| 引用本文: | 姜盛夏，袁玉江，喻树龙，尚华明，张瑞波，秦莉，张合理，张同文.2020.阿尔泰山西伯利亚云杉多种树轮宽度年表研制及其气候响应研究[J].地球环境学报,11(6): |
| JIANG Shengxia, YUAN Yujiang, YU Shulong, SHANG Huaming, ZHANG Ruibo, QIN Li, ZHANG Heli, ZHANG Tongwen.2020.Development of multiple tree-ring width chronologies of Picea obovata for the Altay Mountains, China, and their climate response[J].Journal of Earth Environment,11(6): |
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| 摘要: |
| 利用树轮图像分析法，获取了阿尔泰山较低海拔西伯利亚云杉（Picea obovata）的全轮、早材和晚材树轮宽度数据，并建立三种树轮宽度年表。通过对树轮宽度年表统计特征及年表与气候因子的相关分析发现：早材生长对气候变化的敏感性更强，而晚材宽度中含有的气候信息相对较少。三种年表对气候因子的响应结果较为一致，但也存在一定的差异性。水分是研究区树木径向生长的主要限制因子。其中，全轮和早材年表与上年7月至当年6月的总降水量正相关性最高（p<0.01），晚材年表与当年4月至7月总降水量正相关性最高（p<0.01）。上年降水量的滞后效应对早材生长的影响比晚材更大。滑动相关分析结果显示，降水量对树木径向生长的影响呈减弱趋势。 |
| 关键词: 阿尔泰山 西伯利亚云杉 树木年轮 早材 晚材 气候响应 |
| DOI：10.7515/JEE192060 |
| CSTR：32259.14.JEE192060 |
| 分类号: |
| 基金项目:中国沙漠气象科学研究基金项目（Sqj2016015）；国家自然科学基金项目（41975095）；中央级公益性科研院所基本科研业务费项目（IDM2018004） |
| 英文基金项目:Desert Meteorological Science Research Foundation of China (Sqj2016015); National Natural Science Foundation of China (41975095); Basal Research Fund of Central Public Welfare Scientific Institution (IDM2018004) |
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| Development of multiple tree-ring width chronologies of Picea obovata for the Altay Mountains, China, and their climate response |
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JIANG Shengxia, YUAN Yujiang, YU Shulong, SHANG Huaming, ZHANG Ruibo, QIN Li, ZHANG Heli, ZHANG Tongwen
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1. Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China
2. Key Laboratory of Tree-ring Ecology of Xinjiang Uygur Autonomous Region, Urumqi 830002, China
3. Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration, Urumqi 830002, China
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| Abstract: |
| Background, aim, and scope The Altay Mountains in China extend approximately 500 km from east to west with average elevation of 3000 m. The widespread distribution of conifers within this mountainous area provides good opportunity for undertaking tree-ring research. To date, some dendroclimatological studies have been carried out in this area. However, previous studies have seldom considered the relative widths of earlywood and latewood. Thus, this study focused on tree-ring earlywood and latewood to elucidate the relationship between the radial growth of Siberian spruces and climatic elements. Materials and methods Total of 410 cores from 228 Siberian spruces located in the low-altitude area were collected on the southern slope of the Altay Mountains, China. Every sample was dealt following standard dendrochronological techniques. Every tree ring was scanned using an Epson LA 1600+. The boundary of earlywood and latewood has been confirmed by the 50% gray value of every single tree-ring image, and WinDendro Systems was used to measure the tree-ring, earlywood and latewood widths. Three kinds of ring-width from 150 cores were obtained and developed chronologies (TRW, EWW and LWW) due to the quality of images. Relationships between chronologies and climatic factors were investigated by calculating the Person correlation coefficients and the moving correlation coefficients with a 31-year time window. Results The high values of standard deviation and mean sensitivity of the EWW chronology reveal that earlywood growth responds more sensitively to the changing of climatic elements. Values of mean within-tree correlation, first principal component and expressed population signal of the LWW chronology are obviously lower than that of the TRW and EWW chronologies, which indicate that the coherence of latewood width variation is relatively weaker. Values of signal-to-noise ratio of the TRW and EWW chronology are similar and obviously higher than the LWW chronology. The relatively coherent climate responses suggests that three kinds of chronologies are positively correlated with precipitation, while the relationships between radial growth of spruces and temperature are mainly negative. All three kinds of chronology show significant positive correlations with precipitation in previous July, December and current May, June, and significant negative correlations with temperature in current June. There are also some differences between tree ring growth and climatic factors, such as precipitation in previous August and current July and temperature in previous September and current May. TRW and EWW are most sensitive to the precipitation from previous July to current June, while the relationship between LWW and precipitation during the period of April to July are strongest. The correlation coefficients between three kinds of chronologies and precipitation in July, August and December in the previous year are listed as follows: earlywood > tree-ring > latewood. Moving correlation analysis displayed that although the relationships between the radial growth of spruces and precipitation in May, June, previous July- current June and April—July are relatively stable, the effects of precipitation on tree-ring has gradually decreased. We also find that all three kinds of chronology exhibit divergent response to temperature in May and June, and precipitation in July. Discussion The comparative analysis of characteristics of chronology and radial growth-climate response indicates that earlywood growth is sensitive to the changing of climatic elements, while the latewood widths might contain less climatic signals. The correlation analysis between chronologies and climatic data reveals that the moisture stress is regarded as the mainly limiting element for the formation of tree-ring, and the lag-effect of precipitation on earlywood is more significant than latewood. It has been detected that the tree sensitivity to temperature in May and June and precipitation in July changed significantly over time. With increasing of precipitation, the effect of drought on tree ring growth decreased in the early growing seasons. Conclusions The climate responses of tree-ring, earlywood and latewood are similar, and the moisture is the mainly limiting element for the radial growth of Siberian spruces in the low-altitude area of the Altay Mountains, China. The climate response of earlywood width is stronger than tree-ring width and latewood width and the EWW chronology might contain more climatic signals. Recommendations and perspectives This paper increased the knowledge regarding the growth patterns of tree-ring, earlywood and latewood of Siberian spruces and their climate response. However, the conclusions derived from this study need to be further substantiated because the findings are based on a relatively limited sample depth. Thus, more samples should be collected in a larger spatial scale to better understand the radial growth of Siberian spruces in internal annual scale. |
| Key words: Altay Mountains Picea obovata tree ring earlywood latewood climate response |