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天山不同海拔雪岭云杉径向生长对气候变化的响应
引用本文:石仁娜·加汗,张同文,喻树龙,姜盛夏,许仲林. 天山不同海拔雪岭云杉径向生长对气候变化的响应[J]. 干旱区研究, 2021, 38(2): 327-338
作者姓名:石仁娜·加汗  张同文  喻树龙  姜盛夏  许仲林
作者单位:新疆大学资源与环境科学学院,新疆 乌鲁木齐 830046;中国气象局乌鲁木齐沙漠气象研究所,新疆 乌鲁木齐 830002;中国气象局树木年轮理化研究重点实验室,新疆 乌鲁木齐 830002;中国气象局乌鲁木齐沙漠气象研究所,新疆 乌鲁木齐 830002;中国气象局树木年轮理化研究重点实验室,新疆 乌鲁木齐 830002;新疆大学资源与环境科学学院,新疆 乌鲁木齐 830046
基金项目:新疆维吾尔自治区重点实验室开放课题(2018D04028);国家自然科学基金项目(41975095,U1803245);天山青年计划“杰出青年科技人才”(2019Q007);第二次青藏高原综合科学考察研究子专题(2019QZKK010206);中央级公益性科研院所基本科研业务经费项目(IDM2018004)资助。
摘    要:为研究不同海拔雪岭云杉(Picea schrenkiana)径向生长对气候要素的响应关系,分别在新疆伊犁尼勒克喀什河流域森林低、中、高海拔采集雪岭云杉树芯样本,建立不同海拔雪岭云杉树轮宽度年表.树轮年表与气象资料相关分析结果显示:影响3个采样点树木径向生长的气候因子主要是平均气温和相对湿度,对降水响应微弱.高、低海拔树...

关 键 词:天山  雪岭云杉(Picea schrenkiana)  树木年轮  不同海拔  气候变化  分异现象

Picea schrenkiana response to climate change at different altitudes in Tianshan Mountains
Shirenna Jiahan,ZHANG Tongwen,YU Shulong,JIANG Shengxia,XU Zhonglin. Picea schrenkiana response to climate change at different altitudes in Tianshan Mountains[J]. Arid Zone Research, 2021, 38(2): 327-338
Authors:Shirenna Jiahan  ZHANG Tongwen  YU Shulong  JIANG Shengxia  XU Zhonglin
Affiliation:(College of Resources and Environment Sciences,Xinjiang University,Urumqi 830046,Xinjiang,China;Institute of Desert Meteorology,China Meteorological Administration,Urumqi 830002,Xinjiang,China;Key Laboratory of Tree-ring Physicochemical Research of China Meteorological Administration,Urumqi 830002,Xinjiang,China)
Abstract:In order to study the difference in the response of radial growth of Picea schrenkiana to climate factors at different altitudes,the core samples of schrenk spruce were collected from the low,middle and high altitudes forest areas in the Nilka Kashi river basin of the Western Tianshan Mountains,the tree ring-width standard dendrochronology at different altitude was established.The result of correlation analysis between tree ring chronology and meteorological data showed that,The chronology of the three sampling points mainly responded to temperature and relative humidity,but responded weakly to precipitation.The radial growth of tree ring at high and low altitudes had the same response to temperature and relative humidity,both of which have positive response to temperature,and negative response to relative humidity,while the radial growth at middle altitude was opposite to high and low altitudes.Since the study area occured abrupt climate change in 1991,the width of schrenk spruce appeared the“growth differentiation”,the tree-ring width index of low-high altitudes showed a downward trend,while the middle altitude showed an upward trend.Before and after the abrupt transition point,the radial growth of trees had an unstable response to temperature and relative humidity.The positive correlation of the mid-altitude chronology to the temperature from May to September and the negative correlation to the relative humidity were significantly enhanced,The low and high altitude chronology had a significant negative correlation with the temperature from July to August,and a significant positive correlation with the relative humidity from June to August.According to the response model of schrenk spruce to climate factors,the rapid warming will lead to intensified evaporation,and the relative humidity decrease,which may cause negative effects on the growth of schrenk spruce in the low and high altitude forest,and the appropriate temperature increase may promote the growth of schrenk spruce in the middle forest.
Keywords:Tianshan  Picea schrenkiana  tree ring  different altitudes  climate change  divergence phenomenon
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