globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:5050776
论文题名:
北欧海深层水的研究进展
其他题名: On the Deep Water of the Nordic Seas
作者: 邵秋丽; 赵进平
刊名: 地球科学进展
ISSN: 1001-8166
出版年: 2014
卷: 29, 期:1, 页码:42-55
语种: 中文
中文关键词: 北欧海 ; 深层水 ; 对流混合 ; 溢流 ; 多年变化
英文关键词: The Nordic Seas ; Deep water ; Convective mixing ; Overflow ; Multi-year variation
WOS学科分类: OCEANOGRAPHY
WOS研究方向: Oceanography
中文摘要: 北欧海作为联系北大西洋和北冰洋的纽带,在全球气候系统中具有重要作用。受冷却等作用的影响,北欧海上层海水下沉形成中层水和深层水。该部分海水向南输运,以溢流的形式进入北大西洋深层,是在全球大洋输送带中具有关键性作用的北大西洋深层水的重要来源。通过综述国内外关于北欧海深层水的研究历史和研究现状,剖析了北欧海深层水形成的重要物理过程,分析了影响北欧海深层水的可能因素和物理过程、北欧海深层水的输运过程以及北欧海深层水近年来的变化趋势,为开展相关研究提供参考。
英文摘要: As a connection region between North Atlantic and Arctic Oceans,the Nordic Sea plays a critical role in global climate system. In the Nordic Seas,surface water converts into intermediate water and deep water after cooling and other effects. These waters transport southward,and enter into North Atlantic as a form of overflow, therefore,they are the main source of the North Atlantic Deep Water( NADW) ,which play a key role in global ocean conveyor. The causes and processes of the deep water formation in the Nordic Seas are still uncertain. Based on a review of current and historical research results of the deep water in the Nordic Seas,the most important process for deep water formation-convection is addressed. Factors and physical processes that may have impact on deep water formation are summarized. The transport of deep water in the Nordic Seas is summed up. Multi-year variation of the deep water is described with the aim of giving some instructions and research directions to the readers.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/156625
Appears in Collections:气候变化事实与影响

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作者单位: 中国海洋大学, 物理海洋教育部重点实验室, 青岛, 山东 266100, 中国

Recommended Citation:
邵秋丽,赵进平. 北欧海深层水的研究进展[J]. 地球科学进展,2014-01-01,29(1):42-55
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