Unsupported Browser Detected

Internet Explorer lacks support for the features of this website. For the best experience, please use a modern browser such as Chrome, Firefox, or Edge.

2022 Year End Summary

December 02, 2022

Summary of ocean conditions for juvenile salmon in 2022

2022 was a mix of good and bad ocean conditions for juvenile salmon in the Northern California Current. Basin-scale indices suggested the coolest, most productive year, with the strongest May – Sept negative PDO value in the time series; and almost three consecutive years of equatorial La Niña conditions. However, local physical conditions pointed to poor productivity. These were largely driven by the latest spring transition, and the weakest upwelling at 45°N in the 25-year time series. This was also reflected in the warm local temperatures during the summer on the shelf.

Figure 1: Cumulative Upwelling from the Bakun Upwelling Index at 45 N. Negative trending lines are indicative of downwelling conditions and alternatively, positively increasing lines are indicative of upwelling conditions.
Figure 1: Cumulative Upwelling from the Bakun Upwelling Index at 45 N. Negative trending lines are indicative of downwelling conditions and alternatively, positively increasing lines are indicative of upwelling conditions. The data have been zeroed at the spring transition (straight lines between March and July) and fall transition (straight lines between September and November). We see that 2022 had the latest spring transition in the time-series and the gentle, almost flat slope through the upwelling season shows how weak conditions were. Credit: NOAA Fisheries

Despite the lackluster upwelling, the northern copepod biomass anomalies and copepod species richness showed signs of cool conditions in the spring and early summer, but the anomalies of northern copepods turned weakly negative by mid-summer, resulting in average biomass anomalies for the May – Sept period. There was moderate upwelling early in the season, from Jan – Mar, that likely drove the early transition of the summer copepod community, and resulted in low species richness. The winter ichthyoplankton indices and juvenile Chinook salmon catches were moderate, and juvenile Coho salmon catches were above average.

 

Figure 2: Times series of 3 month running mean for copepod species richness and the northern copepod biomass montly anomalies. Blue indicates cold water conditions and red indicates trends for warm water conditions. Early on in 2022, there were anomalously less copepod species present and anomalously higher northern, cold water copepod biomass. Credit: NOAA Fisheries
Figure 2: Times series of 3 month running mean for copepod species richness and the northern copepod biomass monthly anomalies. Blue indicates cold water conditions and red indicates trends for warm water conditions. Early on in 2022, there were anomalously less copepod species present and anomalously higher northern, cold water copepod biomass. Credit: NOAA Fisheries

 

While the ocean indicators in 2021 pointed towards greatly improved habitat for juvenile salmon and were a welcomed respite following nearly six years of poor ocean conditions, the mixed signals in 2022 suggest that these improvements may have been short-lived. 

Take care and best wishes to you all,

The OEI Team

Figure 3: A rainbow captured along the Newport Hydrographic Line. Credit: NOAA Fisheries
Figure 3: A rainbow captured along the Newport Hydrographic Line. Credit: NOAA Fisheries
Previous: ­­Oregon Sea Grant Summer Scholar Wrap Up

Last updated by Northwest Fisheries Science Center on January 05, 2023