Hostname: page-component-78c5997874-j824f Total loading time: 0 Render date: 2024-11-04T19:04:16.177Z Has data issue: false hasContentIssue false

A Dendroclimatic Reconstruction of Annual Precipitation on the Western Canadian Prairies since A.D. 1505 from Pinus flexilis James

Published online by Cambridge University Press:  20 January 2017

Roslyn A. Case
Affiliation:
Department of Geography, McMaster University, Hamilton, Ontario, L8S 4K1, Canada
Glen M. MacDonald
Affiliation:
Department of Geography, McMaster University, Hamilton, Ontario, L8S 4K1, Canada

Abstract

Tree-ring chronologies from living and sub-fossil Pinus flexilis James (limber pine) trees extend back more than 500 yr on the western edge of the Great Plains in Alberta. Living trees were found to be as old as 526 yr. Tree-ring growth in Pinus flexilis is most sensitive to annual precipitation over the annualization period August to July. The longevity of the trees coupled with their sensitivity to variations in annual precipitation make them an important resource for constructing annually resolved multicentury records of paleohydrology on the northwestern Great Plains. A 487-yr reconstruction of annual precipitation in southwestern Alberta was produced from the tree-ring series. This is the longest dendroclimatological reconstruction of precipitation available from the northern plains. The reconstruction has some similarity to reconstructions from the western Great Plains of the United States. However, there are also many divergences in the timing of droughts. Some of this divergence may reflect the importance of orographic uplift in producing precipitation along the eastern flanks of the Rocky Mountains. Our reconstruction shows that the frequency of droughts in Alberta during the period of instrumental records, about the last 100 yr, has not been appreciably different from conditions of the preceding four centuries. In addition, the most severe drought of this century, which led to widespread farm abandonment between 1918 and 1922, was not the most severe drought in the past 487 yr.

