Ice Transport in the East Greenland Current and Its Causes

Ice Transport in the East Greenland Current and Its Causes
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东格陵兰海流的冰输送及其成因

DOI:
10.14430/arctic3493
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发表时间:
1964
期刊:
影响因子:
--
通讯作者:
E. Vowinckel
E. Vowinckel
中科院分区:
--
文献类型:
--
作者:
E. Vowinckel

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检查,特别是,从格陵兰岛和斯瓦尔巴群岛之间的北冰洋冰出口,因为它影响海洋的能源预算。计算了每月和每年通过风和电流输出的数量,描述了方法。总出口量估计为950,000 - 1,000,000公里,接近俄罗斯估计的1,036,000公里。计算了1921-1956年的年变化,发现风输出和流输出同样变化。北冰洋的冰和洋流的总热量增加波动的平均偏差为4.7%;但对于特定的一年,差异可能为15-20%。
Examines, especially, the export of ice from the Arctic Ocean between Greenland and Svalbard, as it effects the Ocean's energy budget. The amounts exported monthly and annually by wind and by current are calculated, methods described. Total export, estimated at 950,000-1,000,000 km approaches the Russian estimates of 1,036,000 km. Annual variations 1921-1956 are calculated, and export by wind and that by current found equally variable. The general heat gain by ice and currents for the Arctic Ocean fluctuates with a mean deviation of 4.7%; but for a particular year, a difference of 15-20% is likely.