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dc.contributor.authorDong, Huizi
dc.contributor.authorZhou, Meng
dc.contributor.authorSmith, Walker O.
dc.contributor.authorLi, Baosheng
dc.contributor.authorHu, Ziyuan
dc.contributor.authorBasedow, Sünnje Linnéa
dc.contributor.authorGaardsted, Frank
dc.contributor.authorZhang, Zhaoru
dc.contributor.authorZhong, Yisen
dc.date.accessioned2022-12-01T11:34:08Z
dc.date.available2022-12-01T11:34:08Z
dc.date.issued2022-09-06
dc.description.abstractDiapausing populations of Calanus finmarchicus at depth in the Lofoten Basin (LB) return to the continental shelf and slope off the Lofoten-Vesterålen 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. Hovmöller 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.en_US
dc.identifier.citationDong, Zhou, Smith, Li, Hu, Basedow, Gaardsted, Zhang, Zhong. Dynamical Controls of the Eastward Transport of Overwintering Calanus finmarchicus From the Lofoten Basin to the Continental Slope. Journal of Geophysical Research (JGR): Oceans. 2022;127(9)en_US
dc.identifier.cristinIDFRIDAID 2075748
dc.identifier.doi10.1029/2022JC018909
dc.identifier.issn2169-9275
dc.identifier.issn2169-9291
dc.identifier.urihttps://hdl.handle.net/10037/27644
dc.language.isoengen_US
dc.relation.journalJournal of Geophysical Research (JGR): Oceans
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2022 The Author(s)en_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0en_US
dc.rightsAttribution 4.0 International (CC BY 4.0)en_US
dc.titleDynamical Controls of the Eastward Transport of Overwintering Calanus finmarchicus From the Lofoten Basin to the Continental Slopeen_US
dc.type.versionpublishedVersionen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


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Attribution 4.0 International (CC BY 4.0)
Except where otherwise noted, this item's license is described as Attribution 4.0 International (CC BY 4.0)