Hostname: page-component-586b7cd67f-gb8f7 Total loading time: 0 Render date: 2024-11-23T03:19:18.841Z Has data issue: false hasContentIssue false

The potential to strengthen temperature reconstructions in ecoregions with limited tree line using a multispecies approach

Published online by Cambridge University Press:  25 June 2019

M. Ross Alexander*
Affiliation:
Harvard Forest, Petersham, Massachusetts 01366, USA Midwest Dendro LLC, Naperville, Illinois 60565, USA
Jessie K. Pearl
Affiliation:
Laboratory of Tree-Ring Research, University of Arizona, Tucson, Arizona 85721, USA Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA
Daniel A. Bishop
Affiliation:
Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA Department of Earth and Environmental Sciences, Columbia University, New York, New York 10025, USA
Edward R. Cook
Affiliation:
Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA
Kevin J. Anchukaitis
Affiliation:
Laboratory of Tree-Ring Research, University of Arizona, Tucson, Arizona 85721, USA Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA School of Geography and Development, University of Arizona, Tucson, Arizona 85721, USA
Neil Pederson
Affiliation:
Harvard Forest, Petersham, Massachusetts 01366, USA
*
*Corresponding author at: e-mail address: [email protected] (M. R. Alexander).

Abstract

Tree-ring reconstructions of temperature often target trees at altitudinal or latitudinal tree line where annual growth is broadly expected to be limited by and respond to temperature variability. Based on this principal, regions with sparse tree line would seem to be restricted in their potential to reconstruct past temperatures. In the northeastern United States, there are only two published temperature reconstructions. Previous work in the region reconstructing moisture availability, however, has shown that using a greater diversity of species can improve reconstruction model skill. Here, we use a network of 228 tree-ring records composed of 29 species to test the hypothesis that an increase in species diversity among the pool of predictors improves reconstructions of past temperatures. Chamaecyparis thyoides alone explained 31% of the variability in observed cool-season minimum temperatures, but a multispecies model increased the explained variance to 44%. Liriodendron tulipifera, a species not previously used for temperature reconstructions, explained a similar amount of variance as Chamaecyparis thyoides (12.9% and 20.8%, respectively). Increasing the species diversity of tree proxies has the potential for improving reconstruction of paleotemperatures in regions lacking latitudinal or elevational tree lines provided that long-lived hardwood records can be located.

