“…The Luderitz upwelling cell off southern Namibia produces persistent offshore advection and cold temperatures. This upwelling system is believed to be a pelagic barrier (Lett, Veitch, van der Lingen, & Hutchings, 2007) to exchange between the northern Benguela stock, which resides in Namibian/southern Angolan waters north of the Luderitz upwelling (Kreiner, Yemane, Stenevik, & Moroff, 2011), and the western, southern and eastern South African stocks located south of the Luderitz upwelling (Idris, Moloney, & van der Lingen, 2016). Sea surface temperatures for spawning between the northern Benguela and western South African stocks differ by up to 3°C (Mhlongo, Yemane, Hendricks, & van der Lingen, 2015).…”