中国利用树轮资料重建干湿变化研究进展

doi:10.18306/dlkxjz.2016.11.010

Abstract

Abstract:

With accurate dating, high resolution, and high continuity, tree-ring data become one of the important sources for reconstructing the climate change. The sampling sites distribute widely, many tree species were selected, and the chronologies are very long for studying the relationship of the tree ring and dry-wet changes in China. Significant progress has been made in analyzing the response of tree radial growth to dry-wet changes and reconstructing historical dry-wet climate change based on various research proxies, such as tree-ring width, density, and stable isotopes. In general, moisture condition, especially in the spring and autumn and annual humidity are the important influencing factors of tree-radial growth in low altitudes of arid and semi-arid areas. For trees in the upper limit of forest vegetation, relatively cold-wet areas, and the subtropical climate zone in China, the correlation between tree growth and precipitation was weak. Dry-wet climate reconstruction based on tree-ring data in China is plentiful. Up to now, many precipitation series of more than 1000a or even over 2000a were reconstructed in a large number of regions. The longest tree-ring chronology is 4500a, and the longest precipitation reconstruction sequence is 3500a. The brief summary of selected tree-ring results in this article will provide references and help for tree-ring sampling and dry-wet climate reconstruction.

Key words: tree ring, indicator, response, dry-wet change, paleoclimatic reconstruction, research progress, China

Yajun WANG, Mingqi LI. Research progress of dry-wet climate reconstruction by tree ring in China[J].PROGRESS IN GEOGRAPHY, 2016, 35(11): 1397-1410.

Figures/Tables 3

Fig.1

Fig.2

Tab.1

Selected research of dry-wet climate reconstruction (more than 500a) by tree ring in China"

采样点	经度/°E	纬度/°N	高度/m	树种	树轮指标	重建要素	文献
新疆北部	84.78	44.02	2510~2680	天山云杉	宽度	上年7-6月降水量	Yang et al, 2012
天山南坡阿克苏河流域	79.09	41.55	2280~3600	雪岭云杉	宽度	上年8-4月降水量	张瑞波, 魏文寿等, 2009
阿勒泰地区西部	86.84	48.66	2273	西伯利亚落叶松	宽度	6-9月降水量	张同文等, 2008
华山	110.08	34.48	2030~2050	油松华山松	宽度	4-6月降水量	Chen et al, 2016
横断山	99.29~99.45	27.31~27.59	3040~3060	川滇冷杉	宽度	上年5-4月PDSI	Fang et al, 2010
祁连山中段	99.73	38.78	2900~3150	祁连圆柏	宽度	上年8-7月降水量	Tian et al, 2012
青藏高原南部	88.88~89.61	29.25~30.1	4124~4693	大果圆柏	宽度	上年7-6月降水量	刘晶晶, 2014
青海省境内	96.13~100.13	33.8~38.85	3500~4060	祁连圆柏	宽度	5-10月降水量	王振宇等, 2005
乌兰	98.68	37.03	3100~3800	祁连圆柏	宽度	5-6月降水量	Huang et al, 2007
青藏高原东北	96.83~98.66	37.03~37.54	2877~4060	祁连圆柏	宽度	湿润状况	Shao et al, 2010
柴达木盆地东北	97.23~98.42	36.68~37.47	3660~3917	祁连圆柏	宽度	上年7-6月年降水量	Shao et al, 2005
青藏高原东北	97.15~99.97	35.45~38.7	3205~3995	祁连圆柏	宽度	年降水量	Yang et al, 2014
祁连山	101.24~101.26	37.95~37.97	3164~3265	祁连圆柏	宽度	6-7月SPEI	Gou et al, 2015
柴达木盆地	97.53	37.27	4000	祁连圆柏	宽度	生长季湿度	Wang, Liu et al, 2013
德令哈和乌兰地区	97.06~98.66	36.68~37.51	3500~3920	祁连圆柏	宽度	上年7-6月年降水量	邵雪梅等, 2006
都兰地区、东昆仑山和青海南部山脉之间	98.18~98.67	36.06~36.29	3800~4200	祁连圆柏	宽度	上年7-6月年降水量	Liu et al, 2006
青海湖天峻地区	98.40	37.31	3500	祁连圆柏	宽度	前一年年降水量	时兴合等, 2009
青藏高原	91.51~102.02	29.45~37.37	3260~4440	祁连圆柏	宽度	5-6月PDSI	Zhang, Evans et al, 2015
柴达木盆地东北	97.06~98.66	36.68~37.51	3500~3920	祁连圆柏	宽度	5-6月土壤湿度	Yin et al, 2008
都兰2326	97.67~98.33	35.83~36.5		祁连圆柏	宽度	5-6月降水量	Zhang et al, 2003

Tab.1

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Research progress of dry-wet climate reconstruction by tree ring in China

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