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A high-resolution reconstruction of Storglaciären mass balance back to 1780/81 using tree-ring data and circulation indices

Published online by Cambridge University Press:  20 January 2017

Hans W. Linderholm ,
Peter Jansson  and
Deliang Chen
Hans W. Linderholm*
Affiliation:
Regional Climate Group, Department of Earth Sciences, Göteborg University, SE-405 30 Göteborg, Sweden Laboratory for Climate Studies, National Climate Center, China Meteorological Administration, 46 Zhongguancun Nandajie, Haidian, Beijing 100081, China
Peter Jansson
Affiliation:
Tarfala Research Station, Department of Physical Geography and Quaternary Geology, Stockholm University, SE-106 91 Stockholm, Sweden
Deliang Chen
Affiliation:
Regional Climate Group, Department of Earth Sciences, Göteborg University, SE-405 30 Göteborg, Sweden Laboratory for Climate Studies, National Climate Center, China Meteorological Administration, 46 Zhongguancun Nandajie, Haidian, Beijing 100081, China
*
⁎Corresponding author. Regional Climate Group, Department of Earth Sciences, Göteborg University, Box 460, SE-405 30 Göteborg, Sweden. Fax: +46 31 7731986. E-mail address:[email protected] (H.W. Linderholm).
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Abstract

Storglaciären in northernmost Sweden has the world's longest ongoing continuous mass-balance record, starting in 1946. To extend this mass-balance record, we have reconstructed summer (bS) and winter (bW) mass balances separately back to the mass balance year 1780/81 with annual resolution. We used tree-ring data for bS and a set of circulation indices, based on the sea-level pressure, for bW. Both proxies have correlation coefficients with respective mass balance components of ca. 0.7. The reconstructed net balance (bN) of Storglaciären was well correlated to the observations during 1946–1980 (r = 0.8, p < 0.05). Our reconstruction agrees well with previously obtained results of northern Sweden glacier variability, where the predominantly positive bN years between 1890 and 1910 correspond to the well documented post-Little Ice Age advance of Storglaciären. Furthermore, the results suggest that bS, as a function of summer temperatures, is more important than bW in determining the bN, which is contrary to glaciers in the maritime parts of western Scandinavia. In general, bN has been negative over the last 220 yr, suggesting a predomination of continental conditions over northern Sweden. However, the influence of bW increased in the late twentieth century, indicating a shift to a more oceanic climate regime.

Keywords

Mass-balance reconstructionTree ringsCirculation indicesStorglaciärenNorthern Sweden
Type
Research Article
Information
Quaternary Research , Volume 67 , Issue 1 , January 2007 , pp. 12 - 20
Copyright
University of Washington