Type
Research Article
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2019 

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

REFERENCES

Ahmed, M., Anchukaitis, K.J., Asrat, A., Borgaonkar, H.P., Braida, M., Buckley, B.M., Büntgen, U., et al. , 2013. Continental-scale temperature variability during the past two millennia. Nature Geoscience 6, 339346.Google Scholar
Akaike, H., 1974. A new look at the statistical model identification. IEEE Transactions on Automatic Control 19, 716723Google Scholar
Alexander, M.R., Rollinson, C.R., Moore, D.J.P., Speer, J.H., Rubino, D.L., 2018. Determination of death dates of coarse woody debris of multiple species in the central hardwood region (Indiana, USA). Tree-Ring Research 74, 135143.Google Scholar
Anchukaitis, K.J., Wilson, R., Briffa, K.R., Büntgen, U., Cook, E.R., D'Arrigo, R., Davi, N., et al. , 2017. Last millennium Northern Hemisphere summer temperatures from tree rings: Part II, spatially resolved reconstructions. Quaternary Science Reviews 163, 122.Google Scholar
Baas, C., Rubino, D.L., 2014. Pressing hay in the Commonwealth: using tree-ring growth patterns to date the construction of two Kentucky beater hay press barns. Journal of Kentucky Archaeology 3, 231.Google Scholar
Babst, F., Poulter, B., Bodesheim, P., Mahecha, M.D., Frank, D.C., 2017. Improved tree-ring archives will support earth-system science. Nature Ecology & Evolution 1, 0008.Google Scholar
Balanzategui, D., Knorr, A., Heussner, K.U., Wazny, T., Beck, W., Słowiński, M., Helle, G., et al. , 2017. An 810-year history of cold season temperature variability for northern Poland. Boreas 90, 300453.Google Scholar
Braun, E.L., 1950. Deciduous Forests of Eastern North America. Blakiston, Philadelphia, PA.Google Scholar
Briffa, K.R., Jones, P.D., Wigley, T.M.L., Pilcher, J.R., Baillie, M.G.L., 1986. Climate reconstruction from tree rings: Part 2, spatial reconstruction of summer mean sea-level pressure patterns over Great Britain. Journal of Climatology 6, 115.Google Scholar
Brubaker, L.B., 1980. Spatial patterns of tree growth anomalies in the Pacific Northwest. Ecology 61, 798807.Google Scholar
Campbell, R., McCarroll, D., Robertson, I., Loader, N.J., Grudd, H., Gunnarson, B., 2011. Blue intensity in Pinus sylvestris tree rings: a manual for a new palaeoclimate proxy. Tree-Ring Research 67, 127134.Google Scholar
Carbone, M.S., Czimczik, C.I., Keenan, T.F., Murakami, P.F., Pederson, N., Schaberg, P.G., Xu, X., Richardson, A.D., 2013. Age, allocation and availability of nonstructural carbon in mature red maple trees. New Phytologist 200, 11451155.Google Scholar
Carrer, M., 2011. Individualistic and time-varying tree-ring growth to climate sensitivity. PLoS ONE 6, 18.Google Scholar
Cavin, L., Jump, A.S., 2016. Highest drought sensitivity and lowest resistance to growth suppression are found in the range core of the tree Fagus sylvatica L. not the equatorial range edge. Global Change Biology 23, 362379.Google Scholar
Conkey, L.E., 1986. Red spruce tree-ring widths and densities in eastern North America as indicators of past climate. Quaternary Research 26, 232243.Google Scholar
Cook, E.R., 1985. A Time Series Analysis Approach to Tree Ring Standardization. PhD dissertation, School of Renewable Natural Resources, University of Arizona, Tucson.Google Scholar
Cook, E.R., 1987. The decomposition of tree-ring series for environmental studies. Tree-Ring Bulletin 47, 3759.Google Scholar
Cook, E.R., Briffa, K.R., Jones, P.D., 1994. Spatial regression methods in dendroclimatology: a review and comparison of two techniques. Journal of Climatology 14, 379402.Google Scholar
Cook, E.R., Callahan, W., 1992. The Development of a Standard Tree-Ring Chronology for Dating Historical Structures in the Greater Philadelphia Region. Tree-Ring Laboratory, Lamont-Doherty Geological Observatory, Columbia University, New York.Google Scholar
Cook, E.R., Cole, J., 1991. On predicting the response of forests in eastern North America to future climatic change. Climatic Change 19, 271282.Google Scholar
Cook, E.R., D'Arrigo, R.D., Mann, M.E., 2002. A well-verified, multiproxy reconstruction of the winter North Atlantic Oscillation Index since A.D. 1400. Journal of Climate 15, 17541764.Google Scholar
