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
––
9²
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.
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.
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
01/21/2009
Web site owner: Northwest Fisheries Science Center