The Blob, El Niño, La Niñas, and North Pacific marine ecosystems Laurie Weitkamp Northwest Fisheries Science Center Newport Field Station NOAA Fisheries Laurie.weitkamp@noaa.gov
Bill Peterson s Big Picture: Large scale forces and local scale processes affect local biological process Alaska PDO and NPGO British Columbia 65N 60 55 50 Local Conditions Upwelling Spring Transition Coastal currents ENSO U.S.A. 45 40 35 30 25 170 W 160 150 140 130 120 110
Bill Peterson s Big Picture: Large scale forces and local scale processes affect local biological process Alaska 65N 60 PDO and NPGO British Columbia 55 50 hake Local Conditions Upwelling Spring Transition Coastal currents ENSO U.S.A. 45 40 35 30 25 170 W 160 150 140 130 120 110 pyrosomes
Today s talk 1. Physical conditions across the North Pacific 2. Biological response to physical conditions 3. Forecasts
1. Physical conditions across the North Pacific Why the blob formed El Niños/La Niñas Recent sea surface temperature (SST) anomalies
Terminology: Anomaly Actual sea surface Anomalies are values with the seasonal SST anomalies trend temperature removed (SST) Value (temperature) positive anomaly Current values Seasonal trend negative anomaly Time http://polar.ncep.noaa.gov/sst/ophi/
How the blob formed Winter storms mix and cool the ocean Heat transferred to atmosphere STRONG WIND Vertical mixing Nutrients to photic zone High nutrients cold water Heat transferred to depth
Formation of the warm blob (Winter 2013/14): Unusually stationary high pressure over the North Pacific blocked storms, which limited vertical mixing Ridiculously resilient ridge Heat transferred to atmosphere STRONG WIND Warm, Nutrients lownutrient surface photic zone to Vertical mixing waters = the blob Atmospheric pressure anomalies, Nov 1, 2013-Jan 9, 2014 High nutrients cold water Heat transferred to depth
Formation of the warm blob (Winter 2013/14): Unusually stationary high pressure over the North Pacific blocked storms, which limited vertical mixing Heat transferred to atmosphere STRONG WIND Warm, Nutrients lownutrient surface photic zone to Vertical mixing waters = the blob High nutrients cold water Heat transferred to depth
El Niños and La Niñas: Tropical phenomena that impact global weather Typical Pacific Northwest Impacts El Niños: Warm winters (low snow) La Niñas: Cold & wet winters Recent Events 2015/2016 El Niño was one of the largest on record but oceanic teleconnections to our area were weak 2016/2017 La Niña was weak and short lived 2017/2018 La Niña is slightly stronger but rapidly fading
North Pacific surface temperature anomalies Jul 14 Oct 14 Jan 15 Apr 15 Jul 15 The blob Oct 15 Jan 16 Apr 16 Jul 16 Oct 16 El Niño Jan 17 Apr 17 Jul 17 Oct 17 La Niña Jan 18 La Niña http://polar.ncep.noaa.gov/sst/ophi/
SST anomalies, 8 April 2018 http://polar.ncep.noaa.gov/sst/ophi/
2. Biological response to physical conditions Highlights Extremes across the N Pacific Observations from local waters Adult salmon returns, AK to CA Bottom line: Huge response across N Pacific from diatoms to marine mammals; effects still continue Joe Orsi (AFSC) with ocean sunfish in SE Alaska, June 2015
Biological response to warm oceans Tropicals In Oregon Species range extensions from CA to AK Dramatic changes to food webs Domoic acid closes crab and clam fisheries AK-CA Young Chinook & coho in ocean very skinny
Tropicals In Oregon Dramatic changes to food webs Biological response to warm oceans Species range extensions from CA to AK 2016 Red pelagic crabs in Oregon! Anchovies invade the Salish Sea Domoic acid closes crab and clam fisheries AK-CA Changes to food webs continue Young Chinook & coho in ocean very skinny Crab and clam fishery closures
