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References

  • Bhati, J. P., and W.-P. Zingel (1997), Natural resource use pattern in the western Himalayan agriculture: Implications for biodiversity conservation and sustainable development, in Conservation and Economic Evaluation of Biodiversity, edited by P. Pushpangdan, K. Ravi, and V. Santhosh, pp. 575588, Oxford, New Delhi.
  • Bradley, R. S., and P. D. Jones (1993), Little Ice Age summer temperature variations: Their nature and relevance to recent global warming trends, Holocene, 3, 367376.
  • Braeuning, A. (2001), Climate history of Tibetan Plateau during the last 1000 years derived from a network of juniper chronologies, Dendrochronologia, 19, 127137.
  • Briffa, K. R., T. J. Osborn, F. H. Schweingruber, I. C. Harris, P. D. Jones, S. G. Shiyatov, and E. A. Vaganov (2001), Low frequency temperature variations from northern tree ring density network, J. Geophys. Res., 106, 29292941.
  • Briffa, K. R., T. J. Osborn, and F. H. Schweingruber (2004), Large-scale temperature inferences from tree rings: A review, Global Planet. Change, 40, 1126.
  • Cook, E. R., and L. A. Kairiukstis (Eds.) (1990), Methods of Dendrochronology: Applications in Environmental Sciences, Kluwer Acad., Norwell, Mass.
  • Cook, E. R., and K. Peters (1981), The smoothing spline: A new approach to standardizing forest interior tree-ring series for dendroclimatic studies, Tree Ring Bull., 41, 4553.
  • Cook, E. R., P. J. Krusic, and P. D. Jones (2003), Dendroclimatic signals in long tree-ring chronologies from the Himalayas of Nepal, Int. J. Climatol., 23, 707732.
  • Crowley, T. J. (2000), Causes of climate change over the past 1000 years, Science, 289, 270277.
  • D'Arrigo, R., G. Jacoby, M. Free, and A. Robock (1999), Northern Hemisphere temperature variability for the past three centuries: Tree ring and model estimates, Clim. Change, 42, 663675.
  • D'Arrigo, R., G. Jacoby, D. Frank, N. Pederson, E. Cook, B. Buckley, B. Nachin, R. Mijidorj, and C. Dugarjav (2001), 1738 years of Mongolian temperature variability inferred from a tree-ring width chronology of Siberian pine, Geophys. Res. Lett., 28, 543546.
  • Easterling, D. R., et al. (1997), Maximum and minimum temperature trends for the globe, Science, 277, 364367.
  • Esper, J., F. H. Schweingruber, and M. Winiger (2002a), 1300 years of climatic history for western Central Asia inferred from tree rings, Holocene, 12, 267277.
  • Esper, J., E. R. Cook, and F. H. Schweingruber (2002b), Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability, Science, 295, 22502253.
  • Esper, J., S. G. Shiyatov, V. S. Mazepa, R. J. S. Wilson, D. A. Graybill, and G. Funkhouser (2003), Temperature sensitive Tien Shan tree ring chronologies show multi-centennial growth trends, Clim. Dyn., 21, 699706.
  • Fritts, H. C. (1976), Tree-Rings and Climate, Academic, San Diego, Calif.
  • Grove, J. M. (1988), The Little Ice Age, Methuen, New York.
  • Hegerl, G. C., T. J. Crowley, S. K. Baum, K.-Y. Kim, and W. T. Hyde (2003), Detection of volcanic, solar and greenhouse gas signals in paleo-reconstructions of Northern Hemispheric temperature, Geophys. Res. Lett., 30(5), 1242, doi:10.1029/2002GL016635.
  • Hughes, M. K. (2001), An improved reconstruction of summer temperature at Srinagar, Kashmir since 1660 AD, based on tree-ring width and maximum latewood density of Abies pindrow [Royle] Spach, Palaeobotanist, 50, 1319.
  • Jones, P. D., and A. Moberg (2003), Hemispheric and large-scale surface air temperature variations: An extensive revision and an update to 2001, J. Clim., 16, 206223.
  • Kumar, K. R., K. K. Kumar, and G. B. Pant (1994), Diurnal asymmetry of surface temperature trends over India, Geophys. Res. Lett., 21, 677680.
  • Mann, M. E., and P. D. Jones (2003), Global surface temperatures over the past two millennia, Geophys. Res. Lett., 30(15), 1820, doi:10.1029/2003GL017814.
  • Mann, M. E., R. S. Bradley, and M. K. Hughes (1999), Northern Hemisphere temperatures during the past millennium: Inferences, uncertainties and limitations, Geophys. Res. Lett., 26, 759762.
  • Ministry of Environment and Forests (2000), State of the forest, Rep. 1999, Dehradun, India.
  • Negi, G. C. S. (2002), Hydrological research in the Indian Himalayan mountains: Soil and water conservation, Curr. Sci., 83, 974980.
  • Office of the Registrar General (2001), Census of India, New Delhi.
  • Rothlisberger, F., and M. A. Geyh (1985), Glacier variations in Himalayas and Karakorum, Z. Gletscherkd. Glazialgeol., 21, 237249.
  • Sen, K. K., R. L. Senwal, U. Rana, S. Nautiyal, R. K. Maikuri, K. S. Rao, and K. G. Saxena (2002), Patterns and implications of land use/cover change: A case study in Pranmati watershed (Garhawal Himalaya, India), Mt. Res. Dev., 22, 5662.
  • Wigley, T. M. L., K. R. Briffa, and P. D. Jones (1984), On the average value of correlated time series with applications in dendroclimatology and hydrometeorology, Int. J. Climatol., 8, 3354.
  • Wilson, R. J. S., and B. H. Luckman (2002), Tree-ring reconstruction of maximum and minimum temperatures and the diurnal temperature range in British Columbia, Canada, Dendrochronologia, 20, 257268.
  • Zhang, J., and T. J. Crowley (1989), Historical climate records in China and reconstruction of past climates (1470–1970), J. Clim., 2, 833849.