祁连山中部祁连圆柏林线树木生长与积雪响应关系研究

doi:10.7522/j.issn.1000-0240.2015.0035

冰川冻土 ›› 2015, Vol. 37 ›› Issue (2): 318-326.doi: 10.7522/j.issn.1000-0240.2015.0035

祁连山中部祁连圆柏林线树木生长与积雪响应关系研究

王波^1,2, 陈拓¹, 徐国保¹, 刘晓宏¹, 王文志^1,2, 吴国菊^1,2

1. 中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室, 甘肃兰州 730000;
2. 中国科学院大学, 北京 100049

收稿日期:2014-07-21 修回日期:2015-02-10 出版日期:2015-04-25 发布日期:2015-06-06
通讯作者: 陈拓, E-mail: chentuo@lzb.ac.cn. E-mail:chentuo@lzb.ac.cn
作者简介:王波(1990-), 男, 山东滕州人, 2012年毕业于曲阜师范大学, 现为中国科学院寒区旱区环境与工程研究所硕士研究生, 主要研究方向为树木年轮生态学. E-mail: wangbo900824@lzb.zc.cn
基金资助:
国家重大科学研究计划项目(2013CBA01808); 国家自然科学基金委基础科学人才培养基金冰川学冻土学特殊学科点项目(J1210003/J0109); 中国科学院重点部署项目(KZZD-EW-04-05); 国家自然科学基金项目(31070357; 91025002)资助

The relationships between snow cover and Sabina przewalskii radial growth at alpine timberlines in the middle Qilian Mountains

WANG Bo^1,2, CHEN Tuo¹, XU Guobao¹, LIU Xiaohong¹, WANG Wenzhi^1,2, WU Guoju^1,2

1. State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China

Received:2014-07-21 Revised:2015-02-10 Online:2015-04-25 Published:2015-06-06

摘要/Abstract

摘要：

对青海省东北部祁连县周边的冰沟、青羊沟和扎麻什林线地区的祁连圆柏进行了树芯采集, 建立了祁连山中部3个样点林线处祁连圆柏的树轮宽度年表. 相关分析显示, 树轮宽度与前一年积雪深度和当年3-6月积雪面积呈显著负相关. 同时, 建立了树轮宽度与前一年9月份积雪深度的转换函数方程, 解释方差为35.9%, 树轮-雪深重建数据能较好的反映积雪深度变化. 重建序列显示, 自1740年以来, 研究区共有3个积雪深度高值时段, 分别为1740-1780年、1825-1880年和1910-1980年. 并且, 在长时间尺度上, 积雪深度变化与祁连山地区以及中国西部其他地区的冰川进退有较好的对应关系. 另外, 积雪深度在年际变化和长期变化上都与温度变化表现为负相关.

关键词: 树木年轮, 雪深, 林线, 祁连圆柏, 祁连山中部

Abstract:

Three tree-ring width chronologies were established by using the samples of Sabina przewalskii from the timberlines in the Middle Qilian Mountains. Correlation analysis and response analysis showed a significant negative correlation between tree-ring width and snow depth or snow cover area. After identifying the relationship between snow depth and tree growth, the maximum snow depth in September in the previous year is able to be reconstructed using tree-ring width data. The reconstruction reflects the snow depth variation well. And there have been three high snow depth periods in the study area in the last 270 years: 1740-1780, 1825-1880 and 1910-1980. Moreover, in the long term, variation of snow depth keeps pace with glacier variation in the Qilian Mountains and other parts of western China. In addition, snow depth has an obvious negative relationship with temperature.

Key words: tree-ring, snow depth, alpine timberline, Sabina przewalskii, Qilian Mountains

中图分类号:

Q948.11

王波, 陈拓, 徐国保, 刘晓宏, 王文志, 吴国菊. 祁连山中部祁连圆柏林线树木生长与积雪响应关系研究[J]. 冰川冻土, 2015, 37(2): 318-326.

WANG Bo, CHEN Tuo, XU Guobao, LIU Xiaohong, WANG Wenzhi, WU Guoju. The relationships between snow cover and Sabina przewalskii radial growth at alpine timberlines in the middle Qilian Mountains[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2015, 37(2): 318-326.

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祁连山中部祁连圆柏林线树木生长与积雪响应关系研究

The relationships between snow cover and Sabina przewalskii radial growth at alpine timberlines in the middle Qilian Mountains

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