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Centennial-to-millennial fluctuations in July temperatures in North Finland as recorded by timberline tree rings of Scots pine

Published online by Cambridge University Press:  20 January 2017

Maxim Ogurtsov
Affiliation:
Cosmic Ray Laboratory, A.F. Ioffe Physico-Technical Institute, 194021, Blytechnicheskaya 26, St. Petersburg, Russia
Samuli Helama
Affiliation:
Department of Geology, University of Helsinki, PO Box 64, FIN-00014 Helsinki, Finland
Matti Eronen
Affiliation:
Department of Geology, University of Helsinki, PO Box 64, FIN-00014 Helsinki, Finland
Markus Lindholm*
Affiliation:
Department of Geology, University of Helsinki, PO Box 64, FIN-00014 Helsinki, Finland
*
*Corresponding author.E-mail addresses:maxim.ogurtsov@mail.ioffe.ru (M. Ogurtsov), markus.lindolm@goensuu.fi (M. Lindholm).

Abstract

A tree-ring proxy of summer temperature anomalies for northern Finland for the past 7500 yr was analyzed using Fourier spectrum and wavelet approaches. Multicentennial (250–450 yr) variability is present in the proxy record during most of the time range. This variability is suggested to reflect low-frequency variability in the North Atlantic Oscillation. Century-scale (90–130 yr) variation is another important feature of the tree-ring proxy data during the Holocene and may be attributed to Glessberg solar activity variations. In addition, an approximately 2000-yr quasi-period is found in this temperature proxy data, similar to the millennial-scale variability, present in many climate records from the North Atlantic region. The results point to the importance of multiple forcings underlying significant Holocene climatic fluctuations.

