Hostname: page-component-cd9895bd7-p9bg8 Total loading time: 0 Render date: 2024-12-23T18:15:42.648Z Has data issue: false hasContentIssue false

Reconstructed summer temperature in the northern Rocky Mountains wilderness, USA

Published online by Cambridge University Press:  20 January 2017

Kurt F. Kipfmueller*
Affiliation:
Department of Geography, University of Minnesota, Minneapolis, MN, 55455, USA
*
*Fax: +1 612 624 1044 E-mail address:[email protected]

Abstract

Ring widths from whitebark pine (Pinus albicaulis Englem.) and subalpine larch (Larix lyallii Parl.) collected at three high-elevation sites were used to develop tree-growth chronologies to reconstruct summer temperature anomalies. A step-wise multiple regression procedure was used to screen potential predictor variables to generate a transfer function capable of skillfully reconstructing summer temperature. The resulting regression model explained approximately 38% of the adjusted variance in the instrumental temperature record. The fidelity of the reconstruction was verified using product mean and sign tests, both of which suggested significant predictive power in the reconstructions (p<0.05). Reduction of error (RE) and coefficient of efficiency (CE) measures were both positive, indicating the reconstruction contained useful climate information. Cool periods often coincided with reduced solar activity and/or periods of increased volcanic activity. Differences between this reconstruction and others encompassing a broader geographic scale highlight the importance of developing local reconstructions of climate variability, particularly when used in conjunction with ecological data sets that describe the occurrence of fires or insect epidemics. Mixed and divergent climate-response relationships were evident in the whitebark pine chronologies and suggest subalpine larch may be a more useful species than whitebark pine to target for the development of temperature reconstructions in this region.

Type
Original Articles
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Arno, S.F., Habeck, J.R., (1972). Ecology of alpine larch (Larix lyallii Parl.) in the Pacific Northwest.. Ecological Monographs 42, 417450.Google Scholar
Barber, V., Juday, G., Finney, B., (2000). Reduced growth of Alaska white spruce in the twentieth century from temperature-induced drought stress.. Nature, 405, 668672.CrossRefGoogle Scholar
Biondi, F., Perkins, D.L., Cayan, D.R., Hughes, M.K., (1999). July temperature during the second millennium reconstructed from Idaho tree-rings.. Geophysical Research Letters 26, 14451448. Data archived at the World Data Center for Paleoclimatology Boulder, Colorado, USA.CrossRefGoogle Scholar
Briffa, K.R., (2000). Annual climate variability in the Holocene: interpreting the message of ancient trees.. Quaternary Science Reviews 19, 87105.Google Scholar
Briffa, K.R., Jones, P.D., (1992). Basic chronology statistics and assessment.. Cook, E.R., Kairiukstis, L.A. Methods of Dendrochronology Kluwer Academic Publishers, Boston., pp. 137152.Google Scholar
Briffa, K.R., Jones, P.D., Schweingruber, F.H., (1992). Tree-ring density reconstructions of summer temperature patterns across western North America since 1600.. Journal of Climate 5, 735754. Data archived at the World Data Center for Paleoclimatology Boulder, Colorado, USA.2.0.CO;2>CrossRefGoogle Scholar
Briffa, K.R., Jones, P.D., Schweingruber, F.H., Karlén, W., Shiyatov, S.G., (1996). Tree-ring variables as proxy-climate indicators: problems with low-frequency signals.. Jones, P.D., Bradley, R.S., Jouzel, J. Climate Variations and Forcing Mechanisms of the last 2000 years Springer-Verlag, Berlin., pp. 941.Google Scholar
Briffa, K.R., Jones, P.D., Schweingruber, F.H., Osborn, T.J., (1998a). Influence of volcanic eruptions on Northern Hemisphere summer temperature over the past 600 years.. Nature 393, 450455.CrossRefGoogle Scholar
