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Energetic subthermocline currents observed east of Mindanao

机译:在棉兰老岛以东观测到高能热流

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摘要

Two cruises of the JAMSTEC ship Kaiyo, during October 1999 and September 2000, included lowered acoustic Doppler current profiler (ADCP) measurements to 2000 m depth on zonal sections extending east from the Mindanao coast. On the second cruise, the lowered ADCP profiles were augmented by profiles to 1000 m from a 38-kHz shipboard ADCP. All zonal LADCP sections (7°N, 8°, 10°) showed southward flow along the coast extending to at least 2000m depth. Although the Mindanao current in the upper 500m forms a continuous narrow stream along the coast, the deeper southward flow appears to be part of a set of subthermocline eddies within 300 km of the coast; northward flow was found 100-200 km offshore during both cruises. Currents mapped by the shipboard ADCP on the second cruise indicate that cyclonic eddies were centered near 7.5°N, 128°E and 10.2°N, 127°E. Maximum speeds of 0.6 m s~(-1) were observed at 800m depth on the 10°N section, and speeds of 0.2-0.3 m s~(-1) were found below 1500m on all sections.
机译:1999年10月至2000年9月期间,JAMSTEC的Kaiyo船进行了两次巡游,其中包括将棉兰老岛海岸以东延伸的地带上的多普勒电流剖面仪(ADCP)的测量深度降低至2000 m。在第二次巡航中,降低的ADCP轮廓从38 kHz舰载ADCP的轮廓扩展到1000 m。 LADCP的所有区域(7°N,8°,10°)均显示沿海岸向南流动,延伸至至少2000m深度。尽管上部500m处的棉兰老流形成了沿海岸的连续窄流,但更深的向南流动似乎是海岸300公里以内的一组亚热线涡流的一部分。在两次航行中,发现向北流向近海100-200公里。舰载ADCP在第二次巡航中绘制的电流表明,旋风涡流的中心位于7.5°N,128°E和10.2°N,127°E附近。在10°N断面800m深度处的最大速度为0.6 m s〜(-1),在所有断面1500m以下的速度为0.2-0.3 m s〜(-1)。

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