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Intermediate Waters in the East/Japan Sea

机译:东日本海中间水域

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Properties of the intermediate layer in the East/Japan Sea are examined by using CREAMS data taken mainly in summer of 1995. Vertical profiles of potential temperature, salinity and dissolved oxygen and relationships between these physical and chemical properties show that the dissolved oxygen concentration of 250 μmol/l, roughly corresponding to 0.6°C at the depth of about 400 db, makes a boundary between intermediate and deep waters. Water colder than 0.6°C has a very stable relationship between potential temperature and salinity while salinity of the water warmer than 0.6°C is lower in the western Japan Basin than that in the eastern Japan Basin. The low salinity water with high oxygen corresponds to the East Sea Intermediate Water (ESIW; <34.06 psu, >250 μmol/l and >1.0°C) which was previously identified by Kim and Chung (1984) and the high salinity water with high oxygen found in eastern Japan Basin is named as the High Salinity Intermediate Water (HSIW; >34.07 psu, >250 μmol/l and >0.6°C). Spatial distribution of salinity and acceleration potential on the surface of σ? = 27.2 kg/m3 shows that the ESIW prevailing in the western Japan Basin is transported eastward by a zonal flow along the polar front near 40°N and a cyclonic gyre in the eastern Japan Basin is closely related to the HSIW.
机译:使用1995年夏季开始使用的CREAMS数据对东/日本海中间层的性质进行了研究。潜在温度,盐度和溶解氧的垂直剖面以及这些理化性质之间的关系表明,溶解氧浓度为250 μmol/ l大约对应于约400 db深度处的0.6°C,在中层水与深水之间形成边界。低于0.6°C的水在势能温度和盐度之间具有非常稳定的关系,而低于0.6°C的水的盐度在日本西部盆地比在日本东部盆地低。高含氧量的低盐度水对应于先前由Kim和Chung(1984)确定的东海中间水(ESIW; <34.06 psu,> 250μmol/ l和> 1.0°C)和高含盐量的高盐度水在日本东部盆地发现的氧气被称为高盐度中间水(HSIW;> 34.07 psu,> 250μmol/ l和> 0.6°C)。 σ?表面盐度和加速势的空间分布= 27.2 kg / m3表明,日本西部盆地盛行的ESIW是通过纬向气流沿40°N附近的极地锋向东输送的,而日本东部盆地的气旋回旋与HSIW密切相关。

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