Briffa, K.R., Schweingruber, F.H., Jones, P.D., Osborn, T.J., Shiyatov, S.G., Vaganov, E.A., (1998b). Reduced sensitivity of recent tree-growth to temperature at high northern latitudes.. Nature 391, 678681.CrossRefGoogle Scholar
Briffa, K.R., Schweingruber, F.H., Jones, P.D., Osborn, T.J., Harris, I.C., Shiyatov, S.G., Vaganov, E.A., Grudd, H., (1998c). Trees tell of past climates: but are they speaking less clearly today? Philosophical Transactions of the Royal Society of London B 353, 6573.Google Scholar
Briffa, K.R., Osborn, T.J., Schweingruber, F.H., Harris, I.C., Jones, P.D., Shiyatov, S.G., Vaganov, E.A., (2001). Low-frequency temperature variations from a northern tree ring density network.. Journal of Geophysical Research 106, 29292941.Google Scholar
Brohan, P., Kennedy, J.J., Harris, I., Tett, S.F.B., Jones, P.D., (2006). Uncertainty estimates in regional and global observed temperature changes: a new dataset from 1850.. Journal Geophysical Research 111, D12106.Google Scholar
Brunelle-Daines, A., (2002). (2002). Holocene changes in fire, climate, and vegetation in the Northern Rocky Mountains of Idaho and Western Montana. Unpublished Ph.D. Dissertation, University of Oregon.Google Scholar
Carrer, M., Nola, P., Eduard, J.L., Motta, R., Urbinati, C., (2007). Regional variability of climate-growth relationships in Pinus cembra high elevation forests in the Alps.. Journal of Ecology 95, 10721083.CrossRefGoogle Scholar
Ciesla, W.M., Furniss, M.M., (1975). Idaho's haunted forest.. American Forests 81, 3235.Google Scholar
Colenutt, M.E., Luckman, B.H., (1991). Dendrochronological investigation of Larix lyallii at Larch Valley, Alberta.. Canadian Journal of Forest Research 21, 12221233.Google Scholar
Colenutt, M.E., Luckman, B.H., (1995). The dendrochronological characteristics of alpine larch.. Canadian Journal of Forest Research 25, 777789.CrossRefGoogle Scholar
Cook, E.R., (1985). A time series approach to tree ring standardization.. Unpublished Ph.D. Dissertation, The University of Arizona.Google Scholar
Cook, E.R., Peters, K., (1981). The smoothing spline: a new approach to standardizing forest interior tree-ring width series for dendroclimatic studies.. Tree-Ring Bulletin 41, 4553.Google Scholar
Cook, E.R., Krusic, P.J., (2004). The North American Drought Atlas. Lamont-Doherty Earth Observatory and the National Science Foundation..Google Scholar
Cook, E.R., Shiyatov, S., Mazepa, V., (1992a). Estimation of the mean chronology.. Cook, E.R., Kairiukstis, L.A. Methods of Dendrochronology Kluwer Academic Publishers, Boston., pp. 123132.Google Scholar
Cook, E.R., Shiyatov, S., Mazepa, V., (1992b). Tree-ring standardization and growth-trend estimation.. Cook, E.R., Kairiukstis, L.A. Methods of Dendrochronology Kluwer Academic Publishers, Boston., pp. 104123.Google Scholar
Cook, E.R., Briffa, K.R., Jones, P.D., (1994). Spatial regression methods in dendroclimatology: A review and comparison of two techniques.. International Journal of Climatology 14, 379402.CrossRefGoogle Scholar
Cook, E.R., Meko, D.M., Stahle, D.W., Cleaveland, M.K., (1999). Drought reconstructions for the Continental United States.. Journal of Climate 12, 11451162.Google Scholar
Crowley, T.J., (2000). Causes of climate change over the past 1000 years.. Science 289, 270277. Data archived at the World Data Center for Paleoclimatology, Boulder, Colorado, USA.Google Scholar
D'Arrigo, R.D., Jacoby, G.C., (1999). Northern North American tree-ring evidence for regional temperature changes after major volcanic events.. Climatic Change 41, 115.Google Scholar
D'Arrigo, R.D., Kaufmann, R.K., Davi, N., Jacoby, G.C., Laskowski, C., Myneni, R.B., Cherubini, P., (2004). Thresholds for warming-induced growth decline at elevational tree line in the Yukon Territory, Canada.. Biogeochemical Cycles 18, GB3021 doi:10.1029/2004GB002249.Google Scholar