Type
Short Papers
Copyright
University of Washington

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References

Appenzeller, C., Stocker, T.F., Anklin, M., (1998). North Atlantic oscillation dynamics recorded in Greenland ice cores. Science 282, 446449.Google Scholar
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., de Menocal, P., Priore, P., Cullen, H., Hajdas, I., Bonani, G., (1997). A pervasive millennial-scale cycle in North Atlantic Holocene and Glacial climates. Science 278, 12571266.Google Scholar
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M.N., Showers, W., Hoffmann, S., Lotti-Bond, R., Hajdas, I., Bonani, G., (2001). Persistent solar influence on North Atlantic climate during the Holocene. Science 294, 21302135.Google Scholar
Briffa, K.R., Jones, P.D., (1990). Basic chronology statistics and assessment. Cook, E., Kairiukstis, L., Methods of Dendrochronology: Applications in the Environmental Sciences Kluwer Academic Publishers, , Dordrecht., 137152.Google Scholar
Briffa, K.R., Jones, P.D, Schweingruber, H.F., Karlen, 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., Climatic Variations and Forcing Mechanisms of the Last 200 Years. NATO ASI series 1: Global Environmental Change vol. 41, 941.Google Scholar
Briffa, K.R., Osborn, T.J., Schweingruber, F.H., Harris, I.C., Jones, P.D., Shiyatov, S.G., Vaganov, E.V., (2001). Low-temperature variations from a northern tree ring density network. Journal of Geophysical Research 106, D3 29292941.Google Scholar
Cook, E.R., Briffa, K.R., Meko, D.M., Graybill, D.A., Funkhouser, G., (1995). The ‘segment length curse’ in long tree-ring chronology development for palaeoclimatic studies. The Holocene 5, 229237.Google Scholar
Cook, E.R., Buckley, B.M., D'Arrigo, R.D., Peterson, M.J., (2000). Warm-season temperature since 1600 BC reconstructed from Tasmanian tree rings and their relationship to large-scale sea surface temperature anomalies. Climate Dynamics 16, 7991.Google Scholar
Damon, P.E., Jirikowic, J.L., (1992). Solar forcing of global climate change?. Taylor, R.E., Long, A., Kra, R.S., Radiocarbon After Four Decades: An Interdisciplinary Perspective Springer-Verlag, , New York., 117129.Google Scholar
Damon, P.E., Peristykh, A.N., (2000). Radiocarbon calibration and application to geophysics, solar physics and astrophysics. Radiocarbon 42, 1 137150.Google Scholar
Dansgaard, W., Johnsen, S.J., Clausen, H.B., Langway, C.C., (1971). Climatic record revealed by the Camp Century ice core. Turekian, K.K, The Late Cenozoic Glacial Ages Yale University Press, , New Haven., 3755.Google Scholar
Delworth, T., Manabe, S., Stouffer, R.J., (1993). Interdecadal variations of the thermohaline circulation in a coupled ocean–atmosphere model. Journal of Climate 6, 19932011.Google Scholar
Eronen, M., Zetterberg, P., Briffa, K., Lindholm, M., Meriläinen, J., Timonen, M., (2002). The supra-long Scots pine tree-ring record for Finnish Lapland—Part 1: chronology construction and initial interferences. The Holocene.Google Scholar
Fritts, H.C., (1976). Tree-Rings and Climate. Academic Press, , London., 576 p.Google Scholar
Glueck, M.F., Stockton, C.W., (2000). Reconstruction of the North Atlantic Oscillation. International Journal of Climatology 21, 12 14531465.Google Scholar
Grootes, P.M., Stuiver, M., (1997). Oxygen 18/16 variability in Greenland snow and ice with 10−3–to 105-year time resolution. Journal of Geophysical Research 102, C12 2645526740.Google Scholar
Helama, S., Lindholm, M., Timonen, M., Eronen, M., (2002). The supra-long Scots pine tree-ring record for Finnish Lapland—Part 2: interannual to centennial variability in summer temperatures for 7500 years. The Holocene.Google Scholar
Houtermans, J.C., (1971). Geophysical interpretation of Bristlcone pine radiocarbon measurements using a method of Fourier analysis of unequally spaced data. PhD Thesis, , University of Bern., .Google Scholar
Jones, P.D., Briffa, K.R, Barnett, T.P., Telt, S.F.B., (1998). High-resolution palaeoclimatic records for the last millennium: interpretation, integration and comparison with General Circulation Model control-run temperatures. The Holocene 8, 4 455471.Google Scholar
Leventer, A., Domack, E.W., Ishman, S.E., McClennen, C.E., Manley, P., (1996). Productivity cycles of 200–300 years in the Antarctic Peninsula region: understanding linkages among the sun, atmosphere, oceans, sea ice and biota. GSA Bulletin 108, 12 16261644.Google Scholar
Lindholm, M., Eggertsson, Ò., Lovelius, N., Raspopov, O., Shumilov, O., Läänelaid, A., (2001). Growth indices of North European Scots pine record the seasonal North Atlantic Oscillation. Boreal Environment Research 6, 110.Google Scholar
Magny, M., (1993). Solar influences on Holocene climatic changes illustrated by correlation between past lake-level fluctuations and the atmospheric 14C record. Quaternary Research 40, 19.Google Scholar
Magny, M., (1998). Reconstruction of Holocene lake-level changes in the French Jura: methods and results. Harrison, S., Frenzel, B., Huckriede, U., Weiss, M.M., Palaeohydrology as Reflected in Lake Level Changes as Climatic Evidence for Holocene Time Gustav Fischer Verlag, , Stuttgart., 6785.Google Scholar
Mahasenan, N., Watts, R.G., Dowlatabady, H., (1997). Low-frequency oscillations in temperature-proxy records and implications for recent climate change. Geophysical Research Letters 24, 5 563566.Google Scholar
Mann, M.E., Park, J., Bradley, R.S., (1995). Global interdecadal and century-scale climate oscillations during the past five centuries. Nature 378, 266270.Google Scholar
Mikolajewicz, U., Maier-Reimer, E., (1990). Internal secular variability in an ocean general circulation model. Climate Dynamics 4, 145156.CrossRefGoogle Scholar
Ogurtsov, M.G., Kocharov, G.E., Lindholm, M., Eronen, M., Nagovitsyn, Yu.A., (2001). Solar activity and regional climate. Radiocarbon 43, 2a 439447.Google Scholar
Ogurtsov, M.G., Kocharov, G.E., Lindholm, M., Meriläinen, J., Eronen, M., Nagovitsyn, Yu.A., (2002). Evidence of solar variation in tree-ring-based climate reconstructions. Solar Physics 205, 2 403417.Google Scholar
Ogurtsov, M.G., Nagovitsyn, Yu.A., Kocharov, G.E., Jungner, H., (2003). Long-period cycles of Sun's activity recorded in direct solar data and proxies. Solar PhysicsAccepted in.Google Scholar
Seppä, H., Birks, H.J.B., (2002). Holocene climate reconstructions from the Fennoscandian tree-line area based on pollen data from Toskaljavri. Quaternary Research 57, 191199.Google Scholar
Shabalova, M.V., Weber, S.L., (1999). Patterns of temperature variability on multidecadal to centennial timescales. Journal of Geophysical Research 104, 3102331042.Google Scholar
Shnitnikov, A.V., (1957). Variability of the general moistening at continents of the Earth's Northern Hemisphere. Proceedings of Geographical Society of USSR 16, 133.(in Russian).Google Scholar
Sonett, C.P., Finney, S.A., (1990). The spectrum of radiocarbon. Philosophical Transactions of the Royal Society of London. A 330, 423426.Google Scholar
Stuiver, M., Braziunas, T., (1993). Sun, ocean climate and atmospheric 14CO2: an evaluation of causal and spectral relationships. The Holocene 3, 4 289305.Google Scholar
Stuiver, M., Braziunas, T.F., Becker, B., Kromer, B., (1991). Climatic, solar, oceanic and geomagnetic influences on late-glacial and holocene atmospheric 14C/12C changes. Quaternary Research 35, 124.Google Scholar
Stuiver, M., Grootes, P., Braziunas, T., (1995). The GISP2 δ 18O climate record of the past 16500 years and the role of the sun, ocean and volcanoes. Quaternary Research 44, 341354.CrossRefGoogle Scholar
Stuiver, M., Braziunas, T.F., Grootes, P.M., Zielinski, G.A., (1997). Is there evidence for solar forcing of climate in the GISP2 oxygen isotope record?. Quaternary Research 48, 259266.Google Scholar
Torrence, C., Compo, G.P., (1998). A practical guide to wavelet analysis. Bulletin of the American Meteorological Society 79, 61.Google Scholar
Williams, G.E., (1990). Precambrian cyclic rhythmities: solar–climatic or tidal signatures?. Philosophical Transactions of the Royal Society of London. A 330, 445448.Google Scholar
Williams, G.E., Sonett, C.P., (1985). Solar signature in sedimentary cycles from the late Precambrian Elatina formation Australia. Nature 318, 523528.Google Scholar
White, J.W.C., Barlow, L.K., Fisher, D., Grootes, P., Jouzel, J., Johnsen, S.J., Stuiver, M., Clausen, H., (1997). The climate signal in the stable isotopes of snow from Summit, Greenland: results of comparisons with modern climate observations. Journal of Geophysical Research 102, C12 2642526439.Google Scholar