Radial growth response of major conifers to climate change on Haba Snow Mountain, Southwestern China

被引:11
作者
Zhang, Yun [1 ]
Cao, Renjie [1 ]
Yin, Jie [1 ]
Tian, Kun [1 ]
Xiao, Derong [1 ]
Zhang, Weiguo [1 ,2 ]
Yin, Dingcai [1 ,2 ]
机构
[1] Southwest Forestry Univ, Natl Plateau Wetlands Res Ctr, Wetlands Coll, Kunming, Yunnan, Peoples R China
[2] Lanzhou Univ, Coll Earth Environm Sci, MOE Key Laboratroy Western China Environm Syst, Lanzhou, Peoples R China
基金
中国国家自然科学基金;
关键词
Dendrochronology; Northwestern Yunnan plateau; Climate change; Growth response; TREE-GROWTH; BETULA-ERMANII; RING-WIDTH; TEMPERATURE; SPRUCE; TIMBERLINE; FOREST; STANDS;
D O I
10.1016/j.dendro.2020.125682
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Climate change has an inevitable impact on forest ecosystems, to better understand the influence of climate change on forest growth, we analyzed the growth response of four major conifers to climate on Haba Snow Mountain in central Hengduan Mountains. Tree ring samples were taken from four species at their upper distributional limits, and residual chronologies were developed by using tree ring width data. Response function and redundancy analysis were taken to reveal the key climatic factors affecting tree growth and moving interval analysis was applied to detect the stability of growth-climate relationships. The results showed that previous November temperature, precipitation in current February, current May and current June were common factors affecting the radial growth of the studied species. Abies georgei was mainly influenced by the temperature in previous November. The photothermal condition in May and June controlled the growth of Larix potaninii. Moisture condition in previous August and current May was the key factor affecting Pinus densata growth. As for Pinus yunnanensis, the drought in current May was the limiting factor influencing its growth. The dynamic relationship between tree growth and climatic factors varied among species, and the results were consistent with response function analysis. A forecast in future forest growth on Haba Snow Mountain was complex, since future climate change had both positive and negative effects on the radial growth of four major conifers.
引用
收藏
页数:9
相关论文
共 44 条
[1]  
[Anonymous], 1996, An Introduction to Treering Dating
[2]  
[Anonymous], COORECORDER CDENDRO
[3]  
[Anonymous], 2019, GEOMICROBIOL J
[4]  
[Anonymous], 1998, Numerical Ecology
[5]  
Bazzoffi P., 2011, Italian Journal of Agronomy, V6, pe9, DOI 10.4081/ija.2011.6.s1.e9
[6]   Ring-widths of the above tree-line shrub Rhododendron reveal the change of minimum winter temperature over the past 211 years in Southwestern China [J].
Bi, Yingfeng ;
Xu, Jianchu ;
Yang, Jinchao ;
Li, Zongshan ;
Gebrekirstos, Aster ;
Liang, Eryuan ;
Zhang, Shibao ;
Yang, Yang ;
Yang, Yongping ;
Yang, Xuefei .
CLIMATE DYNAMICS, 2017, 48 (11) :3919-3933
[7]   Assessing drought variability since 1650 AD from tree-rings on the Jade Dragon Snow Mountain, southwest China [J].
Bi, Yingfeng ;
Xu, Jianchu ;
Gebrekirstos, Aster ;
Guo, Liang ;
Zhao, Mingxu ;
Liang, Eryuan ;
Yang, Xuefei .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2015, 35 (14) :4057-4065
[8]   DENDROCLIM2002: A C++ program for statistical calibration of climate signals in tree-ring chronologies [J].
Biondi, F ;
Waikul, K .
COMPUTERS & GEOSCIENCES, 2004, 30 (03) :303-311
[9]  
BRAAK C, 2002, CANOCO REFERENCE MAN
[10]   Climate in Medieval time [J].
Bradley, RS ;
Hughes, MK ;
Diaz, HF .
SCIENCE, 2003, 302 (5644) :404-405