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首页> 外文期刊>Russian meteorology and hydrology >Variability and Conjugacy of Ice Conditions in the System of East Arctic Seas (the Laptev,East Siberian, and Chukchi Seas)
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Variability and Conjugacy of Ice Conditions in the System of East Arctic Seas (the Laptev,East Siberian, and Chukchi Seas)

机译:东北极海(拉普捷夫,东西伯利亚和楚科奇海)系统中冰况的变异性和共轭性

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摘要

The analysis of the long-term variability and spatiotemporal conjugacy of formation pro cesses of ice conditions in the water areas of the Laptev, East Siberian, and Chukchi seas is carried out on the basis of the available data on the ice cover conditions in the above seas. On the whole, the type of relationships between the ice processes in the system of East Arctic seas indicates the existence of certain mechanisms generating the wave processes in the climatic system of the Arctic Basin manifested in the phase opposition in the development of ice conditions on the western and eastern peripheries of the basin under consideration. The statistical analysis of series of the ice coverage of water areas under consideration demonstrated that the existence of the long-term trend of this characteristic in some seas has its spatiotemporal features: the probability of the trend existence increases from west to east (from the Laptev Sea to the Chukchi Sea) and the trends are of opposite signs.
机译:基于上述冰盖条件的可用数据,对拉普捷夫,东西伯利亚和楚科奇海水域冰条件的形成过程的长期变化和时空共轭性进行了分析。海域。总体而言,东北极海洋系统中冰过程之间的关系类型表明,北极盆地气候系统中存在某些形成波浪过程的机制,这表现在北极冰情发展过程中的相位相反。该盆地的西部和东部周边地区正在考虑中。对考虑中的水域一系列冰覆盖范围的统计分析表明,某些海洋中这种特征的长期趋势的存在具有时空特征:这种趋势存在的可能性从西向东增加(从Laptev到楚科奇海)与趋势相反。

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  • 来源
    《Russian meteorology and hydrology》 |2012年第7期|p.468-476|共9页
  • 作者单位

    Il'ichev Pacific Oceanological Institute, Far East Branch, Russian Academy of Sciences,ul. Baltiiskaya 43, Vladivostok, 690041 Russia;

    Il'ichev Pacific Oceanological Institute, Far East Branch, Russian Academy of Sciences,ul. Baltiiskaya 43, Vladivostok, 690041 Russia;

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