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Tree-ring-based reconstructions of North American glacier mass balance through the Little Ice Age — Contemporary warming transition

Published online by Cambridge University Press:  20 January 2017

Nathan L. Malcomb  and
Gregory C. Wiles
Nathan L. Malcomb*
Affiliation:
Portland Forestry Sciences Laboratory, Pacific Northwest Research Station, USDA Forest Service, 620 SW Main Street, Suite 400, Portland, OR 97205, USA
Gregory C. Wiles
Affiliation:
Department of Geology, The College of Wooster, 944 College Mall, Wooster, OH 44691, USA
*
*Corresponding author. E-mail addresses:[email protected] (N.L. Malcomb), [email protected] (G.C. Wiles).
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Abstract

Glacier mass-balance reconstructions provide a means of placing relatively short observational records into a longer-term context. In western North America, mass-balance records span four to five decades and capture a relatively narrow window of glacial behavior over an interval that was dominated by warming and ablation. We use temperature- and moisture-sensitive tree-ring series to reconstruct annual mass balance for six glaciers in the Pacific Northwest and Alaska. Mass-balance models rely on the climatic sensitivity of tree-ring chronologies and teleconnection patterns in the North Pacific. The reconstructions extend through the mid to latter portions of the Little Ice Age (LIA) and explore the role of climate variability in forcing mass balance across multiple environmental gradients. Synchronous positive mass-balance intervals coincide with regional moraine building and solar minima, whereas differences in LIA glacier behavior are related to synoptic climate forcing. Secular warming in the late 19th century to present corresponds with the only multi-decadal intervals of negative mass balance in all glacier reconstructions. This suggests that contemporary retreat in western North America is unique with respect to the last several centuries and that regional patterns of glacier variability are now dominated by global climate forcing.

Keywords

Glacier mass balanceTree ringsPacific NorthwestClimate change
Type
Research Article
Information
Quaternary Research , Volume 79 , Issue 2 , March 2013 , pp. 123 - 137
Copyright
University of Washington

