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The possible pivotal role of the eastward dust transport from Central Asia in the global temperature decrease
  • ISSN号:1000-0240
  • 期刊名称:《冰川冻土》
  • 时间:0
  • 分类:P5[天文地球—地质学]
  • 作者机构:[1]Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China, [2]Graduate University of the Chinese Academy of Sciences, Beijing 100039, China, [3]Chemical Laboratory for Atmosphere, China Meteorological Administration, Beijing 100081, China, [4]Urumqi Desert Meteorology, China Meteorological Administration, Urumqi 830002, China
  • 相关基金:Acknowledgements This work was supported by the National Natural Science Foundation of China (Grant No. 40475041), Special Subject of Climate Change of China Meteorological Administration (Grant No. CCSF2005-3- DH14), and China Desert Meteorological Science Foundation (Grant No. SQJ2004002).
中文摘要:

glacial-interglacialgyrations 的出现能与 Milankovitch 理论被解释,这通常被考虑。然而,在理论的一些问题的答案还当前没被导出。在从 CentralAsia 研究东方灰尘运输以后,我们发现了在东方灰尘运输和全球温度减少之间有积极反馈机制。这在北半球的 thehigh 纬度区域放大太阳的放射变化的效果,并且导致全球冰川的时代的出现。积极反馈机制在北半球的 thehigh 纬度区域以太阳的放射的减小开始。随后,全球温度减少,全球冰川的历元发生,在哪个枢轴的因素是从 CentralAsia 的东方灰尘运输。与积极反馈机制的理论,在 Milankovitch 理论的一些问题能被解决很好。

英文摘要:

It is generally considered that the occurrence of glacial-interglacial gyrations can be explained with the Milankovitch theory. However, the solutions of some problems in the theory are currently not derived yet. After researching the eastward dust transport from Central Asia, we have found that there is a positive feedback mechanism between the eastward dust transport and the global temperature decrease. This magnifies the effect of solar radiation change in the high-latitude Hemisphere, and results in area of the Northern the occurrence of the global glacial epoch. The positive feedback mechanism starts with the reduction of solar radiation in the high-latitude area of the Northern Hemisphere. Subsequently, the global temperature decreases and global glacial epoch occurs, in which the pivotal fac- tor is the eastward dust transport from Central Asia. With the theory of the positive feedback mechanism, some problems in the Milankovitch theory can be solved well.

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期刊信息
  • 《冰川冻土》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院 寒区旱区环境与工程研究所
  • 主办单位:中国地理学会 中国科学院寒区旱区环境与工程研究所
  • 主编:程国栋
  • 地址:兰州市天水中路8号
  • 邮编:730000
  • 邮箱:edjgg@lzb.ac.cn
  • 电话:0931-8260767
  • 国际标准刊号:ISSN:1000-0240
  • 国内统一刊号:ISSN:62-1072/P
  • 邮发代号:54-29
  • 获奖情况:
  • 中国自然科学核心期刊,第二届全国优秀地理期刊,甘肃省优秀地理期刊,中国期刊方阵“双效”期刊
  • 国内外数据库收录:
  • 美国地质文献预评数据库,美国剑桥科学文摘,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:17974