Larix olgensis growth–climate response between lower and upper elevation limits: an intensive study along the eastern slope of the Changbai Mountains, northeastern China

Jian Yu , Qijing Liu

Journal of Forestry Research ›› 2018, Vol. 31 ›› Issue (1) : 231 -244.

PDF
Journal of Forestry Research ›› 2018, Vol. 31 ›› Issue (1) : 231 -244. DOI: 10.1007/s11676-018-0788-1
Original Paper

Larix olgensis growth–climate response between lower and upper elevation limits: an intensive study along the eastern slope of the Changbai Mountains, northeastern China

Author information +
History +
PDF

Abstract

Larix olgensis is a dominant tree species in the forest ecosystems of the Changbai Mountains of northeast China. To assess the growth response of this species to global climate change, we developed three tree-ring width and biomass chronologies across a range of elevations in the subalpine forests on the eastern slope of the Changbai Mountains. We used dendroclimatic analyses to study key factors limiting radial growth in L. olgensis and its variation with elevation. The statistical characteristics of chronologies suggested that elevation is a determinant of tree growth patterns in the study area. Response function analysis of chronologies with climate factors indicated that climate–growth relationships changed with increasing elevation: tree growth at high elevation was strongly limited by June temperatures of the previous year, and as elevation decreases, the importance of temperature decreased; tree radial growth at mid-elevation was mainly controlled by precipitation towards the end of the growing season of the current year. Biomass chronologies reflected a stronger climatic signal than tree-ring width chronologies. Spatial correlation with gridded climate data revealed that our chronologies contained a strong regional temperature signal for northeast China. Trees growing below timberline appeared to be more sensitive to climate, thus optimal sites for examining growth trends as a function of climate variation are considered to be just below timberline. Our study objective was to provide information for more accurate prediction of the growth response of L. olgensis to future climate change on the eastern slope of the Changbai Mountains, and to provide information for future climate reconstructions using this tree species in humid and semi humid regions.

Keywords

Tree-ring width / Dendrochronology / Changbai Mountains / Elevation gradient / Timberline / Larix olgensis

Cite this article

Download citation ▾
Jian Yu, Qijing Liu. Larix olgensis growth–climate response between lower and upper elevation limits: an intensive study along the eastern slope of the Changbai Mountains, northeastern China. Journal of Forestry Research, 2018, 31(1): 231-244 DOI:10.1007/s11676-018-0788-1

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

Andreassen K, Solberg S, Tveito OE, Lystad SL. Regional differences in climatic responses of Norway spruce (Picea abies L. Karst) growth in Norway. For Ecol Manag, 2006, 222: 211-221.

[2]

Asad F, Zhu HF, Zhang H, Liang EY, Muhammad S, Farhan SB, Hussain I, Wazir MA, Ahmed M, Esper J. Are Karakoram temperatures out of phase compared to hemispheric trends?. Clim Dyn, 2016, 48: 3381-3390.

[3]

Biondia F, Waikulb K. DENDROCLIM2002: a C++ program for statistical calibration of climate signals in tree-ring chronologies. Comput Geosci, 2004, 30: 303-311.

[4]

Cai QF, Liu Y. Climatic response of three tree species growing at different elevations in the Lüliang Mountains of Northern China. Dendrochronologia, 2013, 31: 311-317.

[5]

Chen L, Wu SH, Pan T. Variability of climate–growth relationships along an elevation gradient in the Changbai Mountain, northeastern China. Trees, 2011, 25: 1133-1139.

[6]

Chen F, Yuan YJ, Wei WS, Fan ZA, Zhang TW, Shang HM, Zhang RB, Yu SL, Ji CR, Qin L. Climatic response of ring width and maximum latewood density of Larix sibirica in the Altay Mountains, reveals recent warming trends. Ann For Sci, 2012, 69: 723-733.

[7]

Cook E, Holmes R (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

[8]

Cullen L, Palmer J, Duncan R, Stewart G. Climate change and tree-ring relationships of Nothofagus menziesii tree-line forests. Can J For Res, 2001, 31: 1981-1991.

[9]

D’Arrigo R, Wilson R, Wiles G, Anchukaitis K, Solomina O, Davi N, Deser C, Dolgova E. Tree-ring reconstructed temperature index for coastal northern Japan: implications for western North Pacific variability. Int J Climatol, 2015, 35: 3713-3720.

[10]

Dai A, Trenberth K, Qian TT. A global dataset of Palmer drought severity index for 1870–2002: relationship with soil moisture and effects of surface warming. J Hydrometeorol, 2004, 5: 1117-1130.

[11]

Dai L, Wu YX, Han SJ, Li YW. Effect of great volcanic eruption on historical vegetation succession on eastern slope of Changbai Mountains. Chin J Ecol, 2008, 27: 1771-1778. (in Chinese with English abstract)

[12]

Dang HS, Zhang YJ, Zhang KR, Jiang MX, Zhang QF. Climate-growth relationships of subalpine fir (Abies fargesii) across the altitudinal range in the Shennongjia Mountains, central China. Clim Change, 2013, 117: 903-917.