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Footnotes

1 Fax: + 1 330 263 2249.

References

Adjusted and Homogenized Canadian Climate Data, Environment Canada. http://ec.gc.ca/dccha-ahccd/Default.asp?lang=En&n=B1F8423A-1 (Accessed on 12 November 2011) Google Scholar
Arendt, A., Eschelmeyer, K., Harrison, W., Lingle, C., and Valentine, V. Rapid wastage of Alaska glaciers and their contribution to rising sea level. Science 297, (2002). 382–386.Google Scholar
Barclay, D., Wiles, G., and Calkin, P. Holocene glacier fluctuations in Alaska. Quaternary Science Reviews 28, (2009). 2034–2048.CrossRefGoogle Scholar
Begét, J. Tephrochronology, lichenometry and radiocarbon dating at Gulkana Glacier, central Alaska Range, USA. The Holocene 4, (1994). 307–313.CrossRefGoogle Scholar
Biondi, F., Kozubowski, T., and Panorska, A. Stochastic modeling of regime shifts. Climate Research 23, (2002). 23–30.Google Scholar
Bitz, C., and Battisti, D. Interannual to decadal variability in climate and the glacier mass balance in Washington, Western Canada, and Alaska. Journal of Climate 12, (1999). 3181–3196.2.0.CO;2>CrossRefGoogle Scholar
Bolch, T., Menounos, B., and Wheate, R. Landsat-based inventory of glaciers in western Canada, 1985–2005. Remote Sensing of Environment 114, (2010). 127–137.Google Scholar
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M., Showers, W., Hoffmann, S., Bond, R., Hajdas, I., and Bonani, G. Persistent solar influence on North Atlantic climate during the Holocene. Science 294, (2001). 2130–2136.Google Scholar
Briffa, K., Schweingruber, F., Jones, P., Osborn, T., Harris, I., Shiyatov, S., Vaganov, E., Grudd, H., and Cowie, J. Trees tell of past climates: but are they speaking less clearly today?. Philosophical Transactions: Biological Sciences 353, (1998). 65–73.CrossRefGoogle Scholar
Burbank, D. Correlations of climate, mass balances, and glacial fluctuations at Mount Rainier, Washington, USA, since 1850. Arctic and Alpine Research 14, (1982). 137–148.Google Scholar
Calkin, P., Wiles, G., and Barclay, D. Holocene coastal glaciations of Alaska. Quaternary Science Reviews 20, (2001). 449–461.Google Scholar
Conway, H., Rasmussen, L., and Marshall, H. Annual mass balance of Blue Glacier, USA: 1955–97. Geografiska Annaler 18, (1999). 509–520.Google Scholar
Cook, E., and Kairiukstis, L. Methods of Dendrochronology: Applications in the Environmental Sciences. (1990). Dordrecht Kluwer Academic Publishers, Google Scholar
D'Arrigo, R., Wilson, R., Deser, C., Wiles, G., Cook, E., and Villalba, R. Tropical-North Pacific climate linkages over the past four centuries. Journal of Climate 18, (2005). 5253–5265.Google Scholar
D'Arrigo, R., and Jacoby, G. Northern North American tree-ring evidence for regional temperature changes after major volcanic events. Climatic Change 41, (1999). 1–15.Google Scholar
Dyurgerov, M. Glacier mass balance and regime measurements and analysis, 1945–2003. Occasional Paper 55, (2005). Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO.Google Scholar
Fauria, M., and Johnson, E. Large-scale climatic patterns control large lightning fire occurrence in Canada and Alaska forest regions. Journal of Geophysical Research 11, (2006). http://dx.doi.org/10.1029/2006JG000181Google Scholar
Friedman, J. A variable span smoother. Technical Report vol. 5, (1984). Stanford University, Palo Alto.Google Scholar
Gedalof, Z., and Smith, D. Dendroclimatic response of mountain hemlock (Tsuga mertensiana) in Pacific North America. Canadian Journal of Forestry Research 31, (2001). 322–332.Google Scholar
Granshaw, F., and Fountain, A. Glacier change (1958–1998) in the North Cascades National Park Complex, Washington, USA. Journal of Glaciology 52, (2006). 251–256.Google Scholar
Graumlich, L. Precipitation variation in the Pacific Northwest (1675–1975) as reconstructed from tree rings. Annals of the Association of American Geographers 77, (1987). 19–29.Google Scholar
Grissino-Mayer, H.D. Evaluating crossdating accuracy: a manual and tutorial for the computer program Cofecha. Tree-ring Research 57, (2001). 205–221.Google Scholar
Heikkinen, O. Dendrochronological evidence of variations of Coleman Glacier, Mount Baker, Washington, USA. Arctic and Alpine Research 16, (1984). 53–64.Google Scholar
Heusser, C. Variations of Blue, Hoh, and White glaciers during recent centuries. Arctic 10, (1957). 139–150.Google Scholar
Hodge, S., Trabant, D., Krimmel, R., Heinrichs, T., March, R., and Josberger, E. Climate variations and changes in mass of three glaciers in Western North America. Journal of Climate 11, (1998). 2161–2179.2.0.CO;2>CrossRefGoogle Scholar
Holmes, R. Computer-assisted quality control in tree-ring dating and measurement. Tree Ring Bulletin 43, (1983). 69–78.Google Scholar
Hu, F., Kaufman, D., Yoneji, S., Nelson, D., Shemesh, A., Huang, Y., Tian, J., Bond, G., Clegg, B., and Brown, T. Cyclic variation and solar forcing of Holocene climate in the Alaska subarctic. Science 301, (2003). 1890–1893.Google Scholar
Jackson, K., and Fountain, A. Spatial and morphological change on Eliot Glacier, Mount Hood, Oregon, USA. Annals of Glaciology 46, (2007). 222–226.CrossRefGoogle Scholar
