“…In this region, krill are indicative of the juvenile salmon forage base (MacFarlane & Norton, 2002, Wells et al, 2012, 2023), and the condition of juvenile Chinook in the GoF is associated with the availability and spatial distribution of krill (Fiechter et al, 2015; Henderson et al, 2019; Wells et al, 2012). For instance, aboveâaverage years for juvenile growth and survival at sea have been linked to early season upwelling driving high krill abundances and good prey retention in nearshore waters where juvenile Chinook salmon enter the ocean (Fiechter et al, 2015; Wells et al, 2012, 2016, 2020). In contrast, anomalous ocean conditions concomitant with weak or late upwelling can result in warmer ocean temperatures, less spatial heterogeneity of the environment (e.g., reduced upwelling shadows, eddies, and fronts), and reduced prey concentration and availability at the time of ocean entry, each of which has been associated with stock collapses and low survival years for Central California Chinook salmon (Graham & Largier, 1997; Lindley et al, 2009; MacFarlane, 2010; Sabal et al, 2020; Wells et al, 2012, 2016; Wing et al, 1998; Woodson & Litvin, 2015).…”