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References

ACIA Impacts of a Warming Arctic: Arctic Climate Impact Assessment. (2004). Cambridge Univ. Press, 140 pp.Google Scholar
Ångström, A., (1968). Sveriges klimat. Andra upplagan. Generalstabens litografiska Anstalts Förlag, . Stockholm:, Sweden.Google Scholar
Blenckner, T., and Chen, D. Comparison of the impact of regional and north-atlantic atmospheric circulation on an aquatic ecosystem. Climate Research 23, (2003). 131–136.Google Scholar
Briffa, K.R. Annual climate variability in the Holocene: interpreting the message of ancient trees. Quaternary Science Reviews 19, (2000). 87–105.Google Scholar
Briffa, K.R., Jones, P.D., Bartholin, T.S., Eckstein, D., Schweingruber, F.H., Karlén, W., Zetterberg, P., and Eronen, M. Fennoscandian summers from AD 500: temperature changes on short and long timescales. Climate Dynamics 7, (1992). 111–119.Google Scholar
Briffa, K.R., Schweingruber, F.H., Jones, P.D., Osborn, T.J., Shiyatov, S.G., and Vaganov, E.A. Reduced sensitivity of recent tree-growth to temperature at high northern latitudes. Nature 391, (1998). 678–682.Google Scholar
Briffa, K.R., Osborn, T.J., Schweingruber, F.H., Jones, P.D., Shiyatov, S.G., and Vaganov, E.A. Tree-ring width and density around the Northern Hemisphere: part 1, local and regional climate signals. Holocene 12, (2002). 737–757.Google Scholar
Carter, R., LeRoy, S., Nelson, T., Laroque, C.P., and Smith, D.J. Dendroglaciological investigations at Hilda Creek rock glacier, Banff National Park, Canadian Rocky Mountains. Géographie physique et Quaternaire 53, (1999). 365–371.Google Scholar
Chen, D. A monthly circulation climatology for Sweden and its application to a winter temperature case study. International Journal of Climatology 20, (2000). 1067–1076.Google Scholar
Chen, D., and Hellström, C. The influence of the North Atlantic Oscillation on the regional temperature variability in Sweden: spatial and temporal variations. Tellus 51A, (1999). 505–516.Google Scholar
Chen, D., and Li, X. Scale dependent relationship between maximum ice extent in the Baltic Sea and atmospheric circulation. Global and Planetary Change 41, (2004). 275–283.Google Scholar
Chen, D., and Omstedt, A. Climate-induced variability of sea level in Stockholm: influence of air temperature and atmospheric circulation. Advances in Atmospheric Sciences 22, (2005). 655–664.Google Scholar
Cook, E.R., Briffa, K.R., and Jones, P.D. Spatial regression methods in dendroclimatology: a review and comparison of two techniques. International Journal of Climatology 14, (1994). 379–402.Google Scholar
Fritts, H.C. Tree-Rings and Climate. (1976). Academic Press, London, England.Google Scholar
Hellström, C., Chen, D., Achberger, C., and Räisänen, J. A comparison of climate change scenarios for Sweden based on statistical and dynamical downscaling of monthly precipitation. Climate Research 19, (2001). 45–55.Google Scholar
Hodge, S.M., Trabant, D.C., Krimmel, R.M., Heinrichs, T.A., March, R.S., and Josberger, E.G. Climate variations and changes in mass of three glaciers in western North America. Journal of Climate 11, (1998). 2161–2179.Google Scholar
Holmes, R.L., Adams, R.K., Fritts, H.C., (1986). Tree-ring chronologies of western North America: California, eastern Oregon and northern Great Basin, with procedures used in the chronology development work, including user manuals for computer programs COFECHA and ARSTAN. Laboratory of Tree-Ring Research, University of Arizona, Tucon. Chronology Series VI.Google Scholar
Holmlund, P. Mass balance of Storglaciären during the 20th century. Geografiska Annaler 69A, (1987). 439–447.Google Scholar
Holmlund, Climatic influence on the size of glaciers in Northern Scandinavia during the last two centuries. Frenzel, B., Boulton, G.S., Gläser, B., Huckriede, U. Glacier Fluctuations during the Holocene. Paleoclimate Research vol. 24, (1997). 115–124. Special Issue: ESF Project “European Paleoclimate and Man” 16. European Science Foundation (ISBN 3-437-25518-5) Google Scholar
