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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Current measurements in the Maluku Sea
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Current measurements in the Maluku Sea

机译：马鲁古海目前的测量

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摘要

A current meter mooring was deployed in the eastern Indonesian archipelago, in the Maluku Sea, between the islands of Sulawesi and Halmahera, to contribute to estimates of the volume of the Indonesian Throughflow, for 13 months (June 1993-July 1994), with meters located at 740, 1250, 1750, and 2240 m below the surface. Hydrocasts for salinity and temperature were made at the time of deployment. The current meter and hydrographic data indicate a predominantly southward flow at the upper three meters throughout the year and a steady northward flow at the bottom meter. T-S and oxygen properties below 1800 m indicate a clockwise circulation in the Maluku Sea, with a vertical velocity of about 2 m/d. If the currents at the mooring, which is located on the western side of the Maluku Sea, are typical of the entire basin width, the average southward through flow between 740 m and 1500 m below the surface, 7 Sv (1 Sv = 10(6) m(3)/s), is comparable in magnitude with estimates of upper layer transport and should be accounted for in estimates of the Indonesian Throughflow. [References: 16]
机译：目前的仪表系泊设备已部署在印度尼西亚东部群岛的马鲁古海，在苏拉威西岛和哈马黑拉岛之间，以协助估计13个月（1993年6月至1994年7月）的印度尼西亚流量。位于地表以下740、1250、1750和2240 m。在部署时进行了盐度和温度的水力发电。当前的水表和水文数据表明，全年中上部三米处主要为南流，而底部水表则为稳定的北流。低于1800 m的T-S和氧气特性表明在Maluku海中存在顺时针环流，垂直速度约为2 m / d。如果位于马鲁古海西侧的系泊流是整个盆地宽度的典型特征，那么海平面以下740 m至1500 m之间的平均南向通流为7 Sv（1 Sv = 10（ 6）m（3）/ s），其大小与上层传输的估计值相当，应该在印度尼西亚流量的估计中考虑。 [参考：16]

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