The role of climate variability in determining patterns of marine fish
production: a test of the storage effect.

By

Anne B. Hollowed1, Steven R. Hare2, Michiyo Shima3 and Warren S. Wooster4
 

1.  Alaska Fisheries Science Center
7600 Sand Point Way NE
Seattle, WA 98115
 

2.  International Pacific Halibut Commission
P. O. Box 95009
Seattle, WA 98145-2009

3.  School of Fisheries
University of Washington
Seattle, WA 98115

4.  School of Marine Affairs
University of Washington
Seattle, Washington 98115
 

Review of oceanographic and climate data from the North Pacific and Bering Sea
revealed events that occur on three principal time scales: a) 1-5 years (El Nino
Southern Oscillation and interannual variation), b) 6-12 years (decadal scale
variability), and c) 30 years (Pacific decadal oscillation, PDO).  The start and
end date these events was examined on a latitudinal basis.  We examined time
series commercial fishery recruitment data for evidence of coherence with one or
more of the time scales noted in oceanographic and climate data.  Our analysis
revealed that time series of marine fish recruitment can be classified on the
basis of the timing of oceanographic and climate events.  We examine the role of
oceanographic forcing in determining marine fish production and the ecological
balance of species within the system.  Specifically we examine the role of the
ôstorage effectö and longevity in minimum spawner biomass levels.
 

Outline: 30 minutes

1.  Introduction: Climate/Storage Effect.
2.  Ocean variability:  Interannual, decadal, PDO
3.  Timing of events by region
4.  Time series of recruitment
5.  Classification
6.  relationship between longevity, productivity and classification
7.  Evidence for storage effect
8.  Conclusions

Lag-1 Autocorrelations for U.S. West Coast and Alaska groundfish and salmon

Summary of Intervention Analysis

Pre and Post regime shift CVs

Office 97 Excel spreadsheet containing the above tables and figures

Comparison of ENSO and PDO (Powerpoint file)

Map showing 2 degree COADS squares (the squares with dots correspond to the temperature anoms in the next plot.  Dot 1 is the southernmost while dot 34 is the northernmost).

Time-latitude plot of sstanoms from January 1950 (month 1 on time scale) to January 1998 (month 577)
 
A two way table classifying years of El Nino/La Nina and pos. PDO/neg. PDO


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