Holmlund, P., and Eriksson, M. The cold surface layer on Storglaciären. Geografiska Annaler 71A, (1989). 241–244.Google Scholar
Holmlund, P., and Jansson, P. The Tarfala mass balance programme. Geografiska Annaler 81A, (1999). 621–631.Google Scholar
Holmlund, P., Jansson, P., and Pettersson, R. A re-analysis of the 58 year mass balance record of Storglaciären, Sweden. Annals of Glaciology 42, (2005). 389–393.Google Scholar
Hooke, R.LeB., Gould, J.E., and Brzozowski, J. Near-surface temperatures near and below the equilibrium line on polar and subpolar glaciers. Zeitschrift für Gletscherkunde und Glazialgeologie 19, 1 (1983). 1–25.Google Scholar
Hurrell, J.W. Decadal trends in the North Atlantic Oscillation: regional temperatures and precipitation. Science 269, (1995). 676–679.Google Scholar
IPCC Houghton, J.T., Ding, Y., Griggs, D.J., Noguer, M., van der Linden, P.J., Dai, X., Manskell, K., and Johnson, C.A. Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the International Panel on Climate Change. (2001). Cambridge Univ. Press, Cambridge. 881 pp.Google Scholar
Isaksen, K., Holmlund, P., Sollid, J.L., and Harris, C. Three deep alpine-permafrost boreholes in Svalbard and Scandinavia. Permafrost and Periglacial Processes 12, (2001). 13–25.Google Scholar
Jansson, P. Effect of uncertainties in measured variables on the calculated mass balance of Storglaciären, Geografiska. Annaler 81A, (1999). 633–642.Google Scholar
Jansson, P., and Linderholm, H. Constraints on latitudinal climate forcing of mass balances of Scandinavian glaciers from combined glacier and tree-ring studies. Annals of Glaciology 42, (2005). 303–310.Google Scholar
Jansson, P., Pettersson, R., in press. Spatial and temporal characteristics of a long mass balance record, Storglaciären. Sweden. Arctic, Antarctic, and Alpine Research.Google Scholar
Jansson, P., Rosqvist, G., and Schneider, T. Glacier fluctuations, suspended sediment flux and glacio-lacustrine sediments. Geografiska Annaler 87A, (2005). 37–50.Google Scholar
Johansson, B., and Chen, D. The influence of wind and topography on precipitation distribution—A case study in Sweden. International Journal of Climatology (2003). 231523–231535.Google Scholar
Jones, P.D., Briffa, K.R., Barnett, T.P., and Tett, S.F.B. High-resolution palaeoclimatic records for the last millennium: interpretation, integration and comparison with General Circulation Model control-run temperatures. Holocene 8, (1998). 455–471.Google Scholar
Jones, P.D., New, M., Parker, D.E., Martin, S., and Rigor, I.G. Surface air temperature and its changes over the past 150 years. Reviews of Geophysics 37, (1999). 173–199.Google Scholar
Jones, P.D., Davies, T.D., Lister, D.H., Slonosky, V., Jönsson, T., Bärring, L., Jönsson, P., Maheras, P., Kolyva-Machera, F., Barriendos, M., Martin-Vide, J., Alcoforado, M.J., Wanner, H., Pfister, C., Schuepbach, E., Kaas, E., Schmith, T., Jacobeit, J., and Beck, C. Monthly mean pressure reconstructions for Europe. International Journal of Climatology 19, (1999). 347–364.Google Scholar
Karlén, W. Lacustrine sediments and tree-limit variations as indicators of Holocene climatic fluctuations in Lappland: Northern Sweden. Geografiska Annaler 58A, (1976). 1–34.Google Scholar
Karlén, W. Dendrochronology, mass balance and glacier front fluctuations in northern Sweden. Mörner, N.-A., and Karlén, W. Climatic Changes on a Yearly to Millennial Basis. (1984). Riedel Publishing, 263–271.Google Scholar
Karlén, W. Scandinavian glacial and climatic fluctuations during the Holocene. Quaternary Science Reviews 7, (1988). 199–209.Google Scholar
Karlén, W., and Denton, G.H. Holocene glacial variations in Sarek National Park, northern Sweden. Boreas 5, (1975). 25–56.Google Scholar
King, L. High mountain permafrost in Scandinavia. Proceedings, 4th International Conference on Permafrost, Washington, DC, National Academy. (1983). 612–617.Google Scholar
Larocque, S.J., and Smith, D.J. “Little Ice Age” proxy glacier mass balance records reconstructed from tree rings in the Mt Waddington area, British Columbia Coast Mountains, Canada. Holocene 15, (2005). 748–757.Google Scholar
