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阿尔泰山北部过去2 000 a 来的气候记录集成
Synthesized Climate Change in the North Altay Mountains in the Past 2 000 Years

查看参考文献47篇

张东良 1,2   李寅波 3   杨运鹏 1   兰波 4  
文摘 在综述阿尔泰山北部过去2 000 a气候变化研究成果的基础上,归纳了文献中所包含气候信息的地理一致性。就气温而言,基于阿尔泰山北部湖芯、树轮和冰芯重建的气温序列真实记录了北半球的重要气候事件,包括罗马最适宜期(0—400年) 、黑暗时代冷期(400—600年) 、中世纪暖期(800—1200年) 、小冰期(1400—1860年)和现代暖期(自1860年以来) 。由太阳活动主控的太阳辐射变化是过去2 000 a来阿尔泰山北部气温变化的主导因素,过去150 a来大气CO_2的增加是现代暖期(自1860年以来)升温的主导因素。就降水而言,阿尔泰山北部过去2 000 a的降水变化趋势显示,高降水时段出现在0—450年、600—800年、1050—1300年、1650—1860年,低降水时段出现在450—600年、800—1050年、1300—1650年、1860—2000年。此外,阿尔泰山北部过去2 000 a来气温和降水的组合并不支持所谓的“暖干—冷湿”水热配置模式。
其他语种文摘 This study firstly reviewed the achievements about climate change in the north Altay Mountains over the past 2 000 years,and then summarized the geographical consistency of climate information contained in these documents. Mutil-proxies (lake cores, tree rings and ice cores) recorded the five important climatic events in the Northern Hemisphere, including the Roman Optimum (0 - 400 AD) ,Dark Age Cold Period (400 - 600 AD) ,Medieval Warm Period (800 - 1200 AD) ,Little Ice Age (1400 - 1860 AD) ,and recent warming period (since 1860 AD) . These climatic events were mainly modulated by solar activity-dominated solar radiation variations in the past 2 000 years and recent warming period since 1860 AD,which were largely attributable to an increase of CO_2 concentration in the past 150 years. The precipitation history in the north Altay Mountains over the past 2 000 years indicated that these periods including 0 - 450, 600 - 800, 1050 - 1300, 1650 - 1860 AD were characterized by high precipitation, and those including 450 - 600, 800 - 1050, 1300 - 1650, 1860 - 2000 AD were featured by low precipitation. In addition, the combination of temperature and precipitation in the north Altay Mountains over the past 2 000 years did not supported the“cold-wet and warm-dry”hydrothermal configuration in the arid zone in Central Asia.
来源 干旱区研究 ,2019,36(1):176-185 【核心库】
DOI 10.13866/j.azr.2019.01.20
关键词 气候记录 ; 树轮 ; 湖芯 ; 冰芯 ; 阿尔泰山
地址

1. 中国科学院新疆生态与地理研究所, 新疆, 乌鲁木齐, 830011  

2. 中国科学院中亚生态与环境研究中心, 新疆, 乌鲁木齐, 830011  

3. 新疆大学资源与环境学院, 新疆, 乌鲁木齐, 830046  

4. 重庆三峡学院, 重庆, 404000

语种 中文
文献类型 研究性论文
ISSN 1001-4675
学科 大气科学(气象学)
基金 国家自然科学青年基金项目 ;  国家自然科学基金面上项目
文献收藏号 CSCD:6414277

参考文献 共 47 共3页

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引证文献 3 篇

1 姚付龙 高分辨率泥炭孢粉记录的天山北坡2400 cal yr B.P.以来植被演替及其对气候变化的响应 地层学杂志,2020,44(1):104-112
被引 6 次

2 刘奇 阿尔泰山泥炭α-纤维素碳和氧同位素的古环境意义--以黑阳坡泥炭为例 干旱区研究,2022,39(1):30-40
被引 0 次

显示所有3篇文献

论文科学数据集

1. 北半球温度代用资料（1000-2000年）

2. 中国西部地区长期干湿指数序列集（AD1500-BP2000）

3. 青藏高原过去1000年环境要素序列数据（温室气体、金属、粉尘）

数据来源：
国家青藏高原科学数据中心
PlumX Metrics
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