D'Arrigo, R.D., Wilson, R., Jacoby, G.C., (2006). On the long-term context for late twentieth century warming.. Journal of Geophysical Research Letters 111, D03103 doi:10.1029/2005JD006352. Data archived at the World Data Center for Paleoclimatology, Boulder, Colorado, USA.Google Scholar
Esper, J., Cook, E.R., Schweingruber, F.H., (2002). Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability.. Science 295, 22502253. Data archived at the World Data Center for Paleoclimatology, Boulder, Colorado, USA.CrossRefGoogle ScholarPubMed
Evenden, J.C., (1944). Montana's thirty-year mountain pine beetle infestation.. Unpublished report to the United States Department of Agriculture Bureau of Entomology and Plant Quarantine. On file USFS Regional Office, Missoula, MT. 16 pp.Google Scholar
Fagre, D.B., Peterson, D.L., Hessl, A.E., (2003). Taking the pulse of mountains: Ecosystem responses to climatic variability.. Climatic Change 59, 263282.Google Scholar
Ferguson, S.A., (1999). Climatology of the Interior Columbia River Basin.. USDA Forest Service General Technical Report, PNW-GTR-445. Pacific Northwest Research Station, Portland, OR. 32 pp.Google Scholar
Finklin, A.I., (1983). Weather and Climate of the Selway–Bitterroot Wilderness.. University Press of Idaho, Moscow, Idaho.Google Scholar
Fritts, H.C., (1974). Relationships of ring widths in arid-site conifers to variations in monthly temperature and precipitation.. Ecological Monographs, 44, 411440.Google Scholar
Fritts, H.C., (1976). Tree Rings and Climate.. Academic Press, New York.Google Scholar
Gervais, B.R., MacDonald, G.M., (2001). Tree-ring and summer-temperature response to volcanic aerosol forcing at the northern tree-line, Kola Peninsula, Russia.. The Holocene 11, 499505.Google Scholar
Graumlich, L.J., Brubaker, L.B., (1986). Reconstruction of annual temperature (1590–1979) for Longmire, Washington, derived from tree-rings.. Quaternary Research 25, 223234.CrossRefGoogle Scholar
Graumlich, L.J., Pisaric, M.F.J., Waggoner, L.A., Littell, J.S., King, J.C., (2003). Upper Yellowstone River flow and teleconnections with Pacific basin climate variability during the past three centuries.. Climatic Change 59, 245262. Data archived at the World Data Center for Paleoclimatology, Boulder, Colorado, USA.Google Scholar
Gray, S.T., Graumlich, L.J., Betancourt, J.L., (2007). Annual precipitation in the Yellowstone National Park Region since AD 1173.. Quaternary Research, 68, 1827.Google Scholar
Grissino-Mayer, H.D., (2001). Evaluating crossdating accuracy: a manual and tutorial for the computer program COFECHA.. Tree-Ring Research 57, (2) 205221.Google Scholar
Holmes, R.L., (1983). Computer-assisted quality control in tree-ring dating and measurement.. Tree-Ring Bulletin 43, 6978.Google Scholar
Hughes, M.K., Woodhouse, C., Brown, P.M., (1998). Tree-ring width index from Flint Creek Range, MT.. IGBP PAGES/World Data Center for Paleoclimatology Data Contribution MT116. NOAA/NCDC Paleoclimatology Program. Boulder, Colorado, USA.Google Scholar
Hutchins, H.E., Lanner, R.M., (1982). The central role of Clark nutcracker in the dispersal and establishment of whitebark pine.. Oecologia 55, 192201.Google Scholar
Intergovernmental Panel on Climate Change (IPCC) (2007). Fourth assessment report, climate change 2007.. Solomon, S., Qin, D., Manning, M., Marquis, M., Averyt, K., Tignor, M.M.B., Miller, H.L. Jr., Chen, Z. The Physical Science Basis Cambridge University Press, Cambridge, United Kingdom.Google Scholar
Jacoby, G.C., D'Arrigo, R.D., (1997). Tree rings, carbon dioxide, and climate change.. Proceedings of the National Academy of Sciences, 94, 83508353.Google Scholar
