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A changing Arctic seasonal ice zone: Observations from 1870-2003 and possible oceanographic consequences

机译:不断变化的北极季节性冰区:1870年至2003年的观测以及可能的海洋学后果

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摘要

Changes in the extent of seasonal ice were investigated using historical and satellite observations for the period 1870-2003. The seasonal ice zone (SIZ) has been gradually expanding since 1870, with a marked acceleration over the past three decades, and has migrated north to encompass all peripheral Arctic seas. The expansion of the SIZ may be increasing the salinity of the upper Arctic Ocean, consistent with recent observations. The migration of the SIZ over continental shelves may also be enhancing the formation rate and salinity of Arctic deep waters, which are subsequently advected to the convective region of the Greenland-Iceland-Norwegian Sea, thereby influencing the formation of North Atlantic deep waters and related global thermohaline circulation.
机译:利用历史和卫星观测资料(1870-2003年)调查了季节性冰面积的变化。自1870年以来,季节性冰区(SIZ)一直在逐渐扩大,在过去的三十年中明显加速,并已向北迁移,以包围所有北极外围海域。 SIZ的扩张可能正在增加北冰洋上层的盐度,这与最近的观察一致。 SIZ在大陆架上的迁移也可能会提高北极深水的形成速度和盐度,随后将其平流到格陵兰-冰岛-挪威海的对流区域,从而影响北大西洋深水的形成及相关全球盐碱循环。

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