Cook, E.R., Jacoby, G.C. Jr., 1977. Tree-ring-drought relationships in the Hudson Valley, New York. Science 198, 399401.Google Scholar
Cook, E.R., Jacoby, G.C., 1979. Evidence for quasi-periodic July drought in the Hudson Valley, New York. Nature 282, 390392.Google Scholar
Cook, E.R., Johnson, A.H., 1989. Climate change and forest decline: a review of the red spruce case. Water, Air, and Soil Pollution 48, 127189.Google Scholar
Cook, E.R., Kairiukstis, L.A. (Eds.), 1990. Methods of Dendrochronology: Applications in the Environmental Sciences. Kluwer Academic, Dordrecht, the Netherlands.Google Scholar
Cook, E.R., Meko, D.M., Stahle, D.W., Cleaveland, M.K., 1999. Drought reconstructions for the continental United States. Journal of Climate 12, 11451162.Google Scholar
Cook, E.R., Pederson, N., 2011. Uncertainty, emergence, and statistics in dendrochronology. Dendroclimatology 77112.Google Scholar
Cook, E.R., Peters, K., 1997. Calculating unbiased tree-ring indices for the study of climatic and environmental change. Holocene 7, 361370.Google Scholar
Daly, C., Taylor, G.H., Gibson, W.P., 1997. The PRISM approach to mapping precipitation and temperature. Proceedings of the 10th Conference of Applied Climatology, American Meteorology, Reno, NV, pp. 1012.Google Scholar
de Graauw, K.K., 2017. Historic log structures as ecological archives: a case study from eastern North America. Dendrochronologia 45, 2334.Google Scholar
Duan, J., Zhang, Q.-B., Lv, L.-X., 2013. Increased variability in cold-season temperature since the 1930s in subtropical China. Journal of Climate 26, 47494757.Google Scholar
Dyer, J.M., 2006. Revisiting the deciduous forests of eastern North America. BioScience 56, 341352.Google Scholar
Emile-Geay, J., McKay, N.P., Kaufman, D.S., von Gunten, L., Wang, J., Anchukaitis, K.J., Abram, N.J., et al. , 2017. A global multiproxy database for temperature reconstructions of the Common Era. Scientific Data 4, 170088.Google Scholar
Frank, D., Esper, J., 2005. Characterization and climate response patterns of a high-elevation, multi-species tree-ring network in the European Alps. Dendrochronologia 22, 107121.Google Scholar
Fritts, H.C., 1976. Tree Rings and Climate. Academic Press, San Diego, CA.Google Scholar
Garcia-Suarez, A.M., Butler, C.J., Baillie, M.G.L., 2009. Climate signal in tree-ring chronologies in a temperate climate: a multi-species approach. Dendrochronologia 27, 183198.Google Scholar
Graumlich, L.J., 1993. Response of tree growth to climatic variation in the mixed conifer and deciduous forests of the upper Great Lakes region. Canadian Journal of Forest Research 23, 133143.Google Scholar
Griffin, D., Woodhouse, C.A., Meko, D.M., Stahle, D.W., Faulstich, H.L., Carrillo, C., Castro, C.L., Leavitt, S.W., 2013. North American monsoon precipitation reconstructed from tree-ring latewood. Geophysical Research Letters 40, 954958.Google Scholar
Hacke, U., Sauter, J.J., 1996. Xylem dysfunction during winter and recovery of hydraulic conductivity in diffuse-porous and ring-porous trees. Oecologia 105, 435439.Google Scholar
Hawley, F., Wedel, N.M., Workman, E.J., 1941. Tree-Ring Analysis and Dating in the Mississippi Drainage. University of Chicago Press, Chicago, IL.Google Scholar
Hayhoe, K., Wake, C.P., Huntington, T.G., Luo, L., Schwartz, M.D., Sheffield, J., Wood, E., et al. , 2006. Past and future changes in climate and hydrological indicators in the US Northeast. Climate Dynamics 28, 381407.Google Scholar
Hijmans, R.J., 2019. raster: Geographic Data Analysis and Modeling. R package version 2.8-19 (accessed May 02, 2019). https://CRAN.R-project.org/package=raster.Google Scholar
Hopton, H.M., Pederson, N., 2005. Climate sensitivity of Atlantic white cedar at its northern range limit. Proceedings of the Arlington Echo Symposium, pp. 16.Google Scholar
Horton, R.G., Yohe, G., Easterling, W., Kates, R., Ruth, M., Sussman, E., Whelchel, A., Wolfe, D., Lipschultz, F., 2014. Northeast. In: Melillo, J.M., Richmond, T.C., Yohe, G.W. (Eds.), Climate Change Impacts in the United States: The Third National Climate Assessment. U.S. Global Change Research Program. U.S. Government Printing Office, Washington, D.C., pp. 371395.Google Scholar
Johnson, A., Cook, E., Siccama, T., 1988. Climate and red spruce growth and decline in the northern Appalachians. Proceedings of the National Academy of Sciences of the United States of America 85, 53695373.Google Scholar
