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

作　　者：郭佩芳 侯一筠 钱成春 周良民 

机构地区：[1]Institute of Oceanology [2]Physical Oceanography Laboratory

出　　处：《Chinese Journal of Oceanology and Limnology》2006年第1期65-68,共4页中国海洋湖沼学报（英文版）

基　　金：Supported by the High-Tech Research and Development Program of China (863 Program, No. 2001AA633070 2003AA604040).

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.这篇论文在东北太平洋在波高地熵给对年度时期和季节变异的简短描述。数量的计算，在北半球由岩石圈系统收到了被介绍。波浪热地熵与在阳光的放射热的数量的差别相比。转移方法上的分析，时期并且导致的这季节变异落后在波高的熵的年度时期和季节变异在西北的太平洋回答的结论由于阳光的放射热的季节变异。而且，在热力学的熵之间的矛盾和信息熵被学习。

关 键 词：wave height field ENTROPY sun radiation heat 

分 类 号：P731.22[天文地球—海洋科学]