Toward climate-resilient fisheries in the Humboldt Current: Developing a scientific foundation for improved adaptive management

The HCS covers an area comprised of 55° of latitude off Peru and Chile (3°23.57′ to 58°21.02′) and extends over 200 nautical miles offshore. The dynamics of the HCS are strongly influenced by seasonal or permanent coastal upwelling. Several features distinguish the HCS from similar ecosystems associated with the Eastern Boundary Upwelling Systems of the world’s oceans (EBUS: California, Canarias, Humboldt and Benguela). First, it extends closest to the equator. Second, it is the most exposed EBUS system to ENSO, the largest source of interannual climatic variability on the planet. Third, although each of the EBUS has similar levels of primary productivity, the HCS contains the most productive fisheries. Lastly, it is associated with the presence of a shallow, intense subsurface oxygen minimum layer that compresses the oxygenated epipelagic habitat to a few dozen meters. Global warming is altering energy and matter exchange between the atmospheric, oceanic, and continental boundaries.