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Sea surface current measurement experiment by CODAR HF radar at coastal water of Eastern of the Yellow Sea and comparisons with different types of coastal circulation models

机译:CODAR HF雷达在黄海东部沿海水域海面测量实验及与不同类型海岸环流模型的比较

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As a part of an intensive joint field experiment held in eastern coastal water of the Yellow Sea in November, 1992, a field measurement experiment was carried out using CODAR HF Radar off the west coast of Korea where a strong tidally driven flow is superposed with rather steady wind driven flow in winter season. The sea surface currents in shallow coastal waters were measured by the HF radar during Nov 15 to 19, 1992. Surface current maps were obtained over an area of about 30 x 30 km and had been compared with results of different types of numerical circulation models. Tide and wind induced flows were computed using 2-D and 3-Dimensional coastal circulation models. The offshore boundary condition of the circulation models was prepared from tide harmonic data base for the Yellow Sea and the East China China Sea and simultaneous water elevation measurement along the boundary during the experiment. Wind stresses and sea-level atmospherical pressure data set reanalyzed by ECMWF were used as meteorological inputs. The tidally induced currents modelled by 2-D circulation model when the wind was relatively weak and wind driven surface flow modelled by 3-D circulation model when the wind was relatively strong and steady were compared with the field measurements. Simple method of empirical calculation of the surface wind driven flow superposed by tidal current calculated by operational real-time tidal current prediction method, CHARRY, developed by Y.Kang (1996) was also compared with those from other models and HF radar data.
机译:作为1992年11月在黄海东部沿海水域进行的密集联合野外试验的一部分,在韩国西海岸外使用CODAR HF雷达进行了野外测量试验,在该试验中,强烈的潮汐驱动气流与冬季稳定的风流。 1992年11月15日至19日,通过高频雷达测量了浅海沿岸海域的海面电流。获得了约30 x 30 km区域的地表电流图,并将其与不同类型的数值环流模型的结果进行了比较。使用2维和3维沿海环流模型计算潮汐和风引起的流量。利用黄海和中国东海的潮汐谐波数据库,并在实验过程中沿边界同时进行水高测量,建立了环流模型的离岸边界条件。 ECMWF重新分析的风应力和海平面气压数据被用作气象输入。将2D环流模型在风相对弱时建模的潮汐感应电流与3D环流模型在风相对强且稳定时建模的风动力面流与现场测量结果进行了比较。还比较了由Y.Kang(1996)开发的由操作实时潮汐流预测方法CHARRY计算出的,由潮汐流叠加的地表风驱动流的简单经验计算方法,并与其他模型和HF雷达数据进行了比较。

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