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Adult Returns



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 •2008 Annual Update
 •January 2009 Forecast
 •Adult Return Data

Large–scale Ocean and Atmospheric Indicators

 •Pacific Decadal Oscillation (PDO)
 •Multivariate El Niño Southern Oscillation Index (MEI)
 • Basin-scale winds

Local and Regional Physical Indicators

 •Sea surface temperature anomalies
 •Coastal upwelling
 •Physical spring transition
 •Deep–water temperature and salinity

Local Biological Indicators

 •Copepod biodiversity
 •Northern copepod anomalies
 •Copepod community structure
 •Biological spring transition
 •June spring Chinook
 •September coho
 •Zooplankton species composition

Indicators Under Development

 •A second mode of North Pacific sea surface temperature variation
 •Phytoplankton biomass
 •Euphausiid egg concentration, adult biomass, and production rates
 •Interannual variation in habitat area
 •Forage fish and Pacific hake abundance
 •Salmon predation index
 •Potential indices for future development

Introduction to Pacific Northwest Oceanography

 •Physical oceanographic considerations
 • Climate–scale physical variability

Ocean Sampling Methods

 •Hydrography, zooplankton, and ichthyoplankton
 •Juvenile salmon sampling

Acknowledgements

References

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Glossary

 


Adult Returns of Chinook and Coho Salmon


For specific stocks of Chinook and coho, the proportion of adult returns from a particular juvenile year class is not often available.  To obtain this information, one would first need to know the number of juveniles that survived to migrate to the ocean, and then wait 0.5–2 years for coho or 1–5 years for Chinook to obtain the number of returning adults (Healy 1991; Sandercock 1991). 

Even then, it would be difficult to distinguish the proportion of fish that died prior to entering the ocean vs. those that died at sea.  Therefore, adult return data that is available, such as counts at dams or traps, can be used only as an index or surrogate measure of abundance.  With these caveats in mind, we present adult return data from various sources with which to compare forecasts based on ocean indicators. 

The table below is color–coded according to ranks of adult return data from each year for which we have corresponding ocean indicator data.  Lower numbers indicate higher returns of fish, and returns among years were ranked against one another, with 1–4 coded green, 5–7 yellow, and 8–11 red. 


 
Adult returns by Year of Ocean Entry¹
  OPIH Coho
(adults:smolts)
Bonneville spring Chinook (n) Bonneville fall Chinook (n) Klamath River fall Chinook(n est.)
 
1998 9 4 5 1
1999 6 1 3 5
2000 1 2 1 3
2001 4 3 2 4
2002 2 5 4 7
2003 3 8 7 6
2004 8 7 8 8
2005 7 9 6 2
2006 5 6 –– 9
2007 10² –– –– ––
2008 –– –– –– ––
 
¹  Counts of spring and fall Chinook are lagged by 2 and 3 years, respectively.  Return ratios for coho are lagged by 1 year.
² Estimate based on jack returns.

Data used in the rank scores above are shown in the chart below.  Note that counts of spring and fall Chinook salmon at Bonneville Dam are shown lagged by 2 and 3 years, respectively.  For example, the number listed for spring Chinook in 1998 indicates fish that returned in 2000.  Note also that return numbers of a single year may represent multiple age classes:  spring Chinook that returned as adults in 2000 may have entered the ocean in 1998, 1997, or 1996. 


 
Adult returns by Year of Ocean Entry¹
  OPIH Coho
(adults:smolts)
Bonneville spring Chinook (n) Bonneville fall Chinook (n) Klamath River fall Chinook (n est.)
 
1998 0.0128 177,741 400,205 617,573
1999 0.0209 391,367 473,786 357,085
2000 0.0460 268,813 610,075 514,524
2001 0.0258 192,010 583,224 401,092
2002 0.0399 168,656 415,684 160,243
2003 0.0281 74,038 299,161 190,568
2004 0.0177 96,456 157,784  88,652
2005 0.0196 66,624 315,080 521,412
2006 0.0219 126,615 ––  31,600²
2007 0.0095² –– –– ––
2008 –– –– –– ––
 
¹ Counts of spring and fall Chinook are lagged by 2 and 3 years, respectively. Return ratios for coho are lagged by 1 year.
² Estimate based on jack returns.

Age at maturity of Chinook salmon may differ depending on genetics, stream of origin, migration timing, and a number of other factors (Myers et al. 1998).  Therefore, lag times for spring and fall Chinook may vary:  those used here were selected based on age–class of the largest proportion of runs for which we had corresponding information (Whiteaker and Fryer 2007).  For coho salmon, age at maturity is more constant within a given area and varies within a shorter time frame (Sandercock 1991; Weitkamp et al. 1995).  Lag times for coho will likely remain at 1 year.

Estimates of SARs for OPIH coho and adult counts for Klamath River fall Chinook were provided by the Pacific Fishery Management Council (PFMC 2008).  Counts of spring and fall Chinook at Bonneville were provided by the Columbia River DART project (1996–present).  These sources are publicly available via the internet.

Note also that these estimates were not adjusted for catch in the fisheries, which can have a major impact on adult numbers.  For example, in 2005, the subyearling Chinook fishery in the the Klamath River was closed, and adult numbers were far higher than in either the preceding or following year.  This was likely due to the fishery closure, which would have masked any change related to ocean conditions or other factors. 








last modified 01/14/2009

                   
   
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