Kagawa, A., Sugimoto, A., Maximov, T.C., 2006. 13CO2 pulse-labelling of photoassimilates reveals carbon allocation within and between tree rings. Plant, Cell & Environment 29, 15711584.Google Scholar
Kosiba, A.M., Schaberg, P.G., Rayback, S.A., Hawley, G.J., 2017. Comparative growth trends of five northern hardwood and montane tree species reveal divergent trajectories and response to climate. Canadian Journal of Forest Research 47, 743754.Google Scholar
Kunkel, K.E., Stevens, L.E., Stevens, S.E., Sun, L., Janssen, E., Wuebbles, D., Rennells, J., DeGaetano, A., Dobson, J.G., 2013. Regional Climate Trends and Scenarios for the U.S. National Climate Assessment: Part 1. Climate of the Northeast U.S. NOAA Technical Report NESDIS 142-1. U.S. Department of Commerce, National Oceanic and Atmospheric Administration, Washington, D.C.Google Scholar
Laderman, A.D., 1989. The Ecology of the Atlantic White Cedar Wetlands: A Community Profile. Biological Report 85(7.21). U.S. Department of the Interior, Fish and Wildlife Service, National Wetland Research Center, Washington, D.C.Google Scholar
Lévesque, M., Andreu-Hayles, L., Pederson, N., 2017. Water availability drives gas exchange and growth of trees in northeastern US, not elevated CO2 and reduced acid deposition. Scientific Reports 7, 19.Google Scholar
Martin-Benito, D., Pederson, N., 2015. Convergence in drought stress, but a divergence of climatic drivers across a latitudinal gradient in a temperate broadleaf forest. Journal of Biogeography 42, 925937.Google Scholar
Mathias, J.M., Thomas, R.B., 2018. Disentangling the effects of acidic air pollution, atmospheric CO2, and climate change on recent growth of red spruce trees in the Central Appalachian Mountains. Global Change Biology 24, 39383953.Google Scholar
Maxwell, J.T., 2016. The benefit of including rarely-used species in dendroclimatic reconstructions: a case study using Juglans nigra in south-central Indiana, USA. Tree-Ring Research 72, 4452.Google Scholar
Maxwell, J.T., Harley, G.L., Matheus, T.J., 2015. Dendroclimatic reconstructions from multiple co-occurring species: a case study from an old-growth deciduous forest in Indiana, USA. Journal of Climatology 35, 860870.Google Scholar
Maxwell, R.S., Harley, G.L., Maxwell, J.T., Rayback, S.A., Pederson, N., Cook, E.R., Barclay, D.J., Li, W., Rayburn, J.A., 2017. An interbasin comparison of tree-ring reconstructed streamflow in the eastern United States. Hydrological Processes 31, 23812394.Google Scholar
Maxwell, J.T., Harley, G.L., Robeson, S.M., 2016. On the declining relationship between tree growth and climate in the Midwest United States: the fading drought signal. Climatic Change 138, 127142.Google Scholar
Maxwell, R.S., Hessl, A.E., Cook, E.R., Pederson, N., 2011. A multispecies tree ring reconstruction of Potomac River streamflow (950–2001). Water Resources Research 47, W05512.Google Scholar
Meko, D., 1997. Dendroclimatic reconstruction with time varying predictor subsets of tree indices. Journal of Climate 10, 687696.Google Scholar
Meko, D., Cook, E.R., Stahle, D.W., Stockton, C.W., Hughes, M.K., 1993. Spatial patterns of tree-growth anomalies in the United States and southeastern Canada. Journal of Climate 6, 17731786.Google Scholar
Overland, J.E., Preisendorfer, R.W., 1982. A significance test for principal components applied to a cyclone climatology. Monthly Weather Review 110, 14.Google Scholar
Pearl, J.K., Anchukaitis, K.J., Pederson, N., Donnelly, J.P., 2017. Reconstructing northeastern United States temperatures using Atlantic white cedar tree rings. Environmental. Research Letters 12, 114012.Google Scholar
Pederson, N., Bell, A.R., Cook, E.R., Lall, U., 2013. Is an epic pluvial masking the water insecurity of the Greater New York City Region? Journal of Climate 26, 13391354.Google Scholar
Pederson, N., Cook, E.R., Jacoby, G.C., Peteet, D.M., Griffin, K.L., 2004. The influence of winter temperatures on the annual radial growth of six northern range margin tree species. Dendrochronologia 22, 729.Google Scholar
Pederson, N., D'Amato, A.W., Dyer, J.M., Foster, D.R., Goldblum, D., Hart, J.L., Hessl, A.E., et al. , 2015. Climate remains an important driver of post-European vegetation change in the eastern United States. Global Change Biology 21, 21052110.Google Scholar