Type
Research Article
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

Atmospheric Environment Service (1986). “An Applied Climatology for Drought in the Prairie Provinces,” Climate Centre Report 86-4. AES Drought Study Group, Downsview.Google Scholar
Bauer, D. J. (1988). “Proceedings of the Prairie Drought Workshop.” National Hydrological Research institute, Saskatoon.Google Scholar
Beaty, C. B. (1975). “The Landscapes of Southern Alberta: A Regional Geomorphology.” University of Lethbridge, Lethbridge.Google Scholar
Biasing, T. J., and Duvick, D. N. (1984). Reconstruction of precipitation history in North American com belt using tree rings. Nature 307 , 143145.Google Scholar
Biasing, T. J. Stahle, D. W., and Duvick, D. N. (1988). Tree-ring-based reconstruction of annual precipitation in the south-central United States from 1750-1980. Water Resources Research 24 , 63171.Google Scholar
Bonsai, B. R. Chakravarti, A, K., and Lawford, R. G. (1993). Teleconnections between North Pacific SST anomalies and growing season extended dry spells on the Canadian prairies, international Journal of Climatology 13 , 865878.Google Scholar
Canadian Forestry Service. (1985). “Forest Insect and Disease Conditions in Canada 1985,” Canadian Insect and Disease Survey. Ministry of Supply and Services Canada, Ottawa.Google Scholar
Dey, B. (1982). Nature and possible causes of droughts on the Canadian Prairies—Case studies. Journal of Climatology 2 , 233249.Google Scholar
Duvick, D. N., and Biasing, T. J. (1981). A dendroclimatic reconstruction of annua! precipitation amounts in Iowa since 16&0. Water Resources Research 17 , 11831189.Google Scholar
Fritts, H. C. (1976). “Tree Rings and Climate.” Academic Press, London.Google Scholar
Fritts, H. C. (1993). “PRECON 3.0 User’s Manual,” dendrochronological modeling. Tucson, AZ.Google Scholar
Fritts, H. C. Lofgren, G. R., and Gordon, G. A., (1979). Variations in climate since 1602 as reconstructed from tree rings. Quartsmary Research 12 , 1846.Google Scholar
Fritts, H. C., and Shatz, D. I. (1975). Selecting and characterizing tree-ring chronologies for dendroclimatic analysis. Tree-Ring Bulletin 35 , 3140.Google Scholar
Godwin, R. B. (1988). Drought: The impending crisis? In “Proceedings of the Prairie Drought Workshop” (Bauer, D. J., Ed.), pp. 1115. National Hydrological Research Institute, Saskatoon.Google Scholar
Government of Alberta and University of Alberta. (1969). “Atlas of Alberta.” Univ. of Alberta Press, Edmonton.Google Scholar
Grissino-Mayer, H. Holmes, R., and Fritts, H. C. (1993). International Tree-Ring Data Bank Program Library User’s Manual.” Laboratory of Tree-Ring Research, University of Arizona, Tucson, AZ.Google Scholar
Hare, F. K., and Thomas, M. K., (1979). “Climate Canada,” 2nd ed. Wiley, Toronto.Google Scholar
Johnson, E. A., and Fryer, G. I. (1989). Population dynamics and age-class distributions in lodgepole pine-Engelmann spruce forests. Ecology 70 , 13351345.Google Scholar
Jones, D. C. (1987). “Empire of Dust: Setting and Abandoning the Prairie Dry Belt.” Univ. of Alberta Press, Edmonton.Google Scholar
Latif, M., and Bamett, T. P. (1994). Causes of decadal climate variability over the North Pacific and North America. Science 266 , 634637.Google Scholar
Loaiciga, H. A. Haston, L., and Michaelsen, J. (1993). Dendrohydrology and long-term hydrologic phenomenon. Reviews of Geophysics 31 , 151171.Google Scholar
Longley, R. W. (1967). The frequency of Chinooks in Alberta. The Albertan Geographer 3 , 2022.Google Scholar
Longley, R. W. (1972). “The Climate of the Prairie Provinces,” pp. 76. Atmospheric Environment Service, Ministry of Supply and Services Canada, Ottawa.Google Scholar
Manabe, S., and Wetherald, R. T. (1987). Large scale changes of soil wetness induced by an increase in atmospheric carbon dioxide. Journal of Atmospheric Science 44 , 12111235.Google Scholar
Meko, D. M. (1982). Drought history in the western Great Plains from tree rings. In “Proceedings of the International Symposium on Hydrometeorology” (Johnson, A. I. and Clark, R. A., Eds.) pp. 321326. American Water Resources Association.Google Scholar
Meko, D. M. (1992). Dendroclimatic evidence from the Great Plains of the United States. In “Climate Since A.D. 1500” (Bradley, R. S. and Jones, P. D., Eds.) pp. 312330. Routledge, London.Google Scholar
Moss, E. H. (1955). The vegetation of Alberta. The Botanical Review 21 , 493564.Google Scholar
Namais, J., and Cayan, D. R. (1981). Large-scale air-sea interactions and short-period climatic fluctuations. Science 214 , 869876.Google Scholar
Nelson, J. G., and England, R. E. (1971). Some comments on the causes and effects of fire in the northern grasslands area of Canada and the nearby United States, Ca. 1750-1900. Canadian Geographer 15 , 295306.Google Scholar
Oladipo, E. O. (1987). Power spectra and coherence of drought in the interior plains. Journal of Climatology 7 , 477491.Google Scholar
Riebsame, W. E. Changnon, S. A. Jr., and Karl, T. R. (1991). “Drought and Natural Resource Management in the United States.” Westview Press, Boulder, LO.Google Scholar
Reinelt, , (1970). On the role of orogeny in the precipitation of Alberta. The Albertan Geographer 6 , 4558.Google Scholar
Stahle, D. W., and Cleaveland, M. K. (1988). Texas drought history reconstructed and analyzed from 1698 to 1980. Journal of Climate 1 , 5974.Google Scholar
Stockton, C. W., and Meko, D. M. (1983). Drought recurrence in the Great Plains as reconstructed from long-term tree-ring records. Journal of Climate and Applied Meteorology 22 , 1729.Google Scholar
Stokes, M. A., and Smiley, T. L. (1968). “An Introduction to Tree-Ring Dating.” Univ. Chicago Press, Chicago.Google Scholar
Szeicz, J.M., and MacDonald, G.M. (1994). Age-dependent tree-ring responses of subarctic white spruce to climate. Canadian Journal of Forest Research 24 , 120132.Google Scholar
Trenberth, K. E. Branstator, G. W., and Arkin, P. A. (1988). Origins of the 1988 North American drought. Science 242 , 16401645.Google Scholar