Jones, P.D., Mann, M.E., (2004). Climate over past millennia.. Reviews of Geophysics 42, MAY 6 2004 42 pp Art. No. RG2002.Google Scholar
Keane, R.E., Arno, S.F., (1993). Rapid decline of whitebark pine in western Montana: evidence from 20-Forestry,year remeasurements.. Western Journal of Applied 8, 4446.Google Scholar
Kendall, K.C., Keane, R.E., (2001). Whitebark pine decline: infection, mortality, and population trends.. Tomback, D.F., Arno, S.F., Keane, R.E. Whitebark Pine Communities Island Press, Washington., pp. 221242.Google Scholar
Kipfmueller, K.F., (2003). Fire-climate-vegetation interactions in subalpine forests of the Selway-Bitterroot Wilderness Area, Idaho and Montana, USA.. Unpublished Ph.D. Dissertation, The University of Arizona.Google Scholar
Kipfmueller, K.F., Swetnam, T.W., Morgan, P., (2002). Climate and mountain pine beetle induced tree mortality in the Selway-Bitterroot Wilderness Area.. Unpubl. Cont. Rep. RMRS-99611-RJVA.Google Scholar
Körner, C., (1998). A re-assessment of high elevation treeline positions and their explanation.. Oecologia, 115, 445459.Google ScholarPubMed
LaMarche, V.C. Jr. (1974). Frequency-dependent relationships between tree-ring series along an ecological gradient and some dendroclimatic implications.. Tree-Ring Bulletin 34, 120.Google Scholar
LaMarche, V.C. Jr., Stockton, C.W., (1974). Chronologies from temperature-sensitive bristlecone pines at upper treeline in the western United States.. Tree-Ring Bulletin, 34, 2145.Google Scholar
LaMarche, V.C. Jr., Graybill, D.A., Fritts, H.C., Rose, M.R., (1984). Increasing atmospheric carbon dioxide: tree ring evidence for growth enhancement in natural vegetation.. Science, 225, 10191021.CrossRefGoogle ScholarPubMed
Lloyd, A.H., Fastie, C.L., (2002). Spatial and temporal variability in the growth and climate response of treeline trees in Alaska.. Climatic Change, 52, 481509.Google Scholar
Logan, J.A., Régnière, J., Powell, J.A., (2003). Assessing the impacts of global warming on forest pest dynamics.. Frontiers in Ecology and the Environment 1, 130137.Google Scholar
Lough, J.M., Fritts, H.C., (1987). An assessment of the possible effects of volcanic eruptions on North American climate using tree-ring data, 1602–1900 A.D.. Climatic Change 10, 219239.Google Scholar
Luckman, B.H., (2000). The little ice age in the Canadian Rockies.. Geomorphology 32, 357384. Data archived at the World Data Center for Paleoclimatology, Boulder, Colorado, USA.Google Scholar
Luckman, B.H., Wilson, R.J.S., (2005). Summer temperatures in the Canadian Rockies during the last millennium: a revised record.. Climate Dynamics 24, 131144.Google Scholar
Luckman, B.H., Jozsa, L.A., Murphy, P.J., (1984). Living seven-hundred-year-old Picea engelmannii and Pinus albicaulis in the Canadian Rockies.. Arctic and Alpine Research 16, 419422.Google Scholar
Mann, M.E., (2007). Climate over the past two millennia.. Annual Review of Earth and Planetary Sciences 35, 111136.Google Scholar
Mann, M.E., Raymond, S., Bradley, R.S., Hughes, M.K., (1999). Northern Hemisphere temperatures during the past millennium: inferences, uncertainties, and limitations.. Geophysical Research Letters 26, 759762. Data archived at the World Data Center for Paleoclimatology, Boulder, Colorado, USA.Google Scholar
McDonald, G.I., Hoff, R.J., (2001). Blister rust: an introduced plague.. Tomback, D.F., Arno, S.F., Keane, R.E. Whitebark Pine Communities Island Press, Washington., pp. 193220.Google Scholar
Michaelsen, J., (1987). Cross-validation in statistical climate forecast models.. Journal of Climate and Applied Meteorology 26, 15891600.2.0.CO;2>CrossRefGoogle Scholar
Osborn, T.J., Briffa, K.R., (2006). The spatial extent of 20th-century warmth in the context of the past 1200 years.. Science 311, 841844.Google Scholar
