渤海、黄海、东海M2潮汐潮流的三维数值模拟
A 3-D numerical simulation of M2 tides and tidal currents in the Bohai Sea, the Huanghai Sea and the East China Sea
-
摘要: 利用建立的一种新的半隐半显三维数值格式,将渤海、黄海、东海作为一个整体,采用球面坐标系下的三维潮波方程组,考虑了引潮力的作用,数值模拟了渤海、黄海、东海的M2分潮的潮汐与潮流,结果较好地体现了渤海、黄海、东海M2分潮的特征.通过比较65个验潮站的实测值与计算值,所得计算结果的振幅差平均为6.4cm,相角差为6.1°,计算与实测符合良好.本文给出的问潮图与Fang于1986年给出的实测占数值综合结果基本一致.对选取的47个测流站,比较了各层潮流调和常数Ucosζ、Usinζ、Vcosη、Vsinη的计算值与实测值的偏差,偏差绝对值的平均在2.6～4.9cm/s之间.并比较分析了潮流的垂直结构,所得结果与实测符合较好.首次揭示出回流点的水平位置不随深度变化这一特性.最后给出了M2分潮的潮能消耗.Abstract: Under the spherical coordinate,a new 3-D semi-implicit numerical model,considering the tide-producing potential,is developed simulate simulate M2 tides and tidal currents in the Isohai Sea,the Huanghai Sea and the East China Sea.The conyutanonal results cointide with the observed M2 tide in these seas.Compared with 65 gauge stations,it is slxnxm that the averaged absolute difference between the simulated and the observed amplitudes is only 6.4 cm; the averaged difference of phase-lags is 6.4°.The calculated M2 tidal chart consists with Fang's chart(1986) which was drawn based on both numerical and observational results.Compared with 47 current station,the averaged absolute deviation between the calculated and observed harrrpnic constant,Ucosζ、Usinζ、Vcosη、Vsinη of vdal currents at different water layers are from 2.6 cm/s to 4.9 cm/s.The calculated vertical structures of tidal currents are also in fairly good agreement with the observed results.It is the first time to reveal that the current-antphidnxmc points at different layers are lcxated at the same horiwntal poition.The dissipation of M2 tidal energy is also given.
-
Key words:
- 3-D numerical simulation /
- tides and tidal currents /
- Bohai sea
-
Hansen W.The Sea.Vol.I.ch.23,tides.New York:John Wiley & Sons,1962,764-801 叶安乐,梅丽明.渤黄东海潮波数值模拟,海洋与湖沼,1995,26(1):63-69 Choi B H.A tidal rrndel of the Yellow Sea and the Eastern China Sea.Korea Ocean Research and Development Institute(KORDI),Rep.80-02,1980 Fang Guohong.Tide and tidal current charts for the marginal seas adjacent to China.C.J.Oceanol.Iitnnol.,1986,4(1):1-16 赵保仁,方国洪,曹德明等.渤、黄、东海潮汐潮流的数值模拟.海洋学报,1994,16(5):1-10 Feng S.A three-dimension weakly nonlinear nndel of tide-induced Lagrdrtgian residual current and mass-transpaat,with an application to the Bohai Sea.Ihree-dimensional Models of Marine and Estuarine Dynamics,Nihoul J C J,Jamart B M eds.Elsevier Science Pub.Com,Amsterda-Oxford-New York,1987,471-488 Choi B H..A three-dimensional model of the East China Sea.Ocean Hydmdynarnics of the Japan and East China Seas(Elsevier Oceargraphy Series),Ichiye Ted.1984209-224 孙文心.三维浅海流体动力学的一种数值方法—流速分解法.物理海洋数值计算.郑州:河南科技出版社.1992,10-195 王辉,苏志清,冯士棺等,渤海三维风生-热盐-潮致Lagrange余流数值计算海洋学报,1993,15(1):9-2 Fang G,Ichiye T.On the vertical structure of tidal current in a homogeneous sea.Geophys.J.R.Astr.Soc.,1983,73(1):65-82 丁文兰.东海潮汐和潮流特征的研究海洋科学集刊,第21集北京:科学出版社.1983.135-148 丁文兰渤海和黄海潮汐潮流分布的基本特征海洋科学集刊,第};集北京:科学出版社,1985,27-40 -
计量
- 文章访问数: 1118
- HTML全文浏览量: 34
- PDF下载量: 844
- 被引次数: 0
下载:
