Hostname: page-component-7dd5485656-bt4hw Total loading time: 0 Render date: 2025-10-31T03:49:21.496Z Has data issue: false hasContentIssue false
  • English
  • Français

Long-Term Temperature Trends and Tree Growth in the Taymir Region of Northern Siberia

Published online by Cambridge University Press:  20 January 2017

Gordon C. Jacoby ,
Nikolai V. Lovelius ,
Oleg I. Shumilov ,
Oleg M. Raspopov ,
Juri M. Karbainov  and
David C. Frank
Gordon C. Jacoby
Affiliation:
Lamont-Doherty Earth Observatory, 61 Route 9W, Palisades, New York 10964
Nikolai V. Lovelius
Affiliation:
Botanic Institute of RAS, Butlerova str., 13, app 393, St. Petersburg, 195256 Russia
Oleg I. Shumilov
Affiliation:
High-Latitude Geophysical Lab. of SPbF IZMIRAN, P.O. Box 123, Apatity, Murmansk Region, 184300 Russia
Oleg M. Raspopov
Affiliation:
St. Petersburg Filial Institute of Terrestrial Magnetism, Ionosphere and Radiowaves Propagation (SPbF IZMIRAN), Muhnoy per., 2, St. Petersburg, 191023 Russia
Juri M. Karbainov
Affiliation:
Taymir State Nature Preserve, Aeroportovskaya St., 20a, KW1, Khatanga 663260, Krasnoyarsk Region, Russia
David C. Frank
Affiliation:
Lamont-Doherty Earth Observatory, 61 Route 9W, Palisades, New York 10964
Get access Rights & Permissions [Opens in a new window]

Abstract

The northernmost conifers in the world are located well above the Arctic Circle in the Taymir region of northern Siberia and have been recording the thermal environment for centuries to millennia. The trees respond to temperatures beyond the narrow season of actual cambial cell division by means of root growth, photosynthesis, lignification of cell walls, and other biochemical processes. Data from annual tree-ring widths are used to reconstruct May–September mean temperatures for the past four centuries. These warm-season temperatures correlate with annual temperatures and indicate unusual warming in the 20th century. However, there is a loss of thermal response in ring widths since about 1970. Previously the warmer temperatures induced wider rings. Most major warming and cooling trends are in agreement with other high-latitude temperature reconstructions based on tree-ring analyses with some regional differences in timing of cooling in the late 18th century and of warming in the late 19th century.

Keywords

tree ringstemperatureArcticpaleoclimateSiberia

Information

Type
Research Article
Information
Quaternary Research , Volume 53 , Issue 3 , May 2000 , pp. 312 - 318
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.)

Article purchase

Temporarily unavailable

References

Blasing, T.J., Duvick, D.N., West, D.C., (1981). Dendroclimatic calibration and verification using regionally averaged and single station precipitation data. Tree-Ring Bulletin 41, 37–43.Google Scholar
Bradley, R.S., Jones, P.D., (1992). Climate since A.D. 1500. Routledge, London.Google Scholar
Briffa, K.R., Schweingruber, F.H., Jones, P.D., Osborn, T.J., Shiyatov, S.G., Vaganov, E.A., (1998). Reduced sensitivity of recent tree-growth to temperature at high northern latitudes. Nature 391, 678–682.Google Scholar
Cook, E.R., (1985). A Time Series Analysis Approach to Tree-Ring Standardization.Google Scholar
Cook, E.R., Kairiukstis, L., (1990). Methods of Dendrochronology. Kluwer Academic, Dordrecht.Google Scholar
D'Arrigo, R.D., Jacoby, G.C., (1992). Dendroclimatic evidence from northern North America. Bradley, R.S., Jones, P.D., Climate since A.D. 1500 Routledge, London.296–311.Google Scholar
Fowells, H.A., (1965). Silvics of Forest Trees of the United States, U. S. Department of Agriculture Handbook Vol. 271. USDA, Washington.Google Scholar
Giddings, J.L. Jr., (1941). Dendrochronology in northern Alaska. University of Arizona Bulletin 12, .Google Scholar
Holmes, R.L., (1983). Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bulletin 44, 69–75.Google Scholar
Hughes, M.K., Vaganov, E.A., Shiyatov, S., Touchan, R., Funkhouser, G., (1999). Twentieth-century summer warmth in northern Yakutia in a 600-year context. Holocene 9, 629–634.Google Scholar
Jacoby, G.C., D'Arrigo, R.D., (1989). Reconstructed Northern Hemisphere annual temperature since 1671 based on high-latitude tree-ring data from North America. Climate Change 14, 39–59.Google Scholar
Jacoby, G.C., D'Arrigo, R.D., (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., Davaajamts, T., (1996). Mongolian tree rings and 20th-century warming. Science 273, 771–773.Google Scholar
Kramer, P.J., Kozlowski, T.T., (1979). Physiology of Woody Plants. Academic Press, San Diego.Google Scholar
Panyushkina, I.P., Vaganov, E.A., Shishov, V.V., (1996). Spatial-temporal variation of radial tree growth in relation to climate in the north of middle Siberia. Dendrochronologia 14, 115–126.Google Scholar
Shiyatov, S.G., Mazepa, V.S., Vaganov, E.A., Schweingruber, F.H., (1996). Summer temperature variations reconstructed by tree-ring data at the polar timberline in Siberia. Dean, J.S., Meko, D.M., Swetnam, T.W., Tree Rings, Environment and Humanity: Proceedings of the International Conference, Tucson, Arizona, 17–21 May 1994 Radiocarbon, Tucson.61–70.Google Scholar
Tranquillini, W., (1979). Physiological Ecology of the Alpine Timberline. Springer-Verlag, New York.CrossRefGoogle Scholar
Vaganov, E.A., Naurazhaev, M.M., Schweingruber, F.H., Briffa, K.R., Moell, M., (1996). An 840-year tree-ring width chronology for Taimir as an indicator of summer temperature changes. Dendrochronologia 14, 193–205.Google 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, 149–151.CrossRefGoogle Scholar