Trees

, 23:1321

Response of regional tree-line forests to climate change: evidence from the northeastern Tibetan Plateau

  • Keyan Fang
  • Xiaohua Gou
  • Fahu Chen
  • Jianfeng Peng
  • Rosanne D’Arrigo
  • William Wright
  • Mai-He Li
Original Paper
  • 252 Downloads

Abstract

Tree-ring width and age structure of Juniperus przewalskii (Qilian juniper) forests were analyzed for four tree-line sites in Qilian and Anyemaqen Mountains, northeastern Tibetan Plateau, to investigate their relationships to climate change. Tree-line growth on Qilian Mountain was mainly limited by temperature at the low-frequency band. However, tree-line growth in the Anyemaqen Mountain was highly correlated with the current growing season temperature at the high-frequency band, and with the previous growing season precipitation at the low-frequency band. A temperature-stressed growth pattern at colder western sites and a moisture-stressed growth pattern at the warm, drier eastern tree-line sites were detected. The number of surviving trees in the tree-line ecotone was not clearly correlated with temperature before the 1900s. An unprecedented rise in the number of trees coincided well with the rapid global warming after the 1900s.

Keywords

Tree ring Age structure Tree-line ecotone Climate–growth relationship Global warming Tree-line dynamics 

References

  1. Bekker MF (2005) Positive feedback between tree establishment and patterns of subalpine forest advancement, Glacier National Park, Montana, USA. Arc Antarct Alp Res 37(1):97–107CrossRefGoogle Scholar
  2. Callaghan TV, Werkman BR, Craford RMM (2002) The tundra–taiga interface and its dynamics: concepts and applications. Ambio Special Rep 12:6–14Google Scholar
  3. Camarero JJ, Gutiérrez E (2004) Pace and pattern of recent tree line dynamics: response of ecotones to climatic variability in the Spanish Pyrenees. Clim Chang 63:181–200CrossRefGoogle Scholar
  4. Cook ER (1985) A time-series analysis approach to tree-ring standardization. PhD dissertation, The University of Arizona, TucsonGoogle Scholar
  5. Cook ER, Kairiukstis LA (1990) Methods of dendrochronology: applications in the environmental sciences. Kluwer, DordrechtGoogle Scholar
  6. Cui H, Liu H, Dai J (2005) Mountain ecology and alpine tree-line research. Science Press, BeijingGoogle Scholar
  7. D’Arrigo R, Wilson R, Jacoby G (2006) On the long-term context for late twentieth century warming. J Geophys Res 111:D03103. doi: 10.1029/2005JD006352
  8. Dai AG, Trenberth KE, Qian T (2004) A global data set of palmer drought severity index for 1870–2002: relationship with soil moisture and effects of surface warming. J Hydrometeorol 5:1117–1130CrossRefGoogle Scholar
  9. Dalen L, Hofgaard A (2005) Differential regional treeline dynamics in the Scandes Mountains. Arc Antarct Alp Res 37(3):284–296CrossRefGoogle Scholar
  10. Esper J, Schweigruber FH (2004) Large-scale tree-line changes recorded in Siberia. Geophys Res Lett 31:L06202. doi:10.1029/2003GL019178 CrossRefGoogle Scholar
  11. Fang K, Gou X, Chen F, Yang M, Li J, He M, Zhang Y, Tian Q, Peng J (2009a) Drought variations in the eastern part of Northwest China over the past two centuries: evidence from tree rings. Clim Res 38:129–135CrossRefGoogle Scholar
  12. Fang K, Gou X, Delphis FL, Li J, Zhang F, Liu X, He M, Zhang Y, Peng J (2009b) Variations of radial growth patterns in trees along three altitudinal transects in north central China. J IAWA (in press)Google Scholar
  13. Fritts HC (1976) Tree ring and climate. Academic Press, LondonGoogle Scholar
  14. Goldblum D, Rigg LS (2005) Tree growth response to climate change at the deciduous-boreal forest ecotone, Ontario, Canada. Can J For Res 35:2709–2718CrossRefGoogle Scholar
  15. Gou X, Chen F, Jacoby G, Cook E, Yang M, Peng J, Zhang Y (2007) Rapid tree growth with respect to the last 400 years in response to climate warming, northeastern Tibetan Plateau. Int J Climatol 27:1497–1503CrossRefGoogle Scholar
  16. Harcombe PA (1987) Tree life table. Bioscience 37:557–568CrossRefGoogle Scholar
  17. Holloway JL Jr (1958) Smoothing and filtering of time series and space fields. In: Landsberg HE (ed) Advances of geophysics. Academic Press, New YorkGoogle Scholar
  18. Holmes RL (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree Ring Bull 43:69–95Google Scholar
  19. Hughes MK, Funkhouser G (2003) Frequency-dependent climate signal in upper and lower forest border tree rings in the mountains of the great basin. Clim Chang 59:233–244CrossRefGoogle Scholar
  20. Körner C (1998) A re-assessment of high elevation treeline positions and the explanation. Oecologia 115:445–459CrossRefGoogle Scholar
  21. Körner C (1999) Alpine plant life. Springer, BerlinGoogle Scholar
  22. Körner C, Paulsen J (2004) A world-wide study of high altitude treeline temperatures. J Biogeogr 31:713–732Google Scholar
  23. LaMarche VC (1974) Frequency-dependent relationships between tree-ring series along an ecological gradient and some dendroclimatic implications. Tree Ring Bull 34:1–20Google Scholar
  24. Lavoie C, Payette S (1994) Recent fluctuations of the lichen-spruce forest limite in subarctic Quebec. J Ecol 82:725–734CrossRefGoogle Scholar
  25. Leuschner C, Moser G, Bertsch C, Röderstein M, Hertel D (2007) Large altitudinal increase in tree root/shoot ratio in tropical mountain forests of Ecuador. Basic Appl Ecol 8:219–230CrossRefGoogle Scholar
  26. Li MH, Yang J (2004) Effects of elevation and microsite on growth of Pinus cembra in the subalpine zone of the Austrian Alps. Ann For Sci 61:319–325CrossRefGoogle Scholar
  27. Li MH, Yang J, Kräuchi N (2003) Growth responses of Picea abies and Larix deciduas to elevation in subalpine areas of Tyrol, Austria. Can J For Res 33(4):653–662CrossRefGoogle Scholar
  28. Li J, Cook ER, D’Arrigo R, Chen F, Gou X, Peng J, Huang J (2008) Common tree growth anomalies over the northeastern Tibetan Plateau during the last six centuries: Implications for regional moisture change. Global Chang Biol 14:2096–2107CrossRefGoogle Scholar
  29. Liang E, Shao X, Hu Y, Lin J (2001) Dendroclimatic evaluation of climate–growth relationships of Meyer spruce (Picea meyeri) on a sandy substrate in semi-arid grassland, north China. Trees Strut Funct 15:230–235Google Scholar
  30. Luckman BH, Kavanagh TA (1998) Documenting the effect of recent climate change at treeline in the Canadian Rockies. In: Beniston Innes JL (ed) The impacts of climate variability on forests. Springer, New York, pp 121–144Google Scholar
  31. Mäkinen H, Nöjd P, Kahle HP (2002) Radial growth variation of Norway spruce across latitudinal and altitudinal gradients in central and northern Europe. For Ecol Manag 171:243–259CrossRefGoogle Scholar
  32. Palmer WC (1965) Meteorological drought: Weather Bureau research paper 45. US Department of Commerce, Washington, DCGoogle Scholar
  33. Pederson N, Varner JM, Palik BJ (2008) Canopy disturbance and tree recruitment over two centuries in a managed longleaf pine landscape. For Ecol Manag 254:85–95CrossRefGoogle Scholar
  34. Peng J, Gou X, Chen F, Li J, Zhang Y, Fang K (2008) Difference in tree growth responses to climate at the upper treeline: a case study of Qilian juniper in the Anyemaqen Mountains. J Integr Plant Biol 50(8):982–990CrossRefPubMedGoogle Scholar
  35. Pfeifer K, Kofler W, Oberhuber W (2005) Climate related causes of distinct radial growth reductions in Pinus Cembra during the last 200 years. Veget Hist Archaeobot 14:211–220CrossRefGoogle Scholar
  36. Stokes MA, Smiley TL (1968) An introduction to tree ring dating. The University of Chicago Press, ChicagoGoogle Scholar
  37. Sveinbjörnsson B, Hofgaard A, Lloyd A (2002) Natural causes of the tundra–taiga boundary. Ambio Special Rep 12:23–29Google Scholar
  38. Takahashi K, Azuma H, Yasue K (2003) Effects of climate on the radial growth of tree species in the upper and lower distribution limits of an altitudinal ecotone on Mount Norikura, Central Japan. Ecol Res 18:549–558CrossRefGoogle Scholar
  39. Wang X, Zhang L, Fang J (2004) Geographical differences in alpine timberline and its climatic interpretation in China. Acta Geographia Sinica 59(6):871–879Google Scholar
  40. Wang N, Zhang C, Li G, Cheng H (2005a) Historic desertification process in Hexi corridor, China. Chinese Geogr Sci 15(3):245–253CrossRefGoogle Scholar
  41. Wang T, Ren H, Ma K (2005b) Climatic signals in tree ring of Picea schrenkiana along an altitudinal gradient in the central Tianshan Mountains, northwestern China. Trees Strut Funct 19:735–741Google Scholar
  42. Wang T, Zhang Q, Ma K (2006) Treeline dynamics in relation to climatic variability in the central Tianshan Mountains, northwestern China. Glob Ecol Biogeogr 15:406–415CrossRefGoogle Scholar
  43. Wigley T, Briffa KR, Jones PD (1984) On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. J Appl Meteorol 23:201–213CrossRefGoogle Scholar
  44. Yang B, Braeuning A, Johnson KR, Shi Y (2002) Temperature variation in China during the last two millennia. Geophys Res Lett 29(9):1324. doi: 10.1029/2001GL014485 CrossRefGoogle Scholar
  45. Zhou X, Wang Z (1987) Vegetation in Qinghai Province. Qinghai People’s Press, XiningGoogle Scholar

Copyright information

© Springer-Verlag 2009

Authors and Affiliations

  • Keyan Fang
    • 1
    • 2
  • Xiaohua Gou
    • 1
  • Fahu Chen
    • 1
  • Jianfeng Peng
    • 1
  • Rosanne D’Arrigo
    • 2
  • William Wright
    • 2
  • Mai-He Li
    • 3
    • 4
  1. 1.Key Laboratory of Western China’s Environmental Systems (MOE), Center for Arid Environment and Paleoclimate Research (CAEP)Lanzhou UniversityLanzhouChina
  2. 2.Tree-Ring LabLamont-Doherty Earth Observatory of Columbia UniversityNew YorkUSA
  3. 3.Tree Physiology DivisionSwiss Federal Research Institute WSLBirmensdorfSwitzerland
  4. 4.Mountain Ecology and Hydrology UnitInstitute of Mountain Hazards and Environment Chinese Academy of SciencesChengduChina

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