[13]

Davi N, Arrigo RD, Jacoby G, Cook E, Anchukaitis K, Nachin B, Rao M, Leland C. A long-term context (931–2005 C.E.) for rapid warming over Central Asia. Quat Sci Rev, 2015, 121: 89-97.

[14]

Dulamsuren C, Hauck M, Leuschner H, Leuschner C. Climate response of tree-ring width in Larix sibirica growing in the drought-stressed forest-steppe ecotone of northern Mongolia. Ann For Sci, 2011, 68: 275-282.

[15]

Fang OY, Wang Y, Shao XM. The effect of climate on the net primary productivity (NPP) of Pinus koraiensis in the Changbai Mountains over the past 50 years. Trees, 2015, 30: 281-294.

[16]

Fritts H. Tree rings and climate, 1976, London: Academic Press.

[17]

Gao LL, Gou XH, Deng Y, Liu WH, Yang MX, Zhao ZQ. Climate–growth analysis of Qilian juniper across an altitudinal gradient in the central Qilian Mountains, northwest China. Trees, 2013, 27: 379-388.

[18]

Gou X, Chen F, Yang M, Li J, Peng J, Jin L. Climatic response of thick leaf spruce (Picea crassifolia) tree-ring width at different elevations over Qilian Mountains, northwestern China. J Arid Environ, 2005, 61: 513-524.

[19]

Grinsted A, Moore JC, Jevrejeva S. Application of the cross wavelet transform and wavelet coherence to geophysical time series. Nonlinear Proc Geophys, 2004, 11: 561-566.

[20]

He MH, Yang B, Brauning A. Tree growth–climate relationships of Juniperus tibetica along an altitudinal gradient on the southern Tibetan Plateau. Trees, 2013, 27: 429-439.

[21]

Holmes R. Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bull, 1983, 43: 69-95.

[22]

Jiang YG, Zhang JH, Han SJ, Chen ZJ, Setälä H, Yu JH, Zheng XB, Guo YT, Gu Y. Radial growth response of Larix gmelinii to climate along a latitudinal gradient in the Greater Khingan Mountains, Northeastern China. Forests, 2016, 7: 295.

[23]

Kharal D, Thapa U, George S, Meilby H, Rayamajhi S, Bhuju D. Tree-climate relations along an elevational transect in Manang Valley, central Nepal. Dendrochronologia, 2017, 41: 57-64.

[24]

King G, Gugerli F, Fonti P, Frank D. Tree growth response along an elevational gradient: climate or genetics?. Oecologia, 2013, 173: 1587-1600.

[25]

Korner C, Paulsen J. A world-wide study of high altitude treeline temperatures. J Biogeogr, 2004, 31: 713-732.

[26]

Liang EY, Wang YF, Xu Y, Liu B, Shao XM. Growth variation in Abies georgei var. smithii along altitudinal gradients in the Sygera Mountains, southeastern Tibetan Plateau. Trees, 2010, 24: 363-373.

[27]

Liang EY, Dawadi B, Pederson N, Eckstein D. Is the growth of birch at the upper timberline in the Himalayas limited by moisture or by temperature?. Ecology, 2014, 95: 2453-2465.

[28]

Lin B, Xu QQ, Liu WH, Zhang GC, Xu QY, Liu QJ. Dendrochronology-based stand growth estimation of Larix olgensis forest in relation with climate on the eastern slope of Changbai Mountain, NE China. Front Earth Sci, 2013, 7: 429-438.

[29]

Liu QJ, Wang Z, Wang SX. Effects of recent volcanic eruptions on alpine and subalpine vegetation in the Changbai Mountain. Sci Geogr Sin, 1993, 13: 57-61. (in Chinese with English abstract)

[30]

Liu QJ, Kondoh A, Takeuchi N. The forest vegetation and its differentiation under disturbance in a temperate mountain, China. J For Res, 1998, 3: 111-117.

[31]

Liu JJ, Qin C, Kang SY. Growth response of Sabina tibetica to climate factors along an elevation gradient in south Tibet. Dendrochronologia, 2013, 31: 255-265.

[32]

Lo Y, Blanco J, Seely B, Welham C, Kimmins J. Relationships between climate and tree radial growth in interior British Columbia, Canada. For Ecol Manag, 2010, 259: 932-942.

[33]

McIntire E, Piper F, Fajardo A. Wind exposure and light exposure, more than elevation-related temperature, limit tree line seedling abundance on three continents. J Ecol, 2016, 104: 1379-1390.

[34]

Norton D. Tuner H, Tranquillini W. A dendrochronological study of Nothofagus solandri tree growth along an elevational gradient, South Islang, New Zealand. Establishment and tending of subalpine forests: research and management, 1985, Berichte: Eidgenössische Anstalt für das forstliche Versuchswesen.

