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Transport Barriers and the Retention of Calanus finmarchicus on the Lofoten Shelf in Early Spring
Author(s) -
Dong Huizi,
Zhou Meng,
Hu Ziyuan,
Zhang Zhaoru,
Zhong Yisen,
Basedow Sünnje L.,
Smith Walker O.
Publication year - 2021
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1029/2021jc017408
Subject(s) - calanus finmarchicus , oceanography , copepod , baroclinity , continental shelf , geology , spring (device) , barotropic fluid , water mass , fishery , biology , crustacean , physics , thermodynamics
Large aggregations of the copepod Calanus finmarchicus occur each spring in the shelf‐slope‐oceanic regions off the Lofoten‐Vesterålen Islands where productive fisheries have traditionally supported local economies. The retention and off‐shelf transport of populations of C. finmarchicus populations were studied by analyzing ocean color remote sensing, satellite altimetry data, and Lagrangian Coherent Structures (LCS) between 2010 and 2019. Our analysis revealed the existence of a transport barrier reoccurring at the shelf break that retains C. finmarchicus on the shelf for 30–70 days in the spring when C. finmarchicus were seasonally ascending to the surface layer. The analysis of baroclinic and barotropic energy conversions indicated that the topographically steered Norwegian Atlantic Current is the primary mechanism in the formation of the transport barrier, which restricts exchanges of C. finmarchicus populations between shelf and oceanic waters. In the mid‐ to late April, an increase in baroclinicity leads to an increase in mesoscale eddies generated on the shelf break near Lofoten‐Vesterålen Islands, breaking down transport barriers and causing off‐shelf transport of C. finmarchicus . The transport barrier predictably reoccurs in early spring which supports the entrapment of C. finmarchicus in the shelf region.