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首页> 外文期刊>Journal of Physical Oceanography >The Summer Circulation in the Gulf of Suez and Its Influence in the Red Sea Thermohaline Circulation
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The Summer Circulation in the Gulf of Suez and Its Influence in the Red Sea Thermohaline Circulation

机译：苏伊士湾的夏季环流及其对红海热盐环流的影响

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摘要

The Gulf of Suez is accepted as an important location for Red Sea Deep Water formation, but the circulation and exchange with the Red Sea around the year remains elusive. A summer cruise in the area gives the opportunity to investigate features of the summertime hydrological structure and exchange with the Red Sea. An inverse estuarine circulation and exchange with the Red Sea is evident. The topographic patterns of the gulf play an important role in the circulation. Two sills, one in midbasin and a second at the mouth of the gulf, inhibit the bottom flow, topographically trapping waters that were formed in the cold season. Although the water mass characteristics of the outflowing waters during the other seasons are not directly related to the deep waters, they can influence the water column structure of the northern Red Sea. A simple box model shows that their contribution can have a significant influence in the formation of the intermediate layer. A hypersaline (40.6 psu) but relatively warm (23 degrees C) water mass, originating in the Gulf of Suez, is detected at intermediate depths (100-150 m), with a strong signal in the western part of the Red Sea.
机译：苏伊士湾被公认为是红海深水形成的重要地点，但全年与红海的环流和交换仍然难以捉摸。该地区的夏季巡游使人们有机会研究夏季水文结构的特征并与红海进行交换。河口逆流和与红海的交换是显而易见的。海湾的地形图在循环中起着重要作用。有两个窗台，一个位于中流域，另一个位于海湾口，抑制了底部水流，地形上捕获了在寒冷季节形成的水。尽管其他季节流出水的水质特征与深水没有直接关系，但它们会影响北部红海的水柱结构。一个简单的盒子模型表明，它们的贡献可对中间层的形成产生重大影响。在中深度（100-150 m）处检测到起源于苏伊士湾的高盐度（40.6 psu）但相对温暖（23摄氏度）的水团，在红海西部具有强烈的信号。

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  • 来源
    《Journal of Physical Oceanography》 |2017年第8期|2047-2053|共7页
  • 作者

    Sofianos S.; Johns W. E.;

  • 作者单位

    Univ Athens, Dept Environm Phys, Athens, Greece;

    Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Dept Meteorol & Phys Oceanog, 4600 Rickenbacker Causeway, Miami, FL 33149 USA;

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