Pederson, N., Tackett, K., McEwan, R.W., Clark, S., Cooper, A., Brosi, G., Eaton, R., Stockwell, R.D., 2012. Long-term drought sensitivity of trees in second-growth forests in a humid region. Canadian Journal of Forest Research 42, 18371850.Google Scholar
Prasad, A.M., Iverson, L.R., Peters, M.P., Matthews, S.N., 2014. Climate Change Tree Atlas. Northern Research Station, U.S. Forest Service, Delaware, OH.Google Scholar
Preisendorfer, R.W., Mobley, C.D., 1988. Principal Component Analysis in Meteorology and Oceanography. Developments in Atmospheric Science, 17. Elsevier, Amsterdam.Google Scholar
Pritzkow, C., Wazny, T., Heussner, K.U., Słowiński, M., Bieber, A., Liñán, I.D., Helle, G., Heinrich, I., 2016. Minimum winter temperature reconstruction from average earlywood vessel area of European oak (Quercus robur) in N-Poland. Palaeogeography, Palaeoclimatology, Palaeoecology 449, 520530.Google Scholar
Reinmann, A.B., Hutyra, L.R., 2016. Edge effects enhance carbon uptake and its vulnerability to climate change in temperate broadleaf forests. Proceedings of the National Academy of Sciences of the United States of America 114, 16.Google Scholar
Richardson, A.D., Carbone, M.S., Keenan, T.F., Czimczik, C.I., Hollinger, D.Y., Murakami, P., Schaberg, P.G., Xu, X., 2013. Seasonal dynamics and age of stemwood nonstructural carbohydrates in temperate forest trees. New Phytologist 197, 850861.Google Scholar
Rohde, R., Muller, R.A., Jacobsen, R., Muller, E., Perlmutter, S., Rosenfeld, A., Wurtele, J., Groom, D., Wickham, C., 2013. A new estimate of the average Earth surface land temperature spanning 1753 to 2011. Geoinformatics and Geostatistics: An Overview 1, 17.Google Scholar
Sperry, J.S., Nichols, K.L., Sullivan, J.E.M., Eastlack, S.E., 1994. Xylem embolism in ring-porous, diffuse-porous, and coniferous trees of northern Utah and interior Alaska. Ecology 75, 17361752.Google Scholar
Stahle, D.W., 1979. Tree-ring dating of historic buildings in Arkansas. Tree-Ring Bulletin 39, 128.Google Scholar
Stahle, D.W., Cleaveland, M.K., 1992. Reconstruction and analysis of spring rainfall over the southeastern U.S. for the past 1000 years. Bulletin of the American Meteorological Society 73, 19471961.Google Scholar
Stahle, D.W., Cleaveland, M.K., Hehr, J.G., 1985. A 450-year drought reconstruction for Arkansas, United States. Nature 316, 530532.Google Scholar
Vaganov, E.A., Anchukaitis, K.J., Evans, M.N., 2011. How well understood are the processes that create dendroclimatic records? A mechanistic model of climatic control on conifer tree-ring growth dynamics. In: Hughes, M.K., Swetnam, T.W., Diaz, H.F. (Eds.), Dendroclimatology: Progress and Prospects. Developments in Paleoecological Research, 11. Springer, Dordrecht, the Netherlands, pp. 3775.Google Scholar
Weedon, J.T., Cornwell, W.K., Cornelissen, J.H.C., Zanne, A.E., Wirth, C., Coomes, D.A., 2009. Global meta-analysis of wood decomposition rates: a role for trait variation among tree species? Ecology Letters 12, 4556.Google Scholar
Weigel, R., Muffler, L., Klisz, M., Kreyling, J., van der Maaten-Theunissen, M., Wilmking, M., Van Der Maaten, E., 2018. Winter matters: sensitivity to winter climate and cold events increases towards the cold distribution margin of European beech (Fagus sylvatica L.). Journal of Biogeography 45, 27792790.Google Scholar
Wigley, T., Briffa, K., Jones, P., 1984. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. Journal of Climate and Applied Meteorology 23, 201213.Google Scholar
Wilson, R., Anchukaitis, K., Briffa, K.R., Büntgen, U., Cook, E., D'Arrigo, R., Davi, N., et al. , 2016. Last millennium Northern Hemisphere summer temperatures from tree rings: Part I, the long term context. Quaternary Science Reviews 134, 118.Google Scholar
Zhao, S., Pederson, N., D'Orangeville, L., HilleRisLambers, J., Boose, E., Penone, C., Bauer, B., Jiang, Y., Manzanedo, R.D., 2018. The International Tree Ring Data Bank (ITRDB) revisited: data availability and global ecological representativity. Journal of Biogeography (in press). https://doi.org/10.1111/jbi.13488.Google Scholar
Supplementary material: File

Alexander et al. supplementary material

Alexander et al. supplementary material 1

Download Alexander et al. supplementary material(File)
File 1.4 MB