| 阿勒泰地区两种树轮宽度年表气候响应特征 |
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| 引用本文： | 牛军强,袁玉江,尚华明,张同文,喻树龙,陈峰,张瑞波,姜盛夏.阿勒泰地区两种树轮宽度年表气候响应特征[J].新疆气象,2016,10(1):59-67. |
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| 作者姓名： | 牛军强 袁玉江 尚华明 张同文 喻树龙 陈峰 张瑞波 姜盛夏 |
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| 作者单位： | 新疆师范大学地理科学与旅游学院;中国气象局乌鲁木齐沙漠气象研究所,中国气象局乌鲁木齐沙漠气象研究所,中国气象局乌鲁木齐沙漠气象研究所,中国气象局乌鲁木齐沙漠气象研究所,中国气象局乌鲁木齐沙漠气象研究所,中国气象局乌鲁木齐沙漠气象研究所,中国气象局乌鲁木齐沙漠气象研究所,中国气象局乌鲁木齐沙漠气象研究所 |
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| 基金项目： | 国家自然科学基金(41275120)、中国气象局气候变化专项(CCSF201438)、科技部气象行业专项(GYHY201206014)、国家自然科学基金(40975056)及科技支撑项目(2012BAC23B01)共同资助。 |
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| 摘 要： | 阿尔泰山是树轮气候研究的理想区域，但此前关于阿尔泰山不同海拔高度西伯利亚落叶松和西伯利亚云杉树轮宽度气候响应差异的对比研究较少。本文利用阿尔泰山上树线西伯利亚落叶松以及森林中下部西伯利亚云杉和西伯利亚落叶松树轮宽度资料，在建立宽度年表的基础上，分析阿尔泰山南坡不同海拔高度不同树种对气候响应的差异。研究结果表明：①上树线与森林中下部区域树轮宽度生长的气候限制因子不同，上树线落叶松树轮宽度生长的气候限制因子为6月平均温度，森林中下部云杉树轮生长的气候限制因子为年度（上年7月到当年6月）或春季（4-6月）降水量。②森林中下部云杉树轮宽度生长对降水的响应要优于落叶松。③上树线西伯利亚落叶松树轮宽度均与当年6月平均温度显著正相关（P<0.001），森林中下部西伯利亚落叶松的气候限制因子不明显。
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| 关 键 词： | 阿勒泰地区 西伯利亚落叶松 西伯利亚云杉 宽度年表特征 气候响应 |
| 收稿时间： | 8/2/2015 12:00:00 AM |
| 修稿时间： | 2015/11/12 0:00:00 |
Characteristics of Tree-ring Width Chronologies in Altay Region and Their Respondings to Climate Change |
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| Niu Jun-qiang,Yuan Yu-jiang,Shang Hua-ming,Zhang Tong-wen,Yu Shu-long,Chen Feng,Zhang Rui-bo and Jiang Sheng-xia.Characteristics of Tree-ring Width Chronologies in Altay Region and Their Respondings to Climate Change[J].Bimonthly of Xinjiang Meteorology,2016,10(1):59-67. |
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| Authors: | Niu Jun-qiang Yuan Yu-jiang Shang Hua-ming Zhang Tong-wen Yu Shu-long Chen Feng Zhang Rui-bo and Jiang Sheng-xia |
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| Institution: | College of Geography Science and Tourism,Xinjiang Normal University;China;Institute of Desert Meteorology,China Meteorological Administration,Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration,Xinjiang Laboratory of Tree Ring Ecology,Urumqi,;China,Institute of Desert Meteorology,China Meteorological Administration,Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration,Xinjiang Laboratory of Tree Ring Ecology,Urumqi,Institute of Desert Meteorology,China Meteorological Administration,Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration,Xinjiang Laboratory of Tree Ring Ecology,Urumqi,Institute of Desert Meteorology,China Meteorological Administration,Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration,Xinjiang Laboratory of Tree Ring Ecology,Urumqi,Institute of Desert Meteorology,China Meteorological Administration,Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration,Xinjiang Laboratory of Tree Ring Ecology,Urumqi,Institute of Desert Meteorology,China Meteorological Administration,Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration,Xinjiang Laboratory of Tree Ring Ecology,Urumqi,Institute of Desert Meteorology,China Meteorological Administration,Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration,Xinjiang Laboratory of Tree Ring Ecology,Urumqi,Institute of Desert Meteorology,China Meteorological Administration,Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration,Xinjiang Laboratory of Tree Ring Ecology,Urumqi |
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| Abstract: | |
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| Keywords: | the Altay region PiceaSobovataSLedeb LarixSSibrica Characteristics of Tree-ring Width Chronologies different responding to Climate change |
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