Ostrom, C.W. Jr. (1990). Time series analysis, regression techniques, second edition.. Quantitative Applications in the Social Sciences. Sage Publications, Newbury Park. v. 07-009.Google Scholar
Pederson, G.T., Gray, S.T., Fagre, D.B., Graumlich, L.J., (2006). Long-duration drought variability and impacts on ecosystem services: a case study from Glacier National Park, Montana.. Earth Interactions 10, 128. Data archived at the World Data Center for Paleoclimatology, Boulder, Colorado, USA.Google Scholar
Perkins, D.L., Swetnam, T.W., (1996). A dendroecological assessment of whitebark pine in the Sawtooth-Salmon River region, Idaho.. Canadian Journal of Forest Research 26, 21232133. Data archived at the World Data Center for Paleoclimatology, Boulder, Colorado, USA.Google Scholar
Peterson, D.W., Peterson, D.L., (1994). Effects of climate on radial growth of conifers in the North Cascade Mountains.. Canadian Journal of Forest Research 24, 19211932.Google Scholar
Robertson, A., Overpeck, J., Rind, D., Mosley-Thompson, E., Zielinski, G., Lean, J., Koch, D., Penner, J., Tegen, I., Healy, R., (2001). Hypothesized climate forcing time series for the last 500 years.. Journal of Geophysical Research 106, 14,78314,803. Data archived at the World Data Center for Paleoclimatology, Boulder, Colorado, USA.Google Scholar
Romme, W.H., (1982). Fires and landscape diversity in subalpine forests of Yellowstone National Park.. Ecological Monographs, 52, 199221.CrossRefGoogle Scholar
Salzer, M.W., Hughes, M.K., (2007). Bristlecone pine tree rings and volcanic eruptions over the last 5000 yr.. Quaternary Research, 67, 5768.Google Scholar
Scuderi, L.A., (1990). Tree-ring evidence for climatically effective volcanic eruptions.. Quaternary Research 34, 6785.CrossRefGoogle Scholar
Simpkin, T., Siebert, L., (1994). Volcanoes of the world. 2nd edition. Tucson, AZ.. Geoscience Press, p. 349.Google Scholar
Swetnam, T.W., Lynch, A.M., (1993). Multicentury, regional-scale patterns of western spruce budworm outbreaks.. Ecological Monographs 63, 399424.CrossRefGoogle Scholar
Tomback, D.F., Hoffmann, L.A., Sund, S.K., (1990). Coevolution of whitebarkpine and nutcrackers.. Schmidt, W.C., McDonald, C. Implications for forest regeneration USDA Forest Service Intermountain Research Station, Ogden, UT., pp. 118129.Google Scholar
Tranquillini, W., (1979). Physiological ecology of the alpine timberline.. Springer-Verlag, Berlin.CrossRefGoogle Scholar
Vaganov, E.A., Hughes, M.K., Kirdyanov, A.V., Schweingruber, F.H., Silkin, P.P., (1999). Influence of snowfall and melt timing on tree growth in subarctic Eurasia.. Nature 400, 149151.Google Scholar
Weisberg, S., (1985). Applied linear regression, 2nd edition.. John Wiley and Sons, New York, NY.Google Scholar
Westerling, A.L., Hidalgo, H.G., Cayan, D.R., Swetnam, T.W., (2006). Warming and earlier spring increase western U.S. wildfire activity.. Science 313, 940943.Google Scholar
Wigley, T.M.L., Briffa, K.R., 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, 201213.Google Scholar
Wiles, G.C., D'Arrigo, R.D., Villalba, R., Calkin, P.E., Barclay, D.J., (2004). Century-scale solar variability and Alaskan temperature change over the past millennium.. Geophysical Research Letters 31, L15203 doi:10.1029/2004GL020050.Google Scholar
Wilmking, M., Juday, G., Barber, V., Zald, H., (2004). Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds.. Global Change Biology 10, 17241736.CrossRefGoogle Scholar
Wilmking, M., D'Arrigo, R.D., Jacoby, G.C., Juday, G.P., (2005). Increased temperature sensitivity and divergent growth trends in circumpolar boreal forests.. Geophysical Research Letters 32, L15715 doi:10.1029/2005GL023331.Google Scholar
Wood, S.L., (1982). The bark and ambrosia beetles of North and central America (Coleoptera: Scolytidae), a taxonomic monograph.. Great Basin Naturalist Memoirs, no. 66. Provo Utah, Brigham Young University.Google Scholar