[go: up one dir, main page]
More Web Proxy on the site http://driver.im/ Skip to main content
Log in

Variability of climate–growth relationships along an elevation gradient in the Changbai Mountain, northeastern China

  • Original Paper
  • Published:
Trees Aims and scope Submit manuscript

Abstract

In order to explore climate–growth relationships at different elevations, tree-ring width chronologies of larch (Larix olgensis) were developed from three sampling sites on the northern slope of the Changbai Mountain, northeastern China. There were no consistent trends in statistical characteristics of the tree-ring chronologies along the elevation gradient, since trees in the forest interior had a complacent growth pattern. Monthly mean temperature and monthly total precipitation were used for the analysis. Correlation analysis indicated that temperatures in winter had negative correlations with tree growth (previous November, December and current March for the low-, mid- and high-elevation sites, respectively). The correlations between tree growth and June temperature varied from weakly negative at low elevations to significantly positive at high elevations. Precipitation in June of the growth year had negative relationship with the high-elevation chronology. However, high precipitation was associated with low temperature in early growing season, further supporting that temperature is a growth-limiting factor at high elevations. Our results suggest that along the elevation gradient, L. olgensis may respond in different ways to local climate change.

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

Access this article

Subscribe and save

Springer+ Basic
£29.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or eBook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

Price includes VAT (United Kingdom)

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4

Similar content being viewed by others

References

  • Barber VA, Juday GP, Finney BP, Wilmking M (2004) Reconstruction of summer temperatures in interior Alaska from tree-ring proxies: evidence for changing synoptic climate regimes. Clim Change 63:91–120

    Article  Google Scholar 

  • Bräuning A (1999) Dendroclimatological potential of drought-sensitive tree stands in southern Tibet for the reconstruction of monsoonal activity. IAWA J 20:325–338

    Google Scholar 

  • Camarero JJ, Guerrero-Campo J, Gutiérrez E (1998) Tree-ring growth and structure of Pinus uncinata and Pinus sylvestris in the central Spanish Pyrenees. Arct Alp Res 30:1–10

    Article  Google Scholar 

  • Cook ER, Holmes RL (1996) Guide for computer program ARSTAN. In: Grissino-Mayer HD, Holmes RL, Fritts HC (eds) The international tree-ring data bank program library version 2.0 user’s manual. University of Arizona, Tucson

    Google Scholar 

  • Cook E, Briffa K, Shiyatov S, Mazepa V (1990) Tree-ring standardization and growth-trend estimation. In: Cook E, Kairiukstis LA (eds) Methods of dendrochronology: applications in the environmental sciences. Kluwer Academic Publishers, Dordrecht, pp 104–123

    Google Scholar 

  • Dittmar C, Zech W, Elling W (2003) Growth variation of common beech (Fagus sylvatica L.) under different climatic and environmental conditions in Europe–a dendroecological study. For Ecol Manag 173:63–78

    Article  Google Scholar 

  • ECJF (Editorial Committee of Jilin Forest) (1988) Jilin forest. Jilin Technology and Science Publishing House; China Forestry Publishing House, Beijing (in Chinese)

  • ECVC (Editorial Committee for Vegetation of China) (1980) Vegetation of China. Science Press, Beijing (in Chinese)

    Google Scholar 

  • Fan Z, Bräuning A, Cao K et al (2009) Growth-climate responses of high-elevation conifers in the central Hengduan Mountains, southwestern China. For Ecol Manag 258:306–313

    Article  Google Scholar 

  • Fritts HC (1965) Tree-ring evidence for climatic changes in western North America. Mon Weather Rev 93:421–443

    Article  CAS  Google Scholar 

  • Frrits HC (1976) Tree rings and climate. Academic Press, London

    Google Scholar 

  • Gervais BR, MacDonald GM (2000) A 403-year record of July temperatures and treeline dynamics of Pinus sylvestris from the Kola Peninsula, northwest Russia. Arct Antarct Alp Res 32:295–302

    Article  Google Scholar 

  • Gostev M, Wiles G, D’Arrigo R, Jacoby G, Khomentovsky P (1996) Early summer temperatures since 1670 A.D. for central Kamchatka reconstructed based on a Siberian larch tree-ring width chronology. Can J For Res 26:2048–2052

    Article  Google Scholar 

  • Holmes RL (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bull 43:69–78

    Google Scholar 

  • Institute of Environment Protection of Jilin (1988) Exploring natural resources and protecting the ecological environment in Changbaishan area. Jilin Technology and Science Publishing House, Changchun

    Google Scholar 

  • Kendall M, Gibbons JD (1990) Rank correlation methods, Fifth edn. Arnold, London

    Google Scholar 

  • Kienast F, Schweingruber FH, Bräker OU et al (1987) Tree-ring studies on conifers along gradients and the potential of single-year analyses. Can J For Res 17:683–696

    Article  Google Scholar 

  • Kullman L (1993) Tree limit dynamics of Betula pubescens ssp. tortuosa in relation to climate variability: evidence from central Sweden. J Vegetation Sci 4:765–772

    Article  Google Scholar 

  • Liang E, Wang Y, Xu Y et al (2010) Growth variation in Abies georgei var. smithii along altitudinal gradients in the Sygera Mountains, southeastern Tibetan Plateau. Trees 24:363–373

    Article  Google Scholar 

  • Pederson N, Cook ER, Jacoby GC et al (2004) The influence of winter temperatures on the annual radial growth of six northern range margin tree species. Dendrochronologia 22:7–29

    Article  Google Scholar 

  • Peterson DW, Peterson DL (1994) Effects of climate on radial growth of subalpine conifers in the North Cascade Mountains. Can J For Res 24:1921–1932

    Article  Google Scholar 

  • Peterson DW, Peterson DL (2001) Mountain hemlock growth responds to climatic variability at annual and decadal time scales. Ecology 82:3330–3345

    Article  Google Scholar 

  • Pilcher JR, Gray B (1982) The relationships between oak tree growth and climate in Britain. J Ecol 70:297–304

    Article  Google Scholar 

  • Rolland C (1993) Tree-ring and climate relationships for Abies alba in the internal Alps. Tree-Ring Bull 53:1–11

    Google Scholar 

  • Savva Y, Oleksyn J, Reich PB et al (2006) Interannual growth response of Norway spruce to climate along an altitudinal gradient in the Tatra Mountains, Poland. Trees 2006(20):735–746

    Article  Google Scholar 

  • Serre F (1978) The dendroclimatological value of the European larch (larix deciduas Mill.) in the French Maritime Alps. Tree-Ring Bull 1978(38):25–34

    Google Scholar 

  • Shao X, Wu X (1997) Reconstruction of climate change on Changbai Mountain, northeast China using tree-ring data. Quat Sci 1:76–85 (in Chinese with English summary)

    Google Scholar 

  • Splechtna BE, Dobry J, Klinka K (2000) Tree-ring characteristics of subalpine fir (Abies lasiocarpa (Hook.) Nutt.) in relation to elevation and climatic fluctuations. Ann Forest Sci 57:89–100

    Article  Google Scholar 

  • Stokes MA, Smiley TL (1968) An introduction to tree-ring dating. University of Arizona Press, Tucson

    Google Scholar 

  • Takahashi K, Tokumitsu Y, Yasue K (2005) Climate factors affecting the tree-ring width of Betula ermanii at the timberline on Mount Norikura, central Japan. Ecol Res 20:445–451

    Article  Google Scholar 

  • Wang M, Tao D (1998) Drought-tolerance of main tree species in Changbai Mountain. Chin J Appl Ecol 9(1):7–10 (in Chinese with English summary)

    Google Scholar 

  • Wang Z, Xu Z, Li X et al (eds) (1980) Major forest types and the community structure characteristics in the northern slope of Changbai Mountain (I). In: Forest ecosystem study. China Forestry Publishing House, Beijing, pp 25–42 (in Chinese)

  • Wigley T, Briffa KR, Jones PD (1984) On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. J Clim Appl Meteorol 23:201–213

    Article  Google Scholar 

  • Wu X, Shao X (1996) A preliminary study on impact of climate change on tree growth using tree ring-width data. Acta Geographica Sinica 51(supplement):92–101 (in Chinese with English summary)

    Google Scholar 

  • Yu D, Wang S, Tang L et al (2005) Relationship between tree ring chronology of Larix olgensis in Changbai Mountains and the climate change. Chin J Appl Ecol 16(1):14–20 (in Chinese with English summary)

    Google Scholar 

  • Zhou K, Yan F, Ye Y (1984) Surface pollen assemblages of different vegetation zones in the northern slope of the Changbai Mountain. In: Institute of Geology, the Chinese Academy of Sciences, Tongji University (eds) Quaternary pollen analysis and environment. Science Press, Beijing, pp 115–122 (in Chinese)

  • Zhu H (2006) A temperature reconstruction for eastern part of northeast China based on a tree ring width network. PhD dissertation, Beijing Normal University, Beijing (in Chinese with English summary)

  • Zhu H, Fang X, Shao X et al (2009) Tree ring-based February–April temperature reconstruction for Changbai Mountain in Northeast China and its implication for East Asian winter monsoon. Clim Past 5:661–666

    Article  Google Scholar 

Download references

Acknowledgments

This research was supported by the National Natural Science Foundation of China (NSFC 40771016). We thank Prof Xuemei Shao, Prof Zhiyong Yin, Dr Dongsheng Zhao, Dr Hui Wang, and Dr Peng Xu for their help in field work. We thank Prof Zhiyong Yin for his help in English improvement of the manuscript.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Shaohong Wu.

Additional information

Communicated by A. Braeuning.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Chen, L., Wu, S. & Pan, T. Variability of climate–growth relationships along an elevation gradient in the Changbai Mountain, northeastern China. Trees 25, 1133–1139 (2011). https://doi.org/10.1007/s00468-011-0588-0

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00468-011-0588-0

Keywords