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Surface circulation of the Japan sea (satellite imagery and drifters data)

机译:日本海的水面环流(卫星图像和漂移数据)

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Joint analysis is carried out of NOAA HRPT IR images (1993-1994) and trajectories sstellite-tracked drifters data (1992-1995) to investigate space-time variability of main elements of the Japan sea dynamics and estimate their kinematic parameters. The most typical diameters, mean orbital velocities and revolution periods of the eddies in the southern area were 90-140 km, 26-34 cm/s and 12-15 days, respectively, their translation velocity did not exceed 2 cm/s. Entrainment of warm (cold) water from south (north) by the eddies determined existence of the East Korean Warm Current, intensive zonal flow around the Yamato Rise and southward cold water intrusions. Seasonal variability of the observed circulation picture, its association with bottom topography and its correspondence with known schemes based on hydrographic data and numerical modelling are discussed.
机译:对NOAA HRPT IR图像(1993-1994年)和轨道跟踪的流星数据(1992-1995年)进行了联合分析,以研究日本海洋动力学主要要素的时空变化并估算其运动学参数。南部涡旋的最典型直径,平均轨道速度和公转周期分别为90-140 km,26-34 cm / s和12-15天,其平移速度不超过2 cm / s。涡流从南部(北部)夹带了温暖的(冷)水,这确定了东朝鲜暖流的存在,大和崛起周围密集的地带流和向南的冷水侵入。讨论了观测到的环流图片的季节性变化,与底部地形的关联以及与基于水文数据和数值模拟的已知方案的对应关系。

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