[35]

Peng JF, Gou XH, Chen FH, Li JB, Liu PX, Zhang Y. Altitudinal variability of climate–tree growth relationships along a consistent slope of Anyemaqen Mountains, northeastern Tibetan Plateau. Dendrochronologia, 2008, 26: 87-96.

[36]

Shao XM, Wu XD. Reconstruction of climate change on Changbai Mountains, northeast China using tree-ring data. Quat Sci, 1997, 1: 76-85. (in Chinese with English abstract)

[37]

Shen CC, Wang LL, Li MY. The altitudinal variability and temporal instability of the climate–tree-ring growth relationships for Changbai larch (Larix olgensis Henry) in the Changbai mountains area, Jilin, Northeastern China. Trees, 2015, 30: 901-912.

[38]

Shi JF, Li JB, Cook ER, Xy Z, Lu HY. Growth response of Pinus tabulaeformis to climate along an elevation gradient in the eastern Qinling Mountains, central China. Clim Res, 2012, 53: 157-167.

[39]

Sidor CG, Vlad R, Popa I, Cherubini P. Different tree-ring responses of Norway spruce to air temperature across an altitudinal gradient in the Eastern Carpathians (Romania). Trees, 2015, 29: 985-997.

[40]

Stokes M, Smiley T. An introduction to tree-ring dating, 1968, Tucson: University of Arizona Press.

[41]

Toledo M, Poorter L, Pena-Claros M, Alarcon A, Balcazar J, Leano C, Licona JC, Llanque O, Vroomans V, Zuidema P, Bongers F. Climate is a stronger driver of tree and forest growth rates than soil and disturbance. J Ecol, 2011, 99: 254-264.

[42]

Wang XD, Liu HQ. Responses of tree islands to air temperature change at treeline on north-facing slopes of the Changbai Mountains. Phys Geogr, 2011, 32: 374-392.

[43]

Wang T, Ren HB, Ma KP. Climatic signals in tree ring of Picea schrenkiana along an altitudinal gradient in the central Tianshan Mountains, northwestern China. Trees, 2005, 19: 736-742.

[44]

Wang H, Shao XM, Jiang Y, Fang XQ, Wu SH. The impacts of climate change on the radial growth of Pinus koraiensis along elevations of Changbai Mountain in northeastern China. For Ecol Manag, 2013, 289: 333-340.

[45]

Wang XD, Liu HQ, Fan WH, Xu JW, Wu ZF, Dong WH. Climate change in Northeast China between 1849 and 2008. Theor Appl Climatol, 2015, 126: 765-773.

[46]

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

[47]

Yang B, He MH, Melvin TM, Zhao Y, Briffa KR. Climate control on tree growth at the upper and lower treelines: a case study in the qilian mountains, tibetan plateau. PLoS One, 2013, 8: e69065.

[48]

Yu DP, Gu HY, Wang JD, Wang QL, Dai LM. Relationships of climate change and tree ring of Betula ermanii tree line forest in Changbai Mountain. J For Res, 2005, 16: 187-192.

[49]

Yu DP, Wang SZ, Tang LN, Dai LM, Wang QL, Wang SX. Relationship between tree ring chronology of Larix olgensis in Changbai Mountains and the climae change. Chin J Appl Ecol, 2005, 16: 14-20. (in Chinese with English abstract)

[50]

Yu DP, Wang GG, Dai LM, Wang QL. Dendroclimatic analysis of Betula ermanii forests at their upper limit of distribution in Changbai Mountain, Northeast China. For Ecol Manag, 2007, 240: 105-113.

[51]

Yu DP, Wang QW, Wang Y, Zhou WM, Ding H, Fang XM, Jiang SW, Dai LM. Climatic effects on radial growth of major tree species on Changbai Mountain. Ann For Sci, 2011, 68: 921-933.

[52]

Yu DP, Liu JQ, Lewis BJ, Li Z, Zhou WM, Fang XM, Wei YW, Jiang SW, Dai LM. Spatial variation and temporal instability in the climate–growth relationship of Korean pine in the Changbai Mountain region of Northeast China. For Ecol Manag, 2013, 300: 96-105.

[53]

Zhang XL, Bai XP, Chang YX, Chen ZJ. Increased sensitivity of Dahurian larch radial growth to summer temperature with the rapid warming in Northeast China. Trees, 2016, 30: 1799-1806.

[54]

Zhao F, Zhang BP, Pang Y, Yao YH. A study of the contribution of mass elevation effect to the altitudinal distribution of timberline in the Northern Hemisphere. J Geogr Sci, 2014, 24: 226-236.

[55]

Zhuang LW, Axmacher JC, Sang WG. Different radial growth responses to climate warming by two dominant tree species at their upper altitudinal limit on Changbai Mountain. J For Res, 2017, 28: 1-10.

AI Summary AI Mindmap
PDF

187

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/