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DETERMINATION OF THE DIRECTION AND VELOCITY OF INTERNAL TIDE WAVE BY MEANS OF MEASUREMENTS AT SINGLE STATION
作者姓名:束星北  赵俊生  王祯祥  孙洪亮  顾学俊  耿世江
作者单位:First Institute of Oceanography, State Oceanic Administration, Qingdao;First Institute of Oceanography, State Oceanic Administration, Qingdao;First Institute of Oceanography, State Oceanic Administration, Qingdao;First Institute of Oceanography, State Oceanic Administration, Qingdao;First Institute of Oceanography, State Oceanic Administration, Qingdao;First Institute of Oceanography, State Oceanic Administration, Qingdao
摘    要:In this paper, the method for determining the direction and velocity of internal tide wave is proposed. The main points are as follows: (1) starting with the continuity equation of incompressible fluid and taking the isotherm whose balance position is situated in the middle of the thermocline as the interface of two-layer ocean, one can get an equation of variations of average total current in the lower and upper layers; (2) WTide (Z) in the above-mentioned equation is expressed in first-order approximation; (3) the internal tide waves are treated as wave packets. Thus, one finds out a statistical relation, AΔu BΔv =ζ, which correlates the average shear effect caused by the internal tide wave with the isothermal fluctuation. The direction and velocity of the wave can be drawn from the formulae: (((1=Arctg (A/B), C1=1/(H0(A2 B2)~1/2).The calculated results agree, in the main, fairly well with two sets of observations at station L3.

收稿时间:1984/9/15 0:00:00
修稿时间:1984/12/30 0:00:00

DETERMINATION OF THE DIRECTION AND VELOCITY OF INTERNAL TIDE WAVE BY MEANS OF MEASUREMENTS AT SINGLE STATION
SHU XINGBEI,ZHAO JUNSHENG,WANG ZHENXIANG,SUN HONGLIANG,GU XUEJUN and GENG SHIJIANG.DETERMINATION OF THE DIRECTION AND VELOCITY OF INTERNAL TIDE WAVE BY MEANS OF MEASUREMENTS AT SINGLE STATION[J].Acta Oceanologica Sinica,1986,5(2):173-182.
Authors:SHU XINGBEI  ZHAO JUNSHENG  WANG ZHENXIANG  SUN HONGLIANG  GU XUEJUN and GENG SHIJIANG
Institution:First Institute of Oceanography, State Oceanic Administration, Qingdao
Abstract:In this paper,the method for determining the direction and velocity of internal tide wave is proposed.The main points are as follows:(1) starting with the continuity equation of incompressible fluid and taking the isotherm whose balance position is situated in the middle of the thermocline as the interface of two-layer ocean,one can get an equation of variations of average total current in the lower and upper layers; (2) WTide (Z) in the above-mentioned equation is expressed in first-order approximation; (3) the internal tide waves are treated as wave packets.Thus,one finds out a statistical relation,AΔū + BΔū=ζ,which correlates the average shear effect caused by the internal tide wave with the isothermal fluctuation.The direction and velocity of the wave can be drawn from the formulae:φ1=Arctg (A/B),C1=1/(H0·√A2+B2).
The calculated results agree,in the main,fairly well with two sets of observations at station L3.
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