Josberger, E., Bidlake, W., March, R., and Kennedy, B. Glacier mass-balance fluctuations in the Pacific Northwest and Alaska, USA. Annals of Glaciology 46, (2007). 291–296.Google Scholar
Koch, J., Osborn, G., and Clague, J.J. Pre-Little Ice Age glacier fluctuations in Garibaldi Provincial Park, southern Coast Mountains, British Columbia. The Holocene 17, (2007). 1069–1078.Google Scholar
Koch, J., Clague, J., and Osborn, G. Glacier fluctuations during the past millennium in Garibaldi Provincial Park, southern Coast Mountains, British Columbia. Canadian Journal of Earth Sciences 44, (2007). 1215–1233.Google Scholar
Koch, J., Menounos, , and Clague, J. Glacier change in Garibaldi Provincial Park, southern Coast Mountains, British Columbia, since the Little Ice Age. Global and Planetary Change 66, (2009). 161–178.Google Scholar
Laroque, S., and Smith, D. Little Ice Age glacial activity in the Mt. Waddington area, British Columbia, Coast Mountains, Canada. Canadian Journal of Earth Sciences 40, (2003). 1413–1436.CrossRefGoogle Scholar
Laroque, S., and Smith, D. ‘Little Ice Age'proxy glacier mass balance records reconstructed from tree rings in the Mt. Waddington Area, British Columbia, Coast Mountains Canada. The Holocene 15, (2005). 748–757.Google Scholar
Lewis, D., and Smith, D. Dendrochronological mass balance reconstruction, Strathcona Provincial Park, Vancouver Island, British Columbia, Canada. Arctic, Antarctic and Alpine 36, (2004). 598–602.CrossRefGoogle Scholar
Ljungqvist, F., Krusic, P., Brattström, G., and Sundqvist, H. Northern Hemisphere temperature patterns in the last 12 centuries. Climate of the Past 8, (2012). 227–249.Google Scholar
Lowell, T. As climate changes, so do glaciers. Proceedings of the National Academy of Sciences of the United States of America 97, (2000). 1351–1354.Google Scholar
Luckman, B. The Little Ice Age in the Canadian Rockies. Geomorphology 32, (2000). 357–384.CrossRefGoogle Scholar
Luckman, B., and Wilson, R. Summer temperatures in the Canadian Rockies during the last millennium: a revised record. Climate Dynamics 24, (2005). 131–141.Google Scholar
MacDonald, G., and Case, R. Variations in the Pacific Decadal Oscillation over the past millennium. Geophyscial Research Letters 32, (2005). L08703 Google Scholar
Mann, M., Zhang, Z., Rutherford, S., Bradley, R., Hughes, M., Shindell, D., Ammann, C., Faluvegi, G., and Ni, F. Global signatures and dynamical origins of the Little Ice Age and Medieval Climate Anomaly. Science 326, (2009). 1256–1260.CrossRefGoogle ScholarPubMed
Mantua, N. Patterns of change in climate and Pacific salmon production. American Fisheries Society Symposium 70, (2009). 1–15.Google Scholar
Mantua, N., and Hare, S. The Pacific Decadal Oscillation. Journal of Oceanography 58, (2001). 35–44.Google Scholar
Mayo, L., and March, R. Air temperature and precipitation at Wolverine Glacier, Alaska: Glacier Growth in a wetter warmer climate. Annals of Glaciology 12, (1990). 191–194.Google Scholar
McCabe, G., Fountain, A., 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
Meier, M. The recent history of advance-retreat and net budget of South Cascade Glacier. Transactions, American Geophysical Union 45, (1964). 608 Google Scholar
Menounos, B., Osborn, G., Clague, J., and Luckman, B. Latest Pleistocene and Holocene glacier fluctuations in western Canada. Quaternary Science Reviews 28, (2009). 2049–2074.Google Scholar
Miller, D. Chronology of neoglacial moraines in the Dome Peak Area, North Cascades Range, Washington. Arctic and Alpine Research 1, (1969). 49–65.Google Scholar
Miller, G., Geirsdóttir, A., Zhong, Y., Larsen, D., Otto-Bliesner, B., Holland, M., Bailey, D., Refsnider, K., Lehman, S., Southon, J., Anderson, C., Björnsson, H., and Thordarson, T. Abrupt onset of the Little Ice Age triggered by volcanism and sustained by sea-ice/ocean feedbacks. Geophysical Research Letters 39, (2012). http://dx.doi.org/10.1029/2011GL050168CrossRefGoogle Scholar
Moberg, A., Sonechkin, D., Holmgren, K., Datsenko, N., and Wibjörn, K. Highly variable Northern Hemisphere temperatures reconstructed from low and high-resolution proxy data. Nature 3265, (2005). 1–5.Google Scholar
Molnia, B. Late nineteenth to early twenty-first century behavior of Alaskan glaciers as indicators of changing regional climate. Global and Planetary Change 56, (2006). 23–56.CrossRefGoogle Scholar
Moore, R., and Demuth, M. Mass balance and streamflow variability at Place Glacier, Canada, in relation to recent climate fluctuations. Hydrological Processes 15, (2001). 3473–3486.Google Scholar
Moore, R., Fleming, S., Menounos, B., Wheate, R., Fountain, A., Stahl, K., Holm, K., and Jakob, M. Glacier change in western North America: influences on hydrology, geomorphic hazards and water quality. Hydrological Processes 23, (2009). 42–61.Google Scholar
Paterson, W. The Physics of Glaciers. (1998). Butterworth and Heinemann Publishers, Oxford.Google Scholar
Pederson, G., Gray, S., Woodhouse, C., Betancourt, J., Fagre, D., Littell, J., Watson, E., Luckman, B., and Graumlich, L. The unusual nature of recent snowpack declines in the North American Cordillera. Science 333, (2011). 332–335.Google Scholar
