渤海M2分潮的伴随模式数值实验
Numerical experiments of the adjoint model for M2 tide in the Bohai Sea
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摘要: 根据渤海海域内M2潮汐调和常数的实测值,采用伴随方法来反演出开边界处的潮汐调和常数.为了取得较好的数值模拟结果,同时对给定的底摩擦系数进行了校正并对水深进行了微调.做了4个实验,并分别计算出调和常数的实测值与模拟值之差的绝对平均值:(1)只用19个验潮站的潮汐调和常数;振幅差为2.4cm,迟角差为5.0°.(2)只用37个观测点的高度计资料;振幅差为4.4cm,迟角差为5.7°.(3)同时利用19个验潮站的潮汐调和常数和37个观测点的高度计资料;振幅差为5.5cm,迟角差为8.5°.(4)同时利用19个验潮站的潮汐调和常数和14个观测点的高度计资料;振幅差为3.3cm,迟角差为5.6°.4个实验结果都较好地体现了渤海M2潮波的特征.Abstract: Adjoint method was used to deduce M2 tidal harmonic constants on the open boundary of the Bohai Sea by using M2 tidal harmonic constants in the inter iorregion.To improve the results of numerical simulation,the prescribed bottom friction coefficients were also adjusted by adjoint assimilation.Four experiments were car ried out.Experiment 1 uses only har monic constats at 19 tidal stations;Experiment 2 uses harmonic constants at 37 points on the T/P Satellite Tracks;Experiment 3 uses all the above data;Experiment 4 uses har monic constants at 19 tidal stations and 14 selected points on the T/P Satellite Tracks.The averaged absolute differences between the simulated and the observed are as follows respectively.For Experiment 1 the averaged absolute difference of the amplitude is 2.4 cm and the averaged absolute difference of the phaselag is 5.0°.For Experiment 2 they are 4.4 cm and 5.7°respectively.Experiment 3 gives 5.5 cm and 8.5°respectively.And Experiment 4 gives 3.3 cm and 5.6°respectively.The results of the four experiments coincide with the observed M2 tide in the Bohai Sea fairly well.
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Key words:
- Bohai Sea /
- M2 tide /
- adjoint method
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