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Variations mechanism in entropy of wave height field and its relation with thermodynamic entropy

         

摘要

This paper gives a brief description of annual period and seasonal variation in the wave height field entropy in the northeastern Pacific. A calculation of the quantity of the, received by lithosphere systems in the northern hemisphere is introduced. The wave heat field entropy is compared with the difference in the quantity of the sun's radiation heat. Analysis on the transfer method, period and lag of this seasonal variation led to the conclusion that the annual period and seasonal variation in the entropy of the wave height field in the Northwestern Pacific is due to the seasonal variation of the sun's radiation heat. Furthermore, the inconsistency between thermodynamic entropy and information entropy was studied.

著录项

  • 来源
    《中国海洋湖沼学报(英文版)》 |2006年第1期|65-68|共4页
  • 作者

  • 作者单位

    Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;

    Physical Oceanography Laboratory, Ocean University of China, Qingdao 266003, China;

    Graduate School of Chinese Academy of Sciences, Beijing 100049, China;

    Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;

    Physical Oceanography Laboratory, Ocean University of China, Qingdao 266003, China;

    Physical Oceanography Laboratory, Ocean University of China, Qingdao 266003, China;

  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 海洋学;
  • 关键词

    wave height field; entropy; sun radiation heat;

    机译:波高场;熵;太阳辐射热;
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