Tropicals In Oregon Dramatic changes to food webs Domoic acid closes crab and clam fisheries AK-CA Biological response to warm oceans Species range extensions from CA to AK 2016 Red pelagic crabs in Oregon! Anchovies invade the Salish Sea Changes to food webs continue High Pacific lamprey counts at Bonneville Dam Pyrosomes explode AK-CA Swordfish off Vancouver Island Extremely low Pacific cod abundance in Gulf of Alaska Young Chinook & coho in ocean very skinny Crab and clam fishery closures Crab and clam fishery closures
Biological response to warm oceans (cont) Pyrosomes still here! March 2018 off the WA/OR coasts S OR/N CA crab and razor clam fisheries closures due to domoic acid continue
Unusual abundances of many fishes in NWFSC Salmon Surveys Surveys in May & June 1998-present
Unusual abundances of many fishes in NWFSC Salmon Surveys Log (CPUE + 1) 0.16 0.14 0.12 0.10 0.08 0.06 0.04 0.02 0.00 Pacific Pompano Pacific pompano 98 99 00 01 02 03 04 05 06 07 08 09 10 11 12 13 14 15 16 17 Year Juvenile rockfish Also unusual abundances of: Jellyfish Squid Pacific mackerel Pacific hake 0.25 Jack Mackerel Age 0 fish = Salmon prey Log (CPUE + 1) 0.20 0.15 0.10 0.05 Jack mackerel Age 1-2 fish = Salmon competitors 0.00 98 99 00 01 02 03 04 05 06 07 08 09 10 11 12 13 14 15 16 17 Year Morgan et al. in prep. Age 3+ fish = Salmon predators
Coho survival (OPI) 1 year later Spring Chinook counts at BON 2 yrs later Extremely low juvenile salmon abundances in 2017 will likely result in poor adult returns in 2018 & 2019 ~95% Columbia River spring stocks Juvenile Chinook in surveys Juvenile coho in surveys Mix of Columbia River, WA & OR coast fish
Unusual adult salmon observations in 2015 Interior Fraser & Salish Sea coho extremely low abundance, small body size, and low fecundity Columbia & Oregon coast coho lowest returns since 1990s Oregon coast Chinook returns high
Unusual adult salmon observations in 2016 Alaska pinks: lowest returns in memory Fraser sockeye lowest on record High chum returns WA & OR coasts, Columbia Fraser chum highest in 20 years Lowest Klamath Chinook return since early 1990s
Unusual salmon observations in 2017 Alaska: Highest chum harvest ever, high pink & sockeye returns (best in W AK) Lowest SE AK Chinook ever Fishery closure for Chinook from BC, WA, OR 2 nd lowest Fraser sockeye on record 2 nd lowest Fraser pink return ever Lowest steelhead returns to OR Coast ever Fishery closure for Klamath Chinook Lowest Central Valley wild fall Chinook return ever
Sea bird die-offs Cassin s Auklets off WA/OR coasts, Winter 2014 Common murres, N. California to Alaska, summer 2015 Cent Alaska Fulmars and shearwaters, Bering Sea, summer 2017
Bad conditions elsewhere can affect our area: California sea lions left S. California for the Columbia 2015: starving sea lion pups in California Source: Bryan Wright, ODFW
Changing behavior? Humpback whales entering large coastal estuaries 2015 2016 2017 Humpback whales in Columbia estuary Humpback whales in the Columbia estuary & San Francisco Bay Humpback whales in San Francisco Bay & Columbia River again! Increased entanglements in crab gear in 2015 & 2016
4. Forecasts Spring 2018 SST forecasts
Forecast SST anomalies NOAA Climate prediction Center coupled forecast model 2 May-Jun-Jul 2018 Jul-Aug-Sep 2018 Sep-Oct-Nov 2018 http://www.cpc.ncep.noaa.gov/products/cfsv2/cfsv2seasonal.shtml
Summary Warm ocean waters present since 2014 still continue across large parts of the North Pacific Ocean Biological response to warm ocean has been huge Effects observed at all levels of marine ecosystem Expect biological effects of warm ocean conditions to continue for several years Big concern for 2018 coho and 2019 Chinook returns because of low 2017 juvenile abundances Big recruitment of hake & mackerel off WA/OR will they stay? Residual effects on other species (e.g., crab, groundfish) uncertain Forecast for warm coastal waters in summer 2018 won t be good for cold water species (salmon, crab) but should benefit warm water species (tuna, sardines, squid).
Questions? Sea lions in Astoria, Oregon