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Historical findings of the Russian physical oceanographers in the Indian Ocean

机译:俄罗斯在印度洋的自然海洋学家的历史发现

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摘要

Abstract This is a review paper related to three findings of Russian physical oceanographers in the Indian Ocean. Observations in the Indian Ocean were used to investigate mesoscale eddies, subsurface equatorial undercurrent, and internal tidal waves near the Mascarene Ridge. Two surveys with measurements of temperature and salinity profiles in the Arabian Sea in 1967 made possible mapping of mesoscale eddies. Repeated moored measurements of currents in the equatorial zone between 55°E and 85°E revealed the existence of seasonal subsurface easterly Tareev undercurrent. A moored array of current and temperature recorders near the Mascarene Ridge was deployed as an antenna for internal tides. The displacements of isotherms caused by internal tides were as large as 150?m. The wave propagated to the southeast from the ridge. The review is intended to summarize the phenomena of the ocean dynamics of the Indian Ocean now when the scientific community of oceanography celebrates the 50th anniversary of the Indian Ocean expedition and plans the second Indian Ocean expedition.
机译:摘要这是一篇与印度洋上的俄罗斯物理海洋学家的三个发现有关的评论论文。在印度洋进行的观测被用来调查Mascarene脊附近的中尺度涡旋,地下赤道暗流和内部潮汐。 1967年在阿拉伯海进行的两次测量温度和盐度剖面的调查使得绘制中尺度涡旋成为可能。在55°E和85°E之间的赤道带反复进行系泊测量,发现存在季节性东风下塔雷耶夫地下暗流。玛斯卡琳山脊附近的系泊的电流和温度记录仪阵列被用作内部潮汐的天线。由内部潮汐引起的等温线位移最大为150?m。波浪从山脊向东南传播。这篇综述旨在总结当印度洋科学界庆祝印度洋探险50周年并计划第二次印度洋探险时印度洋海洋动力学现象。

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