. http://dx.doi.org/10.1073/pnas.0903029106Google Scholar
Schulman, E. Dendroclimatic Changes in Semiarid America. (1956). University of Arizona Press, Tucson, AZ. 142 pp.Google Scholar
Schulman, E. Bristlecone pine, oldest known living thing. National Geographic Magazine 113, (1958). 354–372.Google Scholar
Stahle, D.W., Cook, E.R., Cleaveland, M.K., Therrell, M.D., Meko, D.M., Grissino-Mayer, H.D., Watson, E., and Luckman, B.H. Tree-ring data document 16th century megadrought over North America. EOS. Transactions of the American Geophysical Union 81, (2000). 121 Google Scholar
Stahle, D.W., Fye, F.K., Cook, E.R., and Griffin, R.D. Tree-ring reconstructed megadroughts over North America since AD 1300. Climatic Change 83, (2007). 133–149.Google Scholar
Stockton, C.W. Long Term Streamflow Records Reconstructed from Tree-Rings. (1975). University of Arizona Press, Tucson.Google Scholar
Watson, E., and Luckman, B.H. Tree-ring based reconstructions of precipitation for the Southern Canadian Cordillera. Climatic Change 65, (2004). 209–241.Google Scholar
Watson, T.A., Barnett, F.A., Gray, S.T., and Tootle, G.A. Reconstructed stream flows for the headwaters of the Wind River, Wyoming, USA. Journal of the American Water Resources Association 45, (2009). 224–236.Google Scholar
WestMap http://www.cefa.dri.edu/Westmap/(2010). accessed 03/31/10. Google Scholar
Woodhouse, C.A., and Brown, P.M. Tree-ring evidence for Great Plains drought. Tree-Ring Research 57, (2001). 89–103.Google Scholar
Woodhouse, C.A., and Lukas, J.J. Multi-century tree-ring reconstructions of Colorado streamflow for water resource planning. Climatic Change 78, (2006). 293–315.Google Scholar
Woodhouse, C.A., and Overpeck, J.T. 2000 years of drought variability in the central United States. Bulletin of the American Meteorological Society 79, (1998). 2693–2714.Google Scholar
Woodhouse, C.A., Gray, S.T., and Meko, D.M. Updated streamflow reconstructions for the upper Colorado River Basin. Water Resources Research 42, (2006). W05415 http://dx.doi.org/10.1029/2005WR004455CrossRefGoogle Scholar