“…The spring distribution of C. finmarchicus nauplii reflects spawning events occurring immediately after the seasonal ascent migration from the deep hibernation habitats, where the copepodite stage V (CV) dwells for overwintering ( Broms et al ., 2009 ; BagĂžien et al ., 2012 ; Head et al ., 2013 ). The deep water hibernation strategy reduces loss rates due to predation and advective dispersal during winter, but when the population ascends into surface waters and copepodites molt to the sexually mature adult stages in late winter or spring ( Melle et al ., 2014 ), they are subject to high predation risk and surface circulation that may disperse its members over large distances ( Halvorsen et al ., 2003 ; Gaardsted et al ., 2010 ). Thus, the early spring shelf population of C. finmarchicus nauplii is assumed to be advected in from oceanic populations, where highest abundances have been recorded ( Slagstad and Tande, 1996 ; Halvorsen et al ., 2003 ).…”