Skip to main content
Log in

Precipitation reconstruction using ring-width chronology of himalayan cedar from western himalaya: Preliminary results

  • Published:
Journal of Earth System Science Aims and scope Submit manuscript

Abstract

Himalayan cedar (Cedrus deodara (D. Don) G. Don) due to its long age and wide ecological amplitude in the Himalayan region has strong dendroclimatic potential. A well replicated ring-width chronology of it, derived from the ensemble of tree-ring samples of two adjacent homogeneous sites, has been used to reconstruct precipitation for the non-monsoon months (previous year October to concurrent May) back to AD 1171. This provides the first record of hydrological conditions for the western Himalayan region, India during the whole of the ‘Little Ice Age’ and latter part of the ‘Medieval Warm Period’. The reconstruction revealed the wettest and the driest non-monsoon months during the fourteenth and the thirteenth centuries, respectively. The seventeenth century consistently recorded dry non-monsoon months in the western Himalayan region. Surplus precipitation, especially more pronounced since the 1950s, is recorded in the current century.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Barnett T P, Dumenil L, Schlese U, Roeckner E and Latif M 1989 The effect of Eurasian snow cover on regional and global climate variations;J. Atmos. Sci. 46 661–685

    Article  Google Scholar 

  • Borgaonkar H P, Pant G B and Rupa Kumar K 1994 Dendroclimatic reconstruction of summer precipitation at Srinagar, Kashmir, India since the late eighteenth century;The Holocene 4 299–306

    Article  Google Scholar 

  • Borgaonkar H P, Pant G B and Rupa Kumar K 1996 Ring-width variations inCedrus deodara and its climatic response over the western Himalaya;Int. J. Climatol. 16 1409–1422

    Article  Google Scholar 

  • Briffa K R, Jones P D and Schweingruber F H 1988 Summer temperature patterns over Europe: A reconstruction from 1750 A.D. based on maximum latewood density indices of conifers;Quat. Res. 30 36–52

    Article  Google Scholar 

  • Champion H G and Seth S K 1968A revised survey of the forest types of India; New Delhi

  • Dey B and Bhanukumar O S R U 1983 The Himalayan winter snow cover and summer monsoon rainfall over India;J. Geophys. Res. 88 5471–5474

    Article  Google Scholar 

  • Dhar O N, Kulkarni A K and Sangam R B 1984 Some aspects of winter and monsoon rainfall distribution over the Garhwal Kumaun Himalayas: A brief appraisal;Him. Res. Dev. 1 10–19

    Google Scholar 

  • Douville H and Royer J F 1996 Sensitivity of the Asian summer monsoon to an anomalous Eurasian snow cover within the Meteo-France GCM;Clim. Dyn. 12 449–466

    Article  Google Scholar 

  • Draper N R and Smith H 1981Applied regression analysis; 2nd edition (New York, USA: John Wiley and Sons)

    Google Scholar 

  • Fritts H C 1976Tree rings and climate; (New York: Academic Press)

    Google Scholar 

  • Hughes M K 1992 Dendroclimatic evidence from western Himalaya; In:Climate Since A.D. 1500 (eds) R S Bradley and P D Jones (London: Routledge) pp 415–431

    Google Scholar 

  • Hughes M K and Diaz H F 1994 Was there a ‘Medieval Warm Period’, if so, where and when;Clim. Change 26 109–142

    Article  Google Scholar 

  • Khandekar M L 1991 Eurasian snow cover, Indian monsoon and El Nino/Southern Oscillation — a synthesis;Atmosphere-Ocean 29 636–647

    Article  Google Scholar 

  • Lamb H H 1977Climate: Past, Present and Future;2 (London: Methuen)

    Google Scholar 

  • Overpeck J, Anderson D, Trumbore S and Prell W 1996 The southwest Indian monsoon over the last 18000 years;Clim. Dyn. 12 213–225

    Article  Google Scholar 

  • Pant G B 1979 Role of tree-ring analysis and related studies in palaeoclimatology: preliminary survey and scope for Indian region;Mausam 30 439–448

    Article  Google Scholar 

  • Pant G B 1983 Climatological signals from the annual growth rings of selected tree species in India;Mausam 34 251–256

    Article  Google Scholar 

  • Parthasarthy B, Munot A A and Kothawale D R 1994 All-India monthly and seasonal rainfall series: 1871–1993;Theor. Appl. Climatol. 49 217–224

    Article  Google Scholar 

  • Rothlisberger F and Geyh M A 1985 Glacier variations in the Himalayas and Karakorum. Zeitschr;Gletscher. Glazialgeol. 21 237–249

    Google Scholar 

  • Yadav R R 1998 Temperature variations in the western Himalayan region since late twelfth century AD as inferred from tree-rings; In:Dendrochronology and Environmental Trends, Proceedings of Eurodendro 1998, (eds) V Stravinskiene and R Juknys (Kaunas, Lithuania: Vytautas Magnus University) pp 288–294

    Google Scholar 

  • Yadav R R, Park W-K and Bhattacharyya A 1997 Dendroclimatic reconstruction of April–May temperature fluctuations in the Western Himalaya of India since A.D. 1698;Quat. Res. 48 187–191

    Article  Google Scholar 

  • Yadav R R, Park W-K and Bhattacharyya A 1999 Spring temperature variations in the western Himalaya, India as reconstructed from tree-rings: AD 1390-1987;The Holocene 9 85–90

    Article  Google Scholar 

  • Yang S 1996 ENSO-snow-monsoon associations and seasonal-interannual predictions;Int. J. Climatol. 16 125–134

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Yadav, R.R., Park, WK. Precipitation reconstruction using ring-width chronology of himalayan cedar from western himalaya: Preliminary results. J Earth Syst Sci 109, 339–345 (2000). https://doi.org/10.1007/BF02702206

Download citation

  • Received:

  • Revised:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02702206

Keywords

Navigation