Chin J Plant Ecol ›› 2010, Vol. 34 ›› Issue (9): 1045-1057.DOI: 10.3773/j.issn.1005-264x.2010.09.005
• Research Articles • Previous Articles Next Articles
LI Zong-Shan1, LIU Guo-Hua1,*(), FU Bo-Jie1, ZHANG Qi-Bing2, HU Chan-Juan1, LUO Shu-Zheng1
Received:
2010-03-25
Accepted:
2010-05-25
Online:
2010-03-25
Published:
2010-10-08
Contact:
LIU Guo-Hua
LI Zong-Shan, LIU Guo-Hua, FU Bo-Jie, ZHANG Qi-Bing, HU Chan-Juan, LUO Shu-Zheng. Evaluation of temporal stability in tree growth-climate response in Wolong National Natural Reserve, western Sichuan, China[J]. Chin J Plant Ecol, 2010, 34(9): 1045-1057.
Fig. 2 The standard tree-ring chronology of Abies faxoniana in Wolong National Natural Reserve of western Sichuan, China. , series of chronology; , series of 11-year smoothing average; , sample size.
Fig. 3 Monthly variations of precipitations (bars), mean temperature (line with triangles), maximum temperature (line with squares), and minimum temperature (line with circles) for Dujiangyan meteorological station in western Sichuan, China.
Fig. 4 The boxplots of tree-ring chronology and climatic variables during the two study periods (1956-1976 and 1977-2008). Data points distributed outside up and down border lines of the boxplots are extreme outliers.
Fig. 5 Comparison of the change trends for tree-ring chronology and climate data during the common interval: 1956-2008. A, Tree-ring index and climate over the past 53 years (1956-2008). The lines indicate the series of tree-ring index, and the dotted lines indicate the standardized climate variables. B, The difference series (tree-ring index minus climate variables), shaded to emphasize negative values. The vertical dashed lines separate the two study periods, 1956-1976 and 1977-2008, respectively. PRE, SUN.TIME, TEM, TMN and TMX indicate precipitation, sunshine time, temperature, minimum temperature and maximum temperature, respectively.
Fig. 6 Correlation analysis between tree-ring chronology and climate data. A, Correlations during the study period of 1956-1976. B, Correlations during the study period of 1977-2008. The horizontal dashed lines indicate statistically significant correlations at the p < 0.05 level. PRE, SUN.TIME, TEM, TMN and TMX indicate precipitation, sunshine time, temperature, minimum temperature and maximum temperature, respectively. Numbers on x-axis refer to the corresponding months from prior July (-7) to current October (10) in the correlation analysis.
Fig. 7 Correlations between tree-ring chronology and monthly cloud cover data of CRU_TS2.0 climatic database. A, Correlation results during the study period of 1956-1976. B, Correlation result during the study period of 1977-2008. The horizontal dashed lines indicate statistically significant correlations at the p < 0.05 level.
Fig. 8 The association between tree-ring chronology and Pacific Decadal Oscillation (PDO). A, The changing trend of tree-ring chronology and PDO indices (November to March) over the past 53 years (1956-2008), smoothed using a 11-year low-pass filter. Line indicates the standardized data of chronology and dotted line indicated the standardized PDO indices. The vertical dashed lines separate the two study periods, 1956-1976 and 1977-2008, respectively. B, Correlations between tree-ring chronology and monthly PDO indices, for the two study periods: 1956-1976 (white bar) and 1977-2008 (black bar), respectively. The horizontal dashed and dotted lines indicate statistically significant correlations at the p < 0.05 level for 1956-1976 and 1977-2008, respectively.
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