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Water masses and hydrography in the tropical Pacific during Japanese Pacific Climate Study '91 cruise

机译:日本太平洋气候研究'91航行期间热带太平洋的水团和水文

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Hydrographic measurements by CTD were made in the western-central Equatorial Pacific (160°W–147°E) during the Japanese Pacific Climate Study cruise in January–February 1991. InT-S diagram, three water masses are seen in the layer of σθ kg/m3: salinity water corresponding to the Tropical Water of eastern South Pacific origin, less saline water in the North Pacific, and water with salinity between the above two, found on the equator. In three meridional sections (160°W–160°E), the Tropical Water of eastern South Pacific origin extends further equatorward than the climatological data of Levitus (1982).
机译:1991年1月至2月日本太平洋气候研究航行期间,在中赤道中西部(160°W–147°E)进行了CTD的水文测量。在InT-S图中,在σθ层中看到三个水团。 kg / m3:在赤道上发现的盐分水相当于南太平洋东部起源的热带水,北太平洋的盐分水较少,且盐分在上述两者之间。在三个子午段(160°W-160°E)中,南太平洋东部起源的热带水比利未图斯(1982)的气候资料向赤道方向延伸得更多。

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