Drift, growth, and survival of larval Northeast Arctic cod with simple rules of behaviour

By Frode Vikebø, C. Jørgensen, T. Kristiansen, Ø. Fiksen. 2007

162 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Nature and Landscape Conservation

View Paper: https://www.semanticscholar.org/paper/100e2f5d2a3ee41e4f8f9115813aeafdf4787966

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In Atmospheric Science

In Global and Planetary Change

In Nature and Landscape Conservation

Citations in the corpus

Manual of recommended practices for modelling physical – biological interactions during fish early life (2009, background): “For heterogeneity of the current field to be exploited, vertical swimming with some sort of criteria to choose depth should be modelled (Vikebø et al., 2007; Fiksen et al., 2007).”
Cod, haddock, saithe, herring, and capelin in the Barents Sea and adjacent waters: a review of the biological value of the area (2010, background): “, 2002), annual surface currents, and larval behaviour (Vikebø et al., 2007).”
A review of early life history dynamics of Barents Sea cod (Gadus morhua) (2014, background): “In shallow parts of the water column, there is a higher chance of capturing prey due to increased light, but at the same time a higher risk of being eaten (Fiksen et al., 2007; Vikebø et al., 2007; Kristiansen et al., 2009a).”
Modelling larval fish navigation: the way forward (2014, background): “Other recent studies have used more 71 complex rule-based behaviours to move larvae vertically in search of food or to avoid predators, and 72 have examined the ecological tradeoffs of these individual behavioural choices (Fiksen et al., 2007; 73 Kristiansen et al., 2009; Vikebø et al., 2007).”
Vertical salmon lice behaviour as a response to environmental conditions and its influence on regional dispersion in a fjord system (2014, background): “However, as the current shear close to the surface often is strong (Myksvoll et al. 2011, Asplin et al. 2014), and vertical migration patterns sometimes yield large dispersal effects (Fiksen et al. 2007, Vikebø et al. 2007), this behavioural re - sponse remains important to consider.”
Impacts of climate change on the complex life cycles of fish (2013, background): “Cod in the eastern Barents Sea generally spawn in the coastal areas 548 from Lofoten northwards, while the western Barents Sea and West Spitzbergen 549 component spawn farther offshore and in the areas south of Lofoten (Randa, 1984; 550 Godø, 1986; Vikebø et al., 2007).”