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The coupled characteristics of the physical process between sea rnice of two poles and Tibetan land surface

机译:两极海底与藏族陆地表面物理过程的耦合特征

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摘要

In order to discuss the characteristics of sea ice change of strong signal area rnon Antarctic and Arctic and the correlation between the thermal state on the land rnsurface of Tibetan Plateau and the atmosphere circulation of North Hemisphere or the rnclimate changes in China, and to study the feedback mechanism among “three-pole” rnfactors, the earlier stage “three-pole” strong signal characteristics by using statistic rnmethods such as teleconnection,which affect the regional climate changes in China and rnEast Asia. The cross-correlation feature and coupling effect between ice caps of North rnand South pole and water-thermal state on Tibetan Plateau surface are discussed as rnwell. The contribution of three-pole's earlier stage factors to China's summer climate rnchange and the influence of its dynamic structure are compared here. The formation rnmechanisms of global climate change and regional climate change of China are rninvestigated from the aspect of qualitative correlation mode of global sea-land-air-ice.
机译:为了探讨强信号区南极和北极海冰的变化特征,以及青藏高原陆地表面热状态与北半球大气环流或中国气候变化之间的相关性,研究三极因子之间的反馈机制,早期的“三极”强信号特征是通过使用远程连接等统计方法来影响中国和东亚区域气候变化的。讨论了南北极冰盖与青藏高原地表水热状态的互相关特征及其耦合效应。在此比较了三极早期因素对中国夏季气候变化的贡献及其动态结构的影响。从全球海陆空冰的质相关模型的角度研究了全球气候变化和中国区域气候变化的形成机理。

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  • 来源
    《极地科学进展(英文版)》 |2000年第2期|131-140|共10页
  • 作者

  • 作者单位

    Chinese Academy of Meteorological Sciences, Beijing 100081, China;

    Chinese Academy of Meteorological Sciences, Beijing 100081, China;

    Chinese Academy of Meteorological Sciences, Beijing 100081, China;

    Chinese Academy of Meteorological Sciences, Beijing 100081, China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 自然地理学;
  • 关键词

    Antarctic; Arctic; cryosphere; sea-ice; plateau; climate change.;

    机译:南极;北极;冰冻圈;海冰;高原;气候变化。;
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