Abstract
Dendroecological techniques were employed to explore the growth response of subalpine fir (Abies fargesii) to climatic conditions across its altitudinal range in both the north and south aspects in the Shennongjia Mountains, central China. Correlation function analyses indicated that temperatures in current summer were significantly negatively correlated with fir radial growth at the lower limits, while temperatures in previous autumn and in current spring showed significantly positive correlations with fir radial growth at the mid- and high-elevations in both aspects. Radial growth of the subalpine fir was significantly and positively influenced by precipitation in previous autumn and in current spring at the lower elevations and by precipitation in current spring at the mid-elevations, while precipitation had no significant effects on its radial growth at the upper elevations. Moving correlation functions showed that temperatures in early spring of the current year (i.e., February-April) had a relatively stable effect on tree growth over time at the mid- and upper-elevations in both aspects. Thus, the growth of the subalpine fir responded differently to climatic conditions along the altitudinal gradient, showing that the importance of temperatures for the fir radial growth increased while the importance of precipitation decreased with increasing altitude in both aspects in the Shennongjia Mountains, central China.
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References
Biondi F, Waikul K (2004) DENDROCLIM2002: a C++ program for statistical calibration of climate signals in tree-ring chronologies. Comput Geosci 30:303–311
Brubaker LB (1986) Responses of tree populations to climatic change. Plant Ecol 67:119–130
Buckley BM, Cook ER, Peterson MJ, Barbetti M (1997) A changing temperature response with elevation for Lagarostrobos franklinii in Tasmania, Australia. Clim Chang 36:477–498
Carrer M, Urbinati C (2006) Long-term change in the sensitivity of tree-ring growth to climate forcing in Larix decidua. New Phytol 170:861–872
Case MJ, Peterson DL (2005) Fine-scale variability in growth-climate relationships of Douglas-fir, North Cascade Range, Washington. Can J For Res 35:2743–2755
Cienciala E, Lindroth A, Cermak J, Haellgren JE, Kucera J (1994) The effects of water availability on transpiration, water potential and growth of Picea abies during a growing season. J Hydrol 155:57–71
Cook ER (1985) A time series analysis approach to tree ring standardization. University of Arizona, Tucson, AZ
Cook E, Kairiukstis L (1990) Methods of dendrochronology: applications in the environmental sciences. Kluwer Academic Publishers, Dordrecht
Dang H, Jiang M, Zhang Q, Zhang Y (2007) Growth responses of subalpine fir (Abies fargesii) to climate variability in the Qinling Mountain, China. For Ecol Manag 240:143–150
Dang H, Jiang M, Zhang Y, Dang G, Zhang Q (2009) Dendroecological study of a subalpine fir (Abies fargesii) forest in the Qinling Mountains, China. Plant Ecol 201:67–75
Di Filippo A, Biondi F, Cufar K, de Luis M, Grabner M, Maugeri M, Saba E, Schirone B, Piovesan G (2007) Bioclimatology of beech (Fagus sylvatica L.) in the Eastern Alps: spatial and altitudinal climatic signals identified through a tree-ring network. J Biogeogr 34:1873–1892
Ettl GJ, Peterson DL (1995) Growth response of subalpine fir (Abies lasiocarpa) to climate in the Olympic Mountains, Washington, USA. Glob Chang Biol 1:213–230
Fritts HC (1976) Tree rings and climate. Academic, London
Fritts HC, Swetnam TW (1989) Dendroecology: a tool for evaluating variations in past and present forest environments. Adv Ecol Res 19:111–188
Fritts HC, Smith DG, Cardis JW, Budelsky CA (1965) Tree-ring characteristics along a vegetation gradient in northern Arizona. Ecology 46:393–401
Glassy JM, Running SW (1994) Validating diurnal climatology logic of the MT-CLIM model across a climatic gradient in Oregon. Ecol Appl 4:248–257
Guiot J (1991) The bootstrapped response function. Tree-Ring Bull 51:39–41
Havranek WM, Benecke U (1978) The influence of soil moisture on water potential, transpiration and photosynthesis of conifer seedlings. Plant Soil 49:91–103
Holmes RL (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bull 43:69–78
Holmes RL (1994) Dendrochronology program library, version 1994. Laboratory of Tree-Ring Research, University of Arizona, Tucson
Hughes MK, Wu X, Shao X, Garfin GM (1994) A Preliminary reconstruction of rainfall in North-Central China since AD 1600 from tree-ring density and width. Quat Res 42:88–89
Jackson DA (1993) Stopping rules in principal components analysis: a comparison of heuristical and statistical approaches. Ecology 74:2204–2214
Jump AS, Hunt JM, Penuelas J (2007) Climate relationships of growth and establishment across the altitudinal range of Fagus sylvatica in the Montseny Mountains, northeast Spain. Ecoscience 14:507–518
Kaiser HF (1992) On Cliff’s formula, the Kaiser-Guttman rule, and the number of factors. Percept Mot Ski 74:595–598
