Oncorhynchus mykiss exhibit perhaps the most complex suite of life history traits of any species of Pacific salmonid. They can be anadromous or freshwater resident (and under some circumstances, apparently yield offspring of the opposite form). Resident forms are usually called rainbow, or redband, trout. Those that are anadromous can spend up to 7 years in fresh water prior to smoltification, and then spend up to 3 years in salt water prior to first spawning. The half-pounder life history type in southern Oregon and northern California spends only 2 to 4 months in salt water after smoltification, then returns to fresh water and outmigrates to sea again the following spring without spawning. Another life history variation is the ability of this species to spawn more than once (iteroparity), whereas all other species of Oncorhynchus, except O. clarki, spawn once and then die (semelparity).
The most widespread run type of steelhead is the winter (ocean-maturing) steelhead. Winter steelhead occur in essentially all coastal rivers of Washington, Oregon, and California, south to Malibu Creek. Summer (stream-maturing) steelhead, including spring and fall steelhead in southern Oregon and northern California, are less common; for example, on the Oregon coast only the Rogue, Umpqua, and Siletz Rivers have natural populations of summer steelhead. Inland steelhead of the Columbia River Basin, however, are essentially all stream-maturing steelhead; as discussed earlier, these inland steelhead are referred to in terms of A-run and B-run.
Available information for natural populations of steelhead (Table 3) reveals considerable overlap in migration and spawn timing between populations of the same run type. Moreover, there is a high degree of overlap in spawn timing between populations regardless of run type. California steelhead generally spawn earlier than those in areas to the north; both summer and winter steelhead in California generally begin spawning in December, whereas most populations in Washington begin spawning in February or March. Relatively little information on spawn timing is available for Oregon and Idaho steelhead populations. Among inland steelhead, Columbia River populations from tributaries upstream of the Yakima River spawn later than most downstream populations.
Steelhead exhibit great variation in smolt age and ocean age both within and between populations, but there are some trends.
Smolt age--Smolt age discussed here is based on scale and otolith data from adult steelhead. The emphasis on adult steelhead is based on the assumption that fish surviving to spawning age are expressing the successful and adaptive life history strategy for steelhead in a given geographical location. Steelhead from British Columbia and Alaska most frequently smolt after 3 years in fresh water (Withler 1966, Narver 1969, Sanders 1985). In most other populations for which there are data, the modal smolt age is 2 years (Table 4). Hatchery conditions usually allow steelhead to smolt in 1 year; this difference is often used by biologists to distinguish hatchery and wild steelhead. There appears to be an increase in the frequency of naturally produced 1-year-old smolts in the southern portion of the steelhead range (Table 4). Withler (1966) suggested that there may be a latitudinal cline in steelhead smolt age; however, Titus et al. (in press) found no statistical evidence for a latitudinal cline in steelhead smolt age from California to British Columbia.
Ocean age--North American steelhead most commonly spend 2 years (2-ocean) in the ocean before entering fresh water to spawn (Table 5). Populations in Oregon and California have higher frequencies of age-1-ocean steelhead than populations to the north, but age-2-ocean steelhead generally remains dominant. Withler (1966) and Titus et al. (in press) found that ocean age at spawning (and mean adult length) increased with increasing latitude.
Total age--For most steelhead populations, total age at maturity can be estimated by adding the smolt age and saltwater age. However, summer steelhead (especially in the Columbia River Basin) enter fresh water up to a year prior to spawning, and that year is generally not accounted for in the saltwater age designation; for example, a 2-ocean steelhead from the Yakima River may actually have 3 years between smolting and spawning. Table 6 shows the most common life history patterns expressed by North American steelhead from several river basins. Most steelhead in Alaska and British Columbia are 3/2 (smolt age/ocean age) and have a total age of 5 years at first spawning. For coastal steelhead in Washington, Oregon, and northern California, the modal total age at maturity is 4 years (2/2). Central and southern California steelhead appear to spend less time in the ocean, and they are dominated by 3-year-old (2/1) spawners. Complete life history data for southern California steelhead are lacking; however, it appears that it is common for these fish to smolