The Oscillating Control Hypothesis Reassessment in view of New Information from the Eastern Bering Sea George L. Hunt, Jr. School of Aquatic and Fishery.

Slides:



Advertisements
Similar presentations
Columbia River basin juvenile salmonids : survival in the Columbia River Plume and northern California Current, a decade of observations of ocean conditions.
Advertisements

Spatial distribution and ontogenetic movement of walleye pollock in the eastern Bering Sea Presenters: Troy Buckley, Angie Greig, James Ianelli, Patricia.
Plankton changes and cod recruitment in the North Sea Plankton changes and cod recruitment in the North Sea Grégory Beaugrand 1,3*, Keith M. Brander 2,
Potential Approaches Empirical downscaling: Ecosystem indicators for stock projection models are projected from IPCC global climate model simulations.
Change in Ocean Surface Thermal Habitat in a Continental Shelf Marine Ecosystem and Its Affect on Lower Trophic Level Organisms Kevin Friedland, Joe Kane,
Searching for a good stocking policy for Lake Michigan salmonines Michael L. Jones and Iyob Tsehaye Quantitative Fisheries Center, Fisheries and Wildlife.
The Bering Sea Is it just a Warmer Barents Sea? George L. Hunt, Jr. University of California, Irvine and Bernard Megrey NOAA Alaska Fisheries Science Center.
Zooplankton processes Puget Sound Oceanography Jan. 28, 2011.
Growth and feeding of larval cod (Gadus morhua) in the Barents Sea and the Georges Bank Trond Kristiansen, Frode Vikebø, Svein Sundby, Geir Huse, Øyvind.
Variations in source waters which feed
Climate, Ecosystems, and Fisheries A UW-JISAO/Alaska Fisheries Science Center Collaboration Jeffrey M. Napp Alaska Fisheries Science Center NOAA Fisheries.
Science Behind Sustainable Seafood
P. Stabeno, PMEL The Bering Sea What is BEST? A program designed to understand and predict the consequences of climate change for Bering Sea marine ecosystems.
Energy density of Steller sea lion prey in western Alaska: species, regional, and seasonal differences Elizabeth A. Logerwell 1 and Ruth A. Christiansen.
A Critical Review of the “Regime Shift-Junk Food” Hypothesis for the Steller Sea Lion Decline Lowell Fritz and Sarah Hinckley Alaska Fisheries Science.
Megan Stachura and Nathan Mantua University of Washington School of Aquatic and Fishery Sciences September 8, 2012.
Physical effects on plankton and productivity on the Faroe Plateau E. Gaard, B. Hansen, S. K. Eliasen and K. M. H. Larsen Faroese Fisheries Laboratory.
A Multi-Agency Effort to Address Declines in Yellow Perch Abundance in Lake Michigan David Clapp Michigan Department of Natural Resources and Yellow Perch.
Climate and Fisheries Dr. Gordon H. Kruse Director & Professor of Fisheries, Fisheries Division, School of Fisheries and Ocean Sciences, University of.
North Pacific Climate Regimes and Ecosystem Productivity Changing climate, changing ecosystem: Current issues & results.
Introduction Oithona similis is the most abundant copepod in the Gulf of Alaska, and is a dominant in many ecosystems from the poles to the sub-tropics.
Spatial Fisheries Values in the Gulf of Alaska Matthew Berman Institute of Social and Economic Research University of Alaska Anchorage Ed Gregr Ryan Coatta.
Impact of large-scale climatic changes on pelagic ecosystems in the North Atlantic Grégory Beaugrand CNRS, UMR 8013 ELICO Station Marine Wimereux Université.
Introduction Greenland halibut (Reinhardtius hippoglossoides; GH) have declined significantly since the 1970’s in the eastern Bering Sea (EBS). The reasons.
Time series monitoring in Japan (Introduction of Odate collection and Odate project) Hiroya Sugisaki ・ Kazuaki Tadokoro ・ Sanae Chiba.
Stratification on the Eastern Bering Sea Shelf, Revisited C. Ladd 1, G. Hunt 2, F. Mueter 3, C. Mordy 2, and P. Stabeno 1 1 Pacific Marine Environmental.
Centre for Ecological and Evolutionary Synthesis ICES/NAFO Decadal Symposium Santander, Spain May 12th 2011 The serial recruitment failure to North Sea.
James N. Ianelli Alaska Fisheries Science Center Seattle, WA Trends in North Pacific Cod and Pollock.
Physical and related biological variability in the large-scale North Atlantic, with implications for the NW Atlantic Ken Drinkwater Institute of Marine.
Summary Euphausiids (krill) are important food items of fish, seabirds and whales: consequently, it is important to understand their seasonal cycles. The.
SEABIRDS POSTERS 3 - Seabirds as Indicators 2 - Seabird management and conservation.
Distribution of Sardine in US water used for current harvest guideline Nancy Lo (retiree from SWFSC)and Larry Jacobson (NWFCS) PACIFIC FISHERY MANAGEMENT.
New Science – New Regulations Bruce Herbold (EPA) IEP and POD Management Teams.
Climate, zooplankton and pelagic fish growth in the Central Baltic Sea Christian Möllmann © Georgs Kornilovs ® Marina Fetter ® Friedrich W. Köster © ©
Preliminary Data on Euphausiid Distribution and Growth in the Northern Gulf of Alaska. A.I. Pinchuk, R.R. Hopcroft, K.O. Coyle Institute of Marine Science,
Jennifer M. Marsh M.S. Fisheries Student School of Fisheries and Ocean Sciences University of Alaska Fairbanks.
Science Behind Sustainable Seafood Solving the Ecosystem Problem Alaska Fisheries Science Center.
Myths: Salmon and the Sea Limiting factors are all in fresh water, hence marine survival does not vary The ocean has unlimited capacity to support salmon.
Seasonal variations in mean water column temperatures in the northern GOA (obtained from IMS GLOBEC website ). The temperature.
"The Gulf of Alaska Seward Line & 2006 Russell R. Hopcroft, Kenneth O. Coyle, Tomas J. Weigngartner, Terry E. Whitledge Institute.
Egg production rates of the larger copepods in the Gulf of Alaska: Calanus marshallae, Calanus pacificus, Eucalanus bungii and Neocalanus flemingeri Russell.
Obey the LAW: Calanus finmarchicus dormancy explained Jeffrey Runge School of Marine Sciences, University of Maine and Gulf of Maine Research Institute.
North-East Arctic Haddock Melanogrammus aeglefinus (Linne)
Zooplankton (& their environment) off Vancouver Island in 2005 Warm (but not a lot warmer than 2004) Chlorophyll & nutrients low (but enhanced by JdeF.
The Influence of Spatial Dynamics on Predation Mortality of Bering Sea Walleye Pollock Pat Livingston, Paul Spencer, Troy Buckley, Angie Greig, and Doug.
Vertical Distribution and Migration of Zooplankton Stephen M. Bollens School of Biological Sciences, and School of Earth and Environmental Sciences Washington.
1 Federal Research Centre for Fisheries Institute for Sea Fisheries, Hamburg Hans-Joachim Rätz Josep Lloret Institut de Ciències del Mar, Barcelona Long-term.
1 Assessing Vulnerability of Living Marine Resources in a Changing Climate Roger Griffis Climate Change Coordinator, NOAA Fisheries Service.
Distribution and connectivity between spawning and settling locations of Greenland halibut (Reinhardtius hippoglossoides) in the Bering Sea Dongwha Sohn.
Warming climate alters the biogeography of the southeast Bering Sea 1 Joint Institute for the Study of the Atmosphere and the Oceans, University of Washington.
Multispecies Catch at Age Model (MSCAGEAN): incorporating predation interactions and statistical assumptions for a predator ‑ prey system in the eastern.
The influence of climate on cod, capelin and herring in the Barents Sea Dag Ø. Hjermann (CEES, Oslo) Nils Chr. Stenseth (CEES, Oslo & IMR, Bergen) Geir.
The predatory role of the commander squid, Berryteuthis magister, in the eastern Bering Sea ecosystem Mary Hunsicker, Timothy Essington, Kerim Aydin and.
A comparison of copepod egg production rates in the Gulf of Alaska Russell R. Hopcroft.
Egg production rates of Pseudocalanus mimus and Pseudocalanus newmani in the Gulf of Alaska R.R. Hopcroft, C. Clarke, & A.I. Pinchuk Institute of Marine.
Expected Changes in the Climate Forcing of Alaskan Waters in Late Summer/Early Fall Nicholas A. Bond 1 James E. Overland 2 and Muyin Wang 1 1 University.
North Pacific Climate Regimes and Ecosystem Productivity (NPCREP) NOAA Fisheries Ned Cyr NOAA Fisheries Service Office of Science and Technology Silver.
Population Dynamics and Stock Assessment of Red King Crab in Bristol Bay, Alaska Jie Zheng Alaska Department of Fish and Game Juneau, Alaska, USA.
Tracking life history of each particle Particles could be divided into three groups (Fig. 7) The red group’s period of copepodite stage shortened when.
Zooplankton biogeography as a measure of oceanographic change in Canada Basin (Arctic) Brian Hunt 1, John Nelson 2, Fiona McLaughlin 2, Eddy Carmack 2.
Sara Miller Presentation to the PCCRC board January 21st , 2010
Anthony R. Lupo, Professor
Russell R. Hopcroft & Kenneth O. Coyle
Institute of Marine Science, University of Alaska Fairbanks
Lakes & Large Impoundments Chapter 22
Lake Erie Fisheries Community Status: 2013
Climate change research in the Gulf of Alaska
Ken Coyle, Russ Hopcroft & Alexei Pinchuk
Conclusions: Seabird Counts (October 1997)
The distribution of zooplankton, nutrients, chlorophyll, fish and seabirds relative to the major water masses and current regimes on the shelf of the northern.
Presentation transcript:

The Oscillating Control Hypothesis Reassessment in view of New Information from the Eastern Bering Sea George L. Hunt, Jr. School of Aquatic and Fishery Sciences University of Washington Lisa Eisner Ed Farley Jamal Moss Jeffrey M. Napp NOAA Alaska Fisheries Science Center

Where I want to go in this talk Walleye Pollock one of USA’s most important Fisheries Recently, big drop in pollock biomass in Eastern Bering Sea Gap in production of strong year classes What fuels production of young pollock? Role of Sea Ice Long-term consequences

The Bering Sea Russia Alaska Chirikov Basin < 50 m Anadyr Basin Cape Navarin 50-100 m Alaska 100-200 m Inner Domain Commander Basin Aleutian Basin (west) Middle Domain Aleutian Basin (east) Outer Domain Modified from: Aydin et al. (2002) and Mueter unpbl

Importance of Walleye Pollock Fisheries Number 1 species in USA by weight 2,298.1 million pounds; 28% of US fish catch Value $323,212, 000 Dutch Harbor/Unalaska USA Number 1 port for weight (612.7 million lb.) Number 2 port for value ($195 million) Source: NOAA Fisheries website

Pollock Modeled Biomass Source: NPFMC 2010 SAFE, Dec 2009

Ice, Wind, Bloom and Copepods Early Ice Retreat Late Bloom, Warm Water – Large Copepod Biomass Late Ice Retreat Early Bloom, Cold Water – Small Copepod Biomass February March April May June Hunt et al. 2002

Distribution of Age-0 Walleye Pollock loge transformed catch per unit effort (fish/m3) Moss et al., 2009 Trans .Amer. Fish. Soc.

Year Class Strength Variable Source: NPFMC 2010 SAFE, Dec 2009

What were the Assumptions? Warm water good for copepod survival and growth Euphausiids were always available Warm water good for age-0 pollock feeding and growth Fast growing age-0 pollock will have a greater survival to age-1

The Reality Check The warm years did not lead to big year-classes of pollock Baier and Napp 2003 showed that Calanus marshallae needed an early bloom in cold water Perhaps warm years were good for small copepods but not for the big C. marshallae or for euphausiids So- some bad assumptions! NEW DATA NEEDED

July Copepod Abundance Figure Courtesy of J. Napp, NOAA AFSC

Large zooplankton abundance (# per m3), Bongo Tow, 505 μm mesh net 2002 2003 2004 2005 2006 2007 Hyperiids Neocalanus plumchrus & flemingeri Calanus marshallae

Ice, Wind, Bloom and Copepods Early Ice Retreat Late Bloom, Warm Water – Mostly Small Copepods Late Ice Retreat Early Bloom, Cold Water – Large Calanus favored February March April May June Modified from Hunt et al. 2002

Abundance of Age-1 Pollock VS. Age-0 Abundance the prior year From Moss et al., 2009

Age-0 Pollock Energy Density as a function of wet weight From Moss et al., 2009

Diets of Age-0 Pollock in warm and cold years From Moss et al., 2009

New Since 2002 Mueter- Pollock recruitment dome-shaped with respect to temperature Moss et al.- Early pollock survival & growth better in warm years; growth weak in cold years Baier & Napp- Need early bloom, cool water to have big zoops (C. marshallae, T. raschii) Moss et al- Need sufficient energy to survive winter; size & energy density of age-0s critical Predation on age-0 pollock greater when large zoops scarce in summer

Conclusions Variations in timing of ice retreat affect the availability and size of copepods in spring- warm springs have mostly small copepods, but good early survival of age-0 pollock. High numbers of age-0 pollock in summer do not necessarily lead to high numbers of age-1 pollock the next year In warm years, there is a lack of large crustacean zooplankton in summer, age-0 pollock have low energy density, and there is enhanced cannibalism In warm years, summer lack of large zooplankton may result from their failure to recruit in the spring

Impacts of Availability of Large Zoops Warm year with late bloom and few large copepods or euphausiids Cold year with early bloom and abundant large copepods and euphausiids Mesozooplankton Age-0s Year 2 and older Age-1s

Middle Shelf Copepods (No. m-3) August 1999 vs. 2004 Data Type (from Coyle et al. 2008) 1999 (Cold) 2004 (Warm) P value Oithona similis 348 1633 0.000 Pseudocalanus spp. 404 1211 Acartia spp. 277 507 0.264 Centropagus abdominalis (2.96)-03 0.177 Calanus marshallae 44 (8.13)-04 Calanoid nauplii 161 2.69 0.015

July Zooplankton Biomass Figure courtesy of J. Napp / N. Shiga