Kienast F, Schweingruber FH, Braeker OU, Schaer E (1987) Tree-ring studies on conifers along ecological gradients and the potential of single-year analyses. Can J For Res 17:683–696
Lara A, Aravena JC, Villalba R, Wolodarsky-Franke A, Luckman B, Wilson R (2001) Dendroclimatology of high-elevation Nothofagus pumilio forests at their northern distribution limit in the central Andes of Chile. Can J For Res 31:925–936
Leonelli G, Pelfini M, Battipaglia G, Cherubini P (2009) Site-aspect influence on climate sensitivity over time of a high-altitude Pinus cembra tree-ring network. Clim Chang 96:185–201
Liu HB, Shao XM (2003) Reconstruction of January to April mean temperature at Qinling Mts from 1789 to 1992 using tree ring chronologies. J Appl Meteorol Sci 14:188–196
Liu Y, Ma LM, Hughes MK, Garfin-wool GM, Cai QF, An ZS, Leavitt SW (2001) Seasonal temperature reconstruction from central China based on tree ring data. Palaeobotanist 50:89–94
Lo YH, Blanco JA, Seely B, Welham C, Kimmins JP (2011) Generating reliable meteorological data in mountainous areas with scarce presence of weather records: the performance of MTCLIM in interior British Columbia, Canada. Environ Model Softw 26:644–657
Mäkinen H, Nöjd P, Kahle HP, Neumann U, Tveite B, Mielikäinen K, Röhle H, Spiecker H (2002) Radial growth variation of Norway spruce (Picea abies (L.) Karst.) across latitudinal and altitudinal gradients in central and northern Europe. For Ecol Manag 171:243–259
Mayer D, Butler D (1993) Statistical validation. Ecol Model 68:21–32
Miller BJ, Clinton PW, Buchan GD, Robson AB (1998) Transpiration rates and canopy conductance of Pinus radiata growing with different pasture understories in agroforestry systems. Tree Physiol 18:575–582
Peterson DW, Peterson DL, Ettl GJ (2002) Growth responses of subalpine fir to climatic variability in the Pacific Northwest. Can J For Res 32:1503–1517
Piovesan G, Biondi F, Bernabei M, Di Filippo A, Schirone B (2005) Spatial and altitudinal bioclimatic zones of the Italian peninsula identified from a beech (Fagus sylvatica L.) tree-ring network. Acta Oecol 27:197–210
Running SW, Nemani RR, Hungerford RD (1987) Extrapolation of synoptic meteorological data in mountainous terrain and its use for simulating forest evaporation and photosynthesis. Can J For Res 17:472–483
Savva Y, Oleksyn J, Reich PB, Tjoelker MG, Vaganov EA, Modrzynski J (2006) Interannual growth response of Norway spruce to climate along an altitudinal gradient in the Tatra Mountains, Poland. Trees Struct Funct 20:735–746
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 For Sci 57:89–100
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 18:549–558
Thornton PE, Running SW, White MA (1997) Generating surfaces of daily meteorological variables over large regions of complex terrain. J Hydrol 190:214–251
Villalba R, Boninsegna JA, Veblen TT, Schmelter A, Rubulis S (1997) Recent trends in tree-ring records from high elevation sites in the Andes of Northern Patagonia. Clim Chang 36:425–454
Wang T, Ren HH, Ma KP (2005) Climatic signals in tree ring of Picea schrenkiana along an altitudinal gradient in the central Tianshan Mountains, northwestern China. Trees Struct Funct 19:736–742
White TL (1987) Drought tolerance of southwestern Oregon Douglas-fir. For Sci 33:283–293
Wilmking M, Juday GP, Barber VA, Zald HSJ (2004) Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds. Glob Chang Biol 10:1724–1736
Wilson RJS, Hopfmueller M (2001) Dendrochronological investigations of Norway spruce along an elevational transect in the Bavarian Forest, Germany. Dendrochronologia 19:67–79
Wu XD, Shao XM (1994) A preliminary analysis on response of tree-ring density to climate in the Qinling Mountains of China. Quart J Appl Meteorol 5:253–256
Yoo SJ, Wright BD (2000) Persistence of growth variation in tree-ring chronologies. For Sci 46:507–520
Zhang QB, Hebda RJ (2004) Variation in radial growth patterns of Pseudotsuga menziesii on the central coast of British Columbia, Canada. Can J For Res 34:1946–1954
Zhang Q, Jiang M, Chen F (2007) Canopy recruitment in the beech (Fagus engleriana) forest of Mt. Shennongjia, Central China. J For Res 12:63–67
Acknowledgments
This research was supported by the National Natural Science Foundation of China (31270011, 31130010), the Chinese Academy of Sciences (KSCX2-EW-Q-16, XDA05090305), the National Key Technology R&D Program (2011BAD31B02), and the China Meteorological Administration (CCSF-10-04). We would like to thank anonymous reviewers for their comments and suggestions.
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Dang, H., Zhang, Y., Zhang, K. et al. Climate-growth relationships of subalpine fir (Abies fargesii) across the altitudinal range in the Shennongjia Mountains, central China. Climatic Change 117, 903–917 (2013). https://doi.org/10.1007/s10584-012-0611-5
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DOI: https://doi.org/10.1007/s10584-012-0611-5