中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Dynamical Controls of the Eastward Transport of Overwintering Calanus finmarchicus From the Lofoten Basin to the Continental Slope

文献类型:期刊论文

作者Dong, Huizi6,7; Zhou, Meng7; Smith, Walker O.5,7; Li, Baosheng4; Hu, Ziyuan3; Basedow, Sunnje L.2; Gaardsted, Frank1; Zhang, Zhaoru7; Zhong, Yisen7
刊名JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
出版日期2022-09-01
卷号127期号:9页码:15
ISSN号2169-9275
关键词Calanus finmarchicus eastward transport Lofoten Basin Lagrangian Coherent Structures particle tracking dynamical diagnostics
DOI10.1029/2022JC018909
通讯作者Zhou, Meng(meng.zhou@sjtu.edu.cn)
英文摘要Diapausing populations of Calanus finmarchicus at depth in the Lofoten Basin (LB) return to the continental shelf and slope off the Lofoten-Vesteralen Islands during the phytoplankton spring bloom to feed and spawn, forming surface swarms with a great abundance. To study how overwintering populations of C. finmarchicus move with the deep currents and return to the shelf, Lagrangian transport characteristics of particles in deep water between 2008 and 2019 were analyzed using Global Ocean Reanalysis and Simulation re-analysis data and Lagrangian Coherent Structures (LCSs). Our analyses revealed that persistent eastward transport of diapausing C. finmarchicus between LB and continental slope occurred mainly between 600 and 1,100 m in the Arctic Intermediate Water. The consistency of the vertical distributions of C. finmarchicus abundance and salinity further suggests that physical factors control the horizontal distribution of the species. Hovmoller diagrams of kinetic energy indicate that there is an eastward advection of mean current at depth. The co-occurrence between the eastward transport of LCSs and the eastward advection of the mean current provides direct evidence that the life history of C. finmarchicus is subjected to physical control in the Norwegian Sea. Plain Language Summary Overwintering populations of the copepod Calanus finmarchicus in the Lofoten Basin (LB) are critical for maintaining its life cycle and food web in the northern Norwegian Sea. Horizontal advection and particle tracking simulation between 2008 and 2019 were performed using reanalysis data. Our analyses revealed that eastward transport between 600 and 1,100 m in the Arctic Intermediate Water below the Atlantic Water was responsible for moving C. finmarchicus from the LB to the continental slope. The consistency of the vertical distributions of C. finmarchicus and salinity further suggests that physical factors control the horizontal distribution of the species. The trend of decreasing abundance of C. finmarchicus from west to east in January results from the eastward transport of the species and its accumulation on the continental slope. Eastward transport from the basin to the slope is a key process in the life cycle of C. finmarchicus and demonstrates the importance of large-scale physical-biological interactions in Nordic Seas.
资助项目Sino-Norway Collaborative STRESSOR Project - Natural Science Foundation of China (NSFC)[41861134040] ; Research Council of Norway (RCN)[287043] ; NSFC Special Program[41941008] ; Shanghai Frontiers Science Center of Polar Science (SCOPS)
WOS研究方向Oceanography
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:000855240500001
源URL[http://ir.qdio.ac.cn/handle/337002/180819]  
专题海洋研究所_胶州湾海洋生态系统国家野外研究站
通讯作者Zhou, Meng
作者单位1.Akvaplan Niva Fram Ctr, Tromso, Norway
2.UiT Arctic Univ Norway, Dept Arctic & Marine Biol, Tromso, Norway
3.Chinese Acad Sci, Inst Oceanol, Jiaozhou Bay Natl Marine Ecosyst Res Stn, Qingdao, Peoples R China
4.Second Inst Oceanog MNR, State Key Lab Satellite Ocean Environm Dynam, Hangzhou, Peoples R China
5.Virginia Inst Marine Sci, Gloucester Point, VA 23062 USA
6.Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA
7.Shanghai Jiao Tong Univ, Sch Oceanog, Shanghai, Peoples R China
推荐引用方式
GB/T 7714
Dong, Huizi,Zhou, Meng,Smith, Walker O.,et al. Dynamical Controls of the Eastward Transport of Overwintering Calanus finmarchicus From the Lofoten Basin to the Continental Slope[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2022,127(9):15.
APA Dong, Huizi.,Zhou, Meng.,Smith, Walker O..,Li, Baosheng.,Hu, Ziyuan.,...&Zhong, Yisen.(2022).Dynamical Controls of the Eastward Transport of Overwintering Calanus finmarchicus From the Lofoten Basin to the Continental Slope.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,127(9),15.
MLA Dong, Huizi,et al."Dynamical Controls of the Eastward Transport of Overwintering Calanus finmarchicus From the Lofoten Basin to the Continental Slope".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 127.9(2022):15.

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来源:海洋研究所

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