Linderson, M.-L., Achberger, C., and Chen, D. Statistical downscaling and scenario construction of precipitation in Scania, Southern Sweden. Nordic Hydrology 35, (2004). 261–278.Google Scholar
Luckman, B.H. Glacier fluctuations and tree-ring records for the last millennium in the Canadian Rockies. Quaternary Science Reviews 12, (1993). 441–450.Google Scholar
Matthews, J.A. Glacier and climatic fluctuations inferred from tree-growth variations over the last 250 years, central southern Norway. Boreas 6, (1977). 1–24.Google Scholar
McCabe, G.J., Fountain, A.G., and Dyurgerov, M. Variability in winter mass balance of northern hemisphere glaciers and relations with atmospheric circulation. Arctic, Antarctic, and Alpine Research 32, (2000). 64–72.Google Scholar
Nesje, A., Lie, Ø., and Dahl, S.O. Is the North Atlantic Oscillation reflected in Scandinavian glacier mass balance records?. Journal of Quaternary Science 15, (2000). 587–601.Google Scholar
Nicolussi, K. Jahrringe und Massenbilanz. Dendroklimatologische Rekonstruktion der Massenbilanzreihe bis zum Jahr 1400 mittels Pinus cembra-Reihen aus den Ötztaler Alpen, Tirol. Zeitschrift für Gletscherkunde und Glazialgeologie 30, (1995). 11–52.Google Scholar
Østrem, G., Brugman, M., (1991). Glacier mass balance measurements: a manual for field and office work. Saskatoon: National Hydrology research Institute, and Oslo: the Norwegian Water resources and Electricity Board, .Google Scholar
Pettersson, R., Jansson, P., and Holmlund, P. Cold surface layer thinning on Storglaciären, Sweden, observed by repeated ground penetrating radar surveys. Journal of Geophysical Research 108, F1 (2003). 6004 doi:http://dx.doi.org/10.1029/2003JF000024Google Scholar
Pohjola, V.A., and Rogers, J.C. Atmospheric circulation and variations in Scandinavian glacier mass balance. Quaternary Research 47, (1997). 29–36.Google Scholar
Pohjola, V.A., Cole-Dai, J., Rosqvist, G., Stroeven, A.P., and Thompson, L.G. Potential to recover climatic information from Scandinavian ice cores: an example from the small ice cap Riukojietna. Geografiska Annaler 87A, 1 (2005). 259–270.Google Scholar
Raper, S.C.B., Briffa, K.R., and Wigley, T.M.L. Glacier change in northern Sweden from AD 500: a simple geometric model of Storglaciären. Journal of Glaciology 42, (1996). 341–351.Google Scholar
Rossby, C.G. The scientific basis of modern meteorology in climate and man. Yearbook of Agriculture. (1941). US Department of Agriculture, Washington DC, USA.Google Scholar
Santer, B.D., Taylor, K.E., Wigley, T.M.L., Johns, T.C., Jones, P.D., Karoly, D.J., Mitchell, J.F.B., Oort, A.H., Penner, J.E., Ramaswamy, V., Schwarzkop, M.D., Stouffer, R.J., and Tett, S. A search for human influences on the thermal structure of the atmosphere. Nature 382, (1996). 39–46.Google Scholar
Schytt, V. Glaciers of the Kebnekajse-Massif. Geografiska Annaler 41, (1959). 213–227.Google Scholar
Schytt, V. Glaciologiska metoder i klimatforskningens tjänst. Svensk (1973). 77–88.Google Scholar
Tangborn, W.V. A mass balance model that uses low-altitude meteorological observations and the area-altitude distribution of a glacier. Geografiska Annaler 81A, (1999). 753–765.Google Scholar
Thompson, D.W.J., and Wallace, J.M. The Arctic Oscillation signature in wintertime geopotential height and temperature fields. Geophysical Research Letters 25, (1998). 1297–1300.Google Scholar
Visbeck, M.H., Hurrell, J.W., Polvani, L., and Cullen, H.M. The North Atlantic Oscillation: past, present, and future. Proceedings of the National Academy of Sciences 98, (2001). 12876–12877.Google Scholar
Walters, R.A., and Meier, M.F. Variability of glacier mass balances in western North America. American Geophysical Union, Geophysical Monographs 55, (1989). 365–374.Google Scholar
Watson, E., and Luckman, B.H. Tree-ring based mass-balance estimates for the past 300 years at Peyto Glacier, Alberta, Canada. Quaternary Research 62, (2004). 9–18.Google Scholar