The Northeast Greenland Shelf as a Potential Habitat for the Northeast Arctic Cod

• Published in: Frontiers in Marine Science
• Main Authors: Kjersti O. Strand, Svein Sundby, Jon Albretsen, Frode B. Vikebø
• Format: Article in Journal/Newspaper
• Language: English
• Published: Frontiers Media S.A. 2017
• Subjects: connectivity; pelagic juvenile; cross-shelf; spawning ground; nursery ground; forecast; Science; Q; General. Including nature conservation; geographical distribution; QH1-199.5; Arctic; Barents Sea; Greenland; Lofoten; Lofoten Basin; Norwegian Sea; Arctic cod; Gadus morhua; Northeast Arctic cod
• Online Access: https://doi.org/10.3389/fmars.2017.00304; https://doaj.org/article/f1d52f9976c34986ac0891cf97a74192

Observations (1978–1991) of distributions of pelagic juvenile Northeast Arctic cod (Gadus morhua L.) show that up to 1/3 of the year class are dispersed off the continental shelf and into the deep Norwegian Sea while on the way from the spring-spawning areas along the Norwegian coast to the autumn-settlement areas in the Barents Sea. The fate of this variable fraction of pelagic juveniles off-shelf has been an open question ever since Johan Hjort's (1914) seminal work. We have examined both the mechanisms causing offspring off-shelf transport, and their subsequent destiny using an individual-based biophysical model applied to quantify growth and dispersal. Our results show, consistently with the observations, that total off-shelf transport is highly variable between years and may be up to 27.4%. Offspring from spawning grounds around Lofoten have a higher chance of being displaced off the shelf. The off-shelf transport is dominated by episodic events where frequencies and dates vary between years. Northeasterly wind conditions over a 3–7-day period prior to the off-shelf events are a good proxy for dispersal of offspring off the shelf. Offspring transported into the open ocean are on average carried along three following routes: back onto the adjacent eastern shelves and into the Barents Sea (36.9%), recirculating within the Lofoten Basin (60.7%), or drifting northwest to the northeast Greenland shelf (2.4%). For the latter fraction the transport may exceed 12% depending on year. Recent investigations have discovered distributions of young cod on the northeast Greenland shelf indicating that conditions may support survival for Northeast Arctic cod offspring.