Salmon in California and Southern Oregon, including these Klamath River fish, generally do not need to migrate to the Gulf of Alaska (see
here). These Klamath and Central California fish just head offshore to grow from Southern Oregon through Central California.
View attachment 133493
These California and Southern Oregon chinook and coho take advantage of the year-round upwelling and resources to grow off the coast of these states. Northern Oregon, Washington, and B.C. fish migrate to the Gulf of Alaska because these areas experience "downwelling" in the winter. Because of downwelling, there is very little phytoplankton = very little food in these areas in the winter. The out migrating salmon swim north to find food. The oceanographic currents set up an upwelling gyre in the Gulf of Alaska.
This difference in salmons' marine behavior is driven ultimately by food supply and that is driven by upwelling vs. downwelling oceanographic conditions. During coastal upwelling, winds from the north combine with the Coriolis effect to drive surface waters offshore and are replaced by colder, nutrient-rich water. Phytoplankton need light + nutrients to grow; they feed krill and copepods which feed bait fish which feed salmon. During coastal downwelling, winds from the south combine with the Coriolis effect to drive warmer, nutrient-poor surface waters against the coast. No nutrients means no phytoplankton and no food web.
This figure shows seasonal changes in several upwelling indices along the Pacific coast (from
here). These indices use seasonal wind directions and intensities to predict the intensity of upwelling. Values greater than 0 indicate that the winds favor coastal upwelling. Negative values favor coastal downwelling. For reference: 45oN = Lincoln City, OR; 42oN = just south of Brookings, OR; 39oN = just north of Point Arena, CA; 36oN = south of Big Sur, CA; 33oN = Solana Beach, CA.
View attachment 133494
At all the California locations, values throughout the year are zero or better, producing year-round upwelling. But at 42oN and 45oN upwelling values are negative in the winter (even worse off WA and B.C.); that means downwelling and that means no phytoplankton. In summer, the winds shift and we experience upwelling off the Washington coast (but not as extreme as California). This seasonal oceanographic regime drives killer whale migrations too. The Southern Resident Killer whales that are scarfing tons of chum salmon in the South Puget Sound right now often migrate as far as Monterey Bay in the winter to feed on Central California chinook; they can't just migrate offshore of Washington because there aren't any overwintering salmon for them to eat.
The "North of Falcon" salmon-harvest negotiations have that name because the salmon from rivers north of Cape Falcon (north of Manzanita / Nehalem) generally migrate to Alaska while stocks from rivers south of Cape Falcon remain off the California or Oregon coasts (roughly...). The fish that migrate to Alaska become a bouillabaisse of stocks that belong to Oregon, Washington, B.C., and Alaska. The negotiations are supposed to determine who gets what...
Steve