干旱区研究

干旱区研究 >

2019 , Vol. 36 >Issue 1: 176 - 185

DOI: https://doi.org/10.13866/j.azr.2019.01.20

气候与气候资源

阿尔泰山北部过去2 000 a来的气候记录集成

  • 张东良 ,
  • 李寅波 ,
  • 杨运鹏 ,
  • 兰波
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  • 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
张东良(1990-),男,助理研究员,主要从事中亚过去气候变化研究. E-mail: zhdl@ms.xjb.ac.cn

收稿日期: 2018-01-22

  修回日期: 2018-08-09

  网络出版日期: 2019-01-17

基金资助

国家自然科学青年基金项目(41803024);国家自然科学基金面上项目(41771234)资助

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Synthesized Climate Change in the North Altay Mountains in the Past 2 000 Years

  • ZHANG Dong-liang ,
  • LI Yin-bo ,
  • YANG Yun-peng ,
  • LAN Bo
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  • 1. Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,Urumqi 830011,Xinjiang,China;
    2. Research Center for Ecology and Environment in Central Asia,Chinese Academy of Sciences,Urumqi 830011,Xinjiang,China;
    3. College of Resources and Environment,Xinjiang University,Urumqi 830046,Xinjiang,China;
    4. School of Environmental and Chemical Engineering,Chongqing Three Gorges University,Chongqing 404000,China

Received date: 2018-01-22

  Revised date: 2018-08-09

  Online published: 2019-01-17

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摘要

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CO2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。

关键词： 气候记录; 树轮; 湖芯; 冰芯; 阿尔泰山

本文引用格式

张东良 , 李寅波 , 杨运鹏 , 兰波 . 阿尔泰山北部过去2 000 a来的气候记录集成[J]. 干旱区研究, 2019 , 36(1) : 176 -185 . DOI: 10.13866/j.azr.2019.01.20

Abstract

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 CO2 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.

Key words： climate change; tree ring; lake core; ice core; Altay Mountains

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