Changes to the hydrography and zooplankton in the northern California Current in response to ‘the Blob’of 2014-2015

Fortnightly measurements of hydrography and zooplankton species composition have been sustained along the Newport Hydrographic line since 1996. From this 20 year time series we have established that zooplankton abundance and species composition closely tracks the phase of the Pacific Decadal Oscillation and the El Nino Southern Oscillation. During positive (warm) phase of the PDO, a warm water ‘southern’ subtropical coastal community is found whereas during negative (cold) phase a cold water ‘northern’coastal community dominates. The Blob though was a rule-changer. The Blob began to move slowly ashore at Newport on 14 September 2014 with the seasonal relaxation of upwelling, and within 5 h SST increased 6°C to 19.4°C. On the 25 and 30 September cruises, copepod species richness increased as well, with an anomaly of 2 and 9 species respectively, greater than the 20 year climatology for September. We continued to monitor the plankton throughout the autumn 2014 and winter, spring and summer 2015 and found a total of seventeen copepod species that were either new to Oregon or have occurred only rarely in the past. Many of these species are oceanic with sub-tropical or tropical affinities thus are indicators of tropical waters, suggesting that the Blob water which came ashore in central Oregon had its origins offshore rather than from coastal waters to the south. Some of the copepod species that were new or rarely seen included Subeucalanus crassus, Eucalanus hyalinus, Mecynocera clausi, Calocalanus pavo, Centropages bradyii, and Pleuromamma borealis and P. xiphias. Krill biomass was the lowest in our 20 year time series. The southern California Current neritic krill species Nyctiphanes simplex appears off Oregon during major El Niño events (1983, 1998), but none were seen during The Blob event which again suggests that the origin of the Blob water which appeared off Oregon was from far offshore, not from coastal waters to the south. Note in the figure below that species richness during the Blob period was greater than that observed during the 1997-98 El Nino and lesser El Nino events in 2003-2005 and 2009-10.