Pederson, N., Bell, A., Knight, T., Leland, C., Malcomb, N., Anchukaitis, K., Tackett, K., Scheff, J., Brice, A., Catron, B., Blozan, W., and Riddle, J. Long-term perspective on a modern drought in the American Southeast. Environmental Research Letters 7, (2012). http://dx.doi.org/10.1088/1748-9326/7/1/014034Google Scholar
Pelto, M., and Riedel, J. Spatial and temporal variations in annual balance of North Cascade glaciers, Washington, 1984–2000. Hydrological Processes 15, (2001). 3461–3472.Google Scholar
Peterson, D., and Peterson, D. Mountain hemlock growth responds to climatic variability at annual and decadal time scales. Ecology 82, (2001). 3330–3345.Google Scholar
Péwé, T., and Reger, R. Delta river area, Alaska range. Péwé, T.L., and Reger, R.D. Guidebook to Permafrost and Quaternary Geology Along the Richardson and Glenn Highways Between Fairbanks and Anchorage, Alaska. (1983). University of Alaska, Fairbanks. 47–135.Google Scholar
PRISM Climate Group, Oregon State University http://prism.oregonstate.edu (Accessed on 12 November 2011) Google Scholar
Robinson, B.J., (1998). Reconstruction of the glacial history of the Columbia Icefield. Alberta. M.Sc. thesis. University of Western Ontario, London, Ontario.Google Scholar
Roe, G.H., and O'Neal, M. The response of glaciers to intrinsic climate variability: observations and models of late Holocene variations. Journal of Glaciology 55, (2009). 839–854.Google Scholar
Shea, J., Marshall, S., and Livingston, J. Glacier distributions and climate in the Canadian Rockies. Arctic, Antarctic, and Alpine Research 36, (2004). 272–279.CrossRefGoogle Scholar
Sisson, T., Robinson, J., and Swinney, D. Whole-edifice ice volume change A.D. 1970 to 2007/2008 at Mount Rainier, Washington, based on LiDAR surveying. Geology 39, (2011). 639–642.Google Scholar
Spicer, R. Recent variations of Blue Glacier, Olympic Mountains, Washington, U.S.A.. Arctic and Alpine Research 21, (1989). 1–21.Google Scholar
Trouet, V., and Taylor, A. Multi-century variability in the Pacific North American circulation pattern reconstructed from tree rings. Climate Dynamics 35, (2009). 0930–7575.Google Scholar
United States Geological Survey Long Term Benchmark Glacier Program http://ak.water.usgs.gov/glaciology/all_bmg/3glacier_temp.htm (Accessed 12 November 2011) Google Scholar
Vonmoos, M., Beer, J., and Muscheler, R. Large variations in Holocene solar activity: constraints from Be10 in the Greenland Ice Core Project ice core. Journal of Geophysical Research 111, (2006). A10105 CrossRefGoogle Scholar
Wang, T., Ottera, O., Gao, Y., and Wang, H. The response of the North Pacific Decadal Variability to strong tropical volcanic eruptions. Climate Dynamics (2012). 1–20.Google Scholar
Ware, D., and Thomson, R. Interannual to multidecadal timescale climate variations in the North Pacific. Journal of Climate 13, (2000). 3209–3220.Google Scholar
Watson, E., personal communication (2006).Google Scholar
Watson, E., and Luckman, B. Tree-ring based reconstructions of precipitation for the Southern Canadian Cordillera. Climatic Change 65, (2004). 209–241.Google Scholar
Watson, E., and Luckman, B. Tree-ring based mass balance estimates for the past 300 years at Peyto Glacier, Alberta, Canada. Quaternary Research 62, (2004). 9–18.Google Scholar
Watson, E., Luckman, B., and Yu, B. Long-term relationships between reconstructed seasonal mass balance at Peyto Glacier, Canada, and Pacific sea surface temperatures. The Holocene 16, (2006). 783–790.Google Scholar
Wiles, G., and Calkin, P. Late Holocene, high-resolution glacial chronologies and climate, Kenai Mountains, Alaska. Geological Society of America Bulletin 106, (1994). 281–303.Google Scholar
Wiles, G., Barclay, D., and Calkin, P. Tree-ring dated “Little Ice Age” histories of maritime glaciers from western Prince William Sound, Alaska. The Holocene 9, (1999). 163–173.Google Scholar
Wiles, G., Jacoby, G., Davi, N., and McAllister, R. Late Holocene glacier fluctuations in the Wrangell Mountains, Alaska. Geological Society of America Bulletin 114, (2002). 896–908.Google Scholar
Wiles, G., D'Arrigo, R., Villalba, R., Calkin, P., and Barclay, D. Century-scale solar variability and Alaskan temperature change over the past millennium. Geophysical Research Letters 31, (2004). L15203 Google Scholar
Wiles, G., Barclay, D., Calkin, P., and Lowell, T. Century to millennial-scale temperature variations for the last two thousand years indicated by the glacial geologic records of Southern Alaska. Global and Planetary Change 57, (2008). 115–125.Google Scholar
Wilson, R., Wiles, G., D'Arrigo, R., and Zweck, C. Cycles and shifts: 1300-years of multidecadal temperature variability in the Gulf of Alaska. Climate Dynamics 28, (2006). 425–440.CrossRefGoogle Scholar
Wood, L., Smith, D., and Demuth, M. Extending the Place Glacier mass-balance record to AD 1585, using tree rings and wood density. Quaternary Research 76, (2011). 305–313.Google Scholar
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