中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Subduction/obduction rate in the North Pacific diagnosed by an eddy-resolving model

文献类型:期刊论文

作者Liu Lingling1; Huang Ruixin2; Wang Fan1
刊名CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
出版日期2016-07-01
卷号34期号:4页码:835-846
关键词subduction obduction eddy-resolved high frequency North Pacific
英文摘要Ventilation in the North Pacific is examined using data from the eddy-resolving 1/12 degrees global HYbrid Coordinate Ocean Model (HYCOM) and QuikSCAT wind stress data. For the period January 2004 to December 2006 and area 20 degrees-40 degrees N, the total annual subduction rate is estimated at 79 Sv, and the obduction rate 41 Sv. Resolving the small-scale and high-frequency components of the eddy field can increase the subduction rate by 42 Sv, and obduction by 31 Sv. Lateral induction is the dominant contributor to enhancement of subduction/obduction, and temporal change of mixed layer depth has a secondary role. Further analysis indicates that the high-frequency components of the eddy field, especially those with timescale shorter than 10 days, are the most critical factor enhancing subduction/obduction.
收录类别SCI
语种英语
WOS记录号WOS:000377207800020
源URL[http://ir.qdio.ac.cn/handle/337002/126228]  
专题海洋研究所_海洋环流与波动重点实验室
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China
2.Woods Hole Oceanog Inst, Dept Phys Oceanog, Woods Hole, MA 02543 USA
推荐引用方式
GB/T 7714
Liu Lingling,Huang Ruixin,Wang Fan. Subduction/obduction rate in the North Pacific diagnosed by an eddy-resolving model[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2016,34(4):835-846.
APA Liu Lingling,Huang Ruixin,&Wang Fan.(2016).Subduction/obduction rate in the North Pacific diagnosed by an eddy-resolving model.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,34(4),835-846.
MLA Liu Lingling,et al."Subduction/obduction rate in the North Pacific diagnosed by an eddy-resolving model".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 34.4(2016):835-846.

入库方式: OAI收割

来源:海洋研究所

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