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Long-Term Changes in Metocean-Ice Conditions in the Canadian Beaufort Sea

机译:加拿大波弗特海线虫冰情的长期变化

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Existing long-term metocean-ice data sets are reviewed and analyzedfor estimation of trends and changes relevant to offshore oil and gasand shippingavigation activities in the Canadian Beaufort Sea (CBS).An analysis of 45 years (1968-2012) of sea ice properties fromCanadian Ice Service sea ice charts indicates that the summer and earlyfall concentrations of sea ice are decreasing by up to 7.4% per decade(September to mid-October). Old ice concentrations are decreasing at ahigher rate along the slope and deeper offshore waters of the BeaufortSea at rates of 10.5% per decade. There is also evidence of anincreasing presence of glacial ice features passing through the CanadianBeaufort Sea. In contrast to the deeper offshore waters, the reductionsin ice concentrations over the continental slope are smaller but stillstatistically significant in some subregions. The mid-outer shelf regionalso exhibits substantial reductions in mid-October with the loss of oldice and young ice being a large part of the total ice reduction. However,there have been no significant changes observed in ice thickness incontinental shelf region. The duration of the landfast ice off thecoastline of the CBS is also being reduced with a delay in formationdate of 2.8 weeks per decade and an advance in break-up date of 0.65week per decade.An analysis of long-term air temperatures reveals that the largestwarming occurs in the fall and winter corresponding to a temperatureelevation of about 4°C over the past five decades or an equivalent rateof decadal change of, approximately, 0.8°C. The regional windpatterns in the region exhibit little evidence of long-term trends incoastal zones, while cyclonic activity appears to be increasing inoffshore areas. The combination of the reduced areal extent of sea icein summer and especially in the fall, and continuing and perhapsincreased cyclonic activity in offshore areas, is leading to increasingoccurrences of large ocean waves, as seen through analyses of mooredupward looking sonar data obtained over the past decade.
机译:审查和分析了现有的长期海洋冰数据集 用于估计与海上石油和天然气有关的趋势和变化 和加拿大波弗特海(CBS)的运输/导航活动。 对45年(1968-2012)海冰性质的分析 加拿大制冰局的海冰图表明了夏季和早期 每十年下​​降的海冰浓度下降多达7.4% (9月至10月中旬)。老冰的浓度在 博福特(Beaufort)的山坡和深海沿岸水位较高 每十年以10.5%的速度出海。也有证据表明 穿越加拿大的冰川冰特征越来越多 博福特海。与更深的近海相比,减少的数量 大陆坡上的冰浓度较小,但仍然 在某些次区域具有统计意义。中外货架区 在10月中旬也出现了大幅减少,并且失去了旧的 冰和年轻冰占总减冰量的很大一部分。然而, 没有观察到冰厚度的显着变化 大陆架地区。陆地冰层持续的时间 哥伦比亚广播公司的海岸线也正在减少,形成时间有所延迟 每十年2.8周的日期,分手日期的提前0.65 每十年一次。 对长期空气温度的分析表明,最大的 变暖发生在与温度相对应的秋天和冬天 在过去的五十年中,温度升高约4°C或相当的速度 大约0.8°C的十年变化的平均值。区域风 该区域的格局几乎没有迹象表明该区域的长期趋势 沿海地区,而气旋活动似乎在增加 离岸地区。减少海冰面积的结合 在夏天,特别是在秋天,并持续下去,也许 近海地区气旋活动增加,导致 通过对系泊设备的分析可以看出,发生了大浪 过去十年获得的向上声纳数据。

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