• Biondi, F., A. Gershuno, and D. R. Cayan (2001), North Pacific decadal climate variability since AD 1661, J. Clim., 14, 510.
  • Cook, E. R., K. R. Briffa, S. G. Shiyatov, and V. S. Mazepa (1990), Tree-ring standardization and growth-trend estimation, in Methods of Dendrochronology, edited by E. R. Cook, and L. A. Kairiukstis, pp. 104123, Springer, New York.
  • Cook, E. R., K. R. Briffa, D. M. Meko, D. A. Graybill, and G. Funkhouser (1995), The ‘segment length curse’ in long tree-ring chronology development for palaeoclimatic studies, Holocene, 5, 229237.
  • Dalfes, N. H., G. Kukla, and H. Weiss (1997), Third Millennium BC Climate Change and Old World Collapse, Springer, New York.
  • Gasse, F. (2000), Hydrological changes in the African tropics since the Last Glacial Maximum, Quat. Sci. Rev., 19, 189211.
  • Gedalof, Z., and D. J. Smith (2001), Interdecadal climate variability and regime-scale shifts in Pacific North America, Geophys. Res. Lett., 28, 15151518.
  • Gershunov, A., and T. P. Barnett (1998), Interdecadal modulation of ENSO teleconnections, Bull. Am. Meteorol. Soc., 79, 27152726.
  • Hebda, R. J. (1995), British Columbia vegetation and climate history with focus on 6 ka BP, Geogr. Phys. Quat., 49, 5579.
  • Hebda, R. J., and R. W. Mathewes (1984), Holocene history of cedar and native cultures of the North American Pacific Coast, Science, 225, 711713.
  • Hughes, M. K., and H. F. Diaz (1994), Was there a ‘Medieval Warm Period’, and if so, where and when? Clim. Change, 26, 109142.
  • Latif, M., and T. P. Barnett (1994), Causes of decadal climate variability over the North Pacific and North America, Science, 266, 634637.
  • Leuschner, H. H., U. S. Klaassen, E. Jansma, M. G. L. Baillie, and M. Spurk (2002), Subfossil European bog oaks: Population dynamics and long-term growth depressions as indicator of changes in the Holocene hydro-regime and climate, Holocence, 12, 695706.
  • Mantua, N. J., and S. R. Hare (2002), The Pacific decadal oscillation, J. Oceanogr., 58, 3544.
  • Minobe, S. (1999), Resonance in bidecadal and pentadecadal climate oscillations over the North Pacific: Role in climatic regime shifts, Geophys. Res. Lett., 26, 855858.
  • Moy, C. M., G. O. Seltzer, D. T. Rodbell, and D. M. Anderson (2002), Variability of El Niño/Southern Oscillation activity at millennial timescales during the Holocene epoch, Nature, 420, 162165.
  • Nederbragt, A. J., and J. W. Thurow (2001), A 6000 yr varve record of Holocene climate in Saanich Inlet, British Columbia, from digital sediment color analysis of ODP Leg 169S cores, Mar. Geol., 174, 95110.
  • Newman, M., G. P. Compo, and M. A. Alexander (2003), ENSO-forced variability of the Pacific decadal oscillation, J. Clim., 16, 38533857.
  • Schwalb, A., W. E. Dean, and B. Kromer (2003), Centennial drought cyclicity in the Great Plains, USA: A dominant climate pattern over the past 4000 years, Geophys. Res. Abstr. 5, abstract 11580.
  • Stokes, M. A., and T. L. Smiley (1996), An Introduction to Tree-Ring Dating, Univ. of Ariz. Press, Tucson.
  • Torrence, C., and G. P. Compo (1998), A practical guide to wavelet analysis, Bull. Am. Meteorol. Soc., 79, 6178.
  • Weiss, H. (2000), Beyond the Younger Dryas, in Confronting Natural Disaster: Engaging the Past to Understand the Future, edited by G. Bawden, and R. Reycraft, pp. 7598, Univ. of N. M. Press, Albuquerque.
  • Weiss, H., M.-A. Courty, W. Wetterstrom, F. Guichard, L. Senior, R. Meadow, and A. Curnow (1993), The genesis and collapse of third millennium north Mesopotamian civilization, Science, 261, 9951004.
  • Woodhouse, C. A., and J. T. Overpeck (1998), 2000 years of drought variability in the central United States, Bull. Am. Meteorol. Soc., 79, 26932714.
  • Zhang, Q.-B., and R. J. Hebda (2004), Variation in radial growth patterns of Pseudotsuga menziesii on the central coast of British Columbia, Canada, Can. J. For. Res., 34, 19461954.
  • Zhang, Q.-B., R. J. Hebda, Q.-J. Zhang, and R. I. Alfaro (2000), Modeling tree-ring growth responses to climatic variables using artificial neural networks, For. Sci., 46, 229239.