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Frazil ice growth and production during katabatic wind events in the Ross Sea, Antarctica

机译:南极洲罗斯海的Katabatic风险活动中的冰雪增长和生产

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Katabatic winds in coastal polynyas expose the ocean to extreme heat loss, causing intense sea ice production and dense water formation around Antarctica throughout autumn and winter. The advancing sea ice pack, combined with high winds and low temperatures, has limited surface ocean observations of polynyas in winter, thereby impeding new insights into the evolution of these ice factories through the dark austral months. Here, we describe oceanic observations during multiple katabatic wind events during May 2017 in the Terra Nova Bay and Ross Sea polynyas. Wind speeds regularly exceeded 20ms?1, air temperatures were below ?25°C, and the oceanic mixed layer extended to 600m. During these events, conductivity–temperature–depth (CTD) profiles revealed bulges of warm, salty water directly beneath the ocean surface and extending downwards tens of meters. These profiles reflect latent heat and salt release during unconsolidated frazil ice production, driven by atmospheric heat loss, a process that has rarely if ever been observed outside the laboratory. A simple salt budget suggests these anomalies reflect in situ frazil ice concentration that ranges from 13 to 266×10-3kgm?3. Contemporaneous estimates of vertical mixing reveal rapid convection in these unstable density profiles and mixing lifetimes from 7 to 12min. The individual estimates of ice production from the salt budget reveal the intensity of short-term ice production, up to 110cmd?1 during the windiest events, and a seasonal average of 29cmd?1. We further found that frazil ice production rates covary with wind speed and with location along the upstream–downstream length of the polynya. These measurements reveal that it is possible to indirectly observe and estimate the process of unconsolidated ice production in polynyas by measuring upper-ocean water column profiles. These vigorous ice production rates suggest frazil ice may be an important component in total polynya ice production.
机译:Katabatic风吹在沿海大多数,将海洋暴露于极端热量损失,在秋季和冬季造成南极洲的强烈海冰生产和密集的水形成。推进的海冰包与高风和低温相结合,在冬季有限的地表海洋观测,从而阻碍了通过黑暗的澳大利多月份进入这些冰工厂的进化。在这里,我们在2017年5月在Terra Nova Bay和Ross Sea Polynyas的多个Katabatic风险期间描述了海洋观测。风速定期超过20ms?1,空气温度低于Δ25°C,海洋混合层延伸到600米。在这些事件期间,电导率 - 温度深度(CTD)型材透露了海洋表面直接下方温热,咸水的凸出凸出水,并将下向下延伸。这些型材在不整合的逃生冰制造过程中反映了潜热和盐释放,由大气热损失驱动,这是一个很少在实验室外观察到的过程。简单的盐预算表明,这些异常反映了原位逃离的冰浓度,范围为13至266×10-3kgm?3。垂直混合的同期估计揭示了这些不稳定密度型材中的快速对流,并将寿命与7-12分钟混合。从盐预算中的冰产量估计揭示了短期冰产量的强度,最大的事件期间高达110cmd?1,季节性平均值29cmd?1。我们进一步发现,Frazil Coverations Covary具有风速,沿着Polynya的上游长度的位置。这些测量表明,通过测量上海水柱型材,可以间接观察和估计多纳斯中未溶解的冰产量的过程。这些充满活力的冰块产率建议逃离冰可能是总冰冰的重要组成部分。

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