Modelling the variability of exchanges between the Arctic Ocean and the Nordic Seas

作者: Rüdiger Gerdes

DOI: 10.1007/978-94-011-4132-1_22

关键词: HydrographyClimatologyWater massFront (oceanography)RidgeStructural basinAtlantic waterOceanographyGeologyNordic SeasThe arctic

摘要: A large scale warming in the interior of Arctic indicates an increased influence Atlantic Water [1,2,3]. The front between water masses and Pacific character, measured by hydrographic geochemical properties southern Canadian Basin, has apparently shifted from a position over Lomonosov Ridge to more eastern Mendeleyev Ridge[4]. Analysis recent cruise data historical Steele Boyd [5] Grotefendt et al. [6] indicate wide spread layer Eurasian Basin. They attribute inflow through Fram Strait Barents Sea.

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