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Boreal temperature variability inferred from maximum latewood density and tree-ring width data, Wrangell Mountain region, Alaska

Published online by Cambridge University Press:  20 January 2017

Nicole K. Davi ,
Gordon C. Jacoby  and
Gregory C. Wiles
Nicole K. Davi*
Affiliation:
Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA
Gordon C. Jacoby
Affiliation:
Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA
Gregory C. Wiles
Affiliation:
Department of Geology, The College of Wooster, Wooster, OH 44691, USA
*
*Corresponding author. Fax: +1-845-365-8152.E-mail address:[email protected] (N. K. Davi).
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Abstract

Variations in both width and density of annual rings from a network of tree chronologies were used to develop high-resolution proxies to extend the climate record in the Wrangell Mountain region of Alaska. We developed a warm-season (July–September) temperature reconstruction that spans A.D. 1593–1992 based on the first eigenvector from principal component analysis of six maximum latewood density (MXD) chronologies. The climate/tree-growth model accounts for 51% of the temperature variance from 1958 to 1992 and shows cold in the late 1600s–early 1700s followed by a warmer period, cooling in the late 1700s–early 1800s, and warming in the 20th century. The 20th century is the warmest of the past four centuries. Several severely cold warm-seasons coincide with major volcanic eruptions. The first eigenvector from a ring-width (RW) network, based on nine chronologies from the Wrangell Mountain region (A.D. 1550–1970), is correlated positively with both reconstructed and recorded Northern Hemisphere temperatures. RW shows a temporal history similar to that of MXD by increased growth (warmer) and decreased growth (cooler) intervals and trends. After around 1970 the RW series show a decrease in growth, while station data show continued warming, which may be related to increasing moisture stress or other factors. Both the temperature history based on MXD and the growth trends from the RW series are consistent with well-dated glacier fluctuations in the Wrangell Mountains and some of the temperature variations also correspond to variations in solar activity.

Keywords

PaleoclimateTree ringsMaximum latewood densityRing widthTemperatureBorealAlaska
Type
Research Article
Information
Quaternary Research , Volume 60 , Issue 3 , November 2003 , pp. 252 - 262
Copyright
University of Washington

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References

Barber, V.A., Juday, G.P., and Finney, B.P., (2000). Reduced growth of Alaskan white spruce in the twentieth century from temperature-induced drought stress. Nature 405, 668–673.CrossRefGoogle ScholarPubMed
Blasing, T.J., Duvick, D.N., and West, D.C., (1981). Calibration and verification using regionally averaged single station precipitation data. Tree-Ring Bulletin 41, 37–44.Google Scholar
Briffa, K.R., Jones, P.D., and Schweingruber, F.H., (1992). Tree-ring reconstructions of summer temperature patterns across western North America since 1600. Journal of Climate 5, 735–754.Google Scholar
Briffa, K., Schweingruber, F., Jones, P., Osborn, T., Shyatov, G., and Cook, E., (1998). Reduced sensitivity of recent tree growth to temperature at high northern latitudes. Nature 391, 678–682.Google Scholar
Chapman, W.L., and Walsh, J.E., (1993). Recent variation of sea ice and air temperature in high latitudes. Bulletin of the American Meteorological Society 74, 33–47.2.0.CO;2>CrossRefGoogle Scholar
Cook, E.R., (1985). A Time Series Analysis Approach to Tree-Ring Standardization. Univ. of Arizona, Tucson. [Ph.D. thesis] Google Scholar
Cook, E.R., and Kairiukstis, L., (1990). Methods of Dendrochronology. Applications in the Environmental Sciences. Kluwer, Dordrecht.Google Scholar
D'Arrigo, R.D., and Jacoby, G.C., (1999). Temperature changes after volcanic events. Climatic Change 41, 1–15.Google Scholar
D'Arrigo, R.D., Jacoby, G.C., Free, M., and Robock, A., (1999). Northern Hemisphere temperature variability for the past three centuries. tree-ring and model estimates. Climatic Change 42, 663–675.CrossRefGoogle Scholar
Dai, J., Mosely-Thomas, E., and Thompson, L.G., (1991). Ice core evidence for an explosive tropical volcanic eruption 6 years preceding Tambora. Journal of Geophysical Research 96, 17361–17366.Google Scholar
Denton, G.H., and Karlén, W., (1977). Holocene glacial and tree-line variations in the White River Valley and Skolai Pass, Alaska and Yukon Territory. Quaternary Research 7, 63–111.Google Scholar
Eddy, J., (1976). The Maunder Minimum. Science 192, 1189–1202.Google Scholar
Eddy, J., (1992). Before Tambora. the sun and the climate: 1790–1830. Harington, C. The Year Without a Summer? World Climate in 1816. Canadian Museum of Nature, Ottawa. 11 Google Scholar
Esper, J., Cook, E.R., and Schweingruber, F.H., (2002). Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science 295, 2250–2253.CrossRefGoogle ScholarPubMed
Fritts, H.C., (1976). Tree Rings and Climate. Academic Press, London.Google Scholar
Holmes, R.L., (1983). Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bulletin 44, 69–75.Google Scholar
Hosie, R.C., (1990). Native Trees of Canada. eighth ed Markham, Ontario.Google Scholar
Intergovernmental Panel on Climate Change (IPCC). (2001). Mc Carthy, J.J., Canziani, O.F., Leary, N.A., Dokken, D.J., White, K.S. (Eds.), Climate Change 2001: Impacts, Adaptations and Vulnerability—Contributions of Working Group II to the IPCC Third Assessment Report. Cambridge Univ. Press, Cambridge, UK.Google Scholar
Jacoby, G.C., and D'Arrigo, R.D., (1989). Reconstructed Northern Hemisphere annual temperatures since 1671 based on high-lattitude tree-ring data from North America. Climatic Change 14, 39–59.Google Scholar
Jacoby, G.C., and D'Arrigo, R., (1995). Tree-ring width and density evidence of climatic and potential forest change in Alaska. Global Biogeochemical Cycles 9, 227–234.Google Scholar
Jacoby, G.C., D'Arrigo, R.D., and Juday, G., (1999). Tree-ring indicators of climate change at northern latitudes. World Resource Review 11, 21–29.Google Scholar
Jacoby, G.C., Lovelius, N., Shumilov, O., Raspopov, O., Karbainov, J., and Frank, D., (2000). Long-term temperature trends and tree growth in the Taymir region of Northern Siberia. Quaternary Research 53, 312–318.Google Scholar
Jones, P.D., (1994). Hemispheric surface air temperature variations. a reanalysis and update to 1993. Journal of Climate 7, 1794–1802.2.0.CO;2>CrossRefGoogle Scholar
Jones, P.D., Briffa, K.R., and Schweingruber, F.H., (1995). Tree-ring evidence of the widespread effects of explosive volcanic eruptions. Geophysical Research Letters 22, 1333–1336.Google Scholar
Lenz, O., Schaer, E., and Schweingruber, F.H., (1976). Methodological problems relative to the measurement of the density and width of growth rings by X-ray densitograms of wood. Holzforschung 30, 114–123.Google Scholar
Lloyd, A.H., and Fastie, C.L., (2002). Spatial and temporal variability in the growth and climate response of treeline trees in Alaska. Climatic Change 52, 481–509.CrossRefGoogle Scholar
Luckman, B.H., Watson, E., Youngblut, D.K., (2002). Dendroclimatic reconstructions of precipitation and temperature patterns in British Columbia and the Yukon Territory. Final report to the Meteorological Service of Canada, Collaborative Research Agreement, (2001). –(2002). April 2002 Google Scholar
Mann, M., Bradley, R., and Hughes, M., (1999). Northern Hemisphere temperatures during the past millenium. inferences, uncertainties, and limitations. Geophysical Research Letters 26, 759–762.CrossRefGoogle Scholar
Maunder, E., (1922). The prolonged sunspot minimum 1675–1715. British Astronomical Association Journal 32, 140–145.Google Scholar
New, M., Hulme, M., and Jones, P.D., (2000). Representing twentieth century space–time climate variability. Part 2, Development of 1901–1996 monthly grids of terrestrial surface climate. Journal of Climate 13, 2217–2238.Google Scholar
Parker, M.L., and Jozsa, L.A., (1973). X-ray scanning machine for tree-ring width and density analysis. Wood and Fiber 5, 192–197.Google Scholar
Schweingruber, F.H., (1988). Tree Rings. Basics and Applications of Dendrochronology. D. Reidel, Dordrecht, The Netherlands. 276 Google Scholar
Schweingruber, F.H., Briffa, K.R., and Nogler, P., (1993). A tree-ring densitometric transect from Alaska to Labrador. comparison of ring-width and maximum-latewood-density chronologies in the conifer belt of northern North America. International Journal of Biometeorology 37, 151–169.Google Scholar
Serreze, M.C., Walsh, J.E., Chapin, F.S. III, Osterkamp, T., Dyurgerov, M., Romanovsky, V., Oechel, W.C., Morison, J., Zhang, T., and Barry, G., (2000). Observational evidence of recent change in the northern high-latitude environment. Climatic Change 46, 159–207.Google Scholar
Simkin, T., and Siebert, L., (1994). Volcanoes of the World. second ed Geoscience Press, Tucson.Google Scholar
Thetford, R.D., D'Arrigo, R.D., and Jacoby, G.C., (1991). An image analysis for determining densometric and ring width time series. Canadian Journal of Forest Research 21, 1544–1548.Google Scholar
Vaganov, E.A., Hughes, M.K., Kirdyanov, A.V., Schweingruber, F.H., and Silkin, P.P., (1999). Influence of snowfall and melt timing on tree growth in subarctic Eurasia. Nature 400, 149–151.Google Scholar
Viereck, L.A., and Little, E.L., (1972). Alaska Trees and Shrubs. Forest Service Agricultural Handbook 410 (70–176230). United States Department of Agriculture, Washington, DC.Google Scholar
Wigley, T.M., Briffa, K.R., and Jones, P.D., (1984). On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. Journal of Climate and Applied Meteorology 23, 201–213.Google Scholar
Wiles, G.C., D'Arrigo, R.D., and Jacoby, G.C., (1998). Gulf of Alaska atmospheric–ocean variability over recent centuries inferred from coastal tree-ring records. Climatic Change 38, 289–306.Google Scholar
Wiles, G.C., Jacoby, G.C., Davi, N.K., and McAllister, R.P., (2002). Late Holocene glacial fluctuations in the Wrangell Mountains, Alaska. Geological Society of America Bulletin 114, 896–908.Google Scholar
Wiles, G.C., McAllister, R.P., Davi, N.K., and Jacoby, G.C., (2003). Eolian response to Little Ice Age climate change, Tana Dunes, Chugach Mountains, Alaska, U.S.A. Arctic, Antarctic, and Alpine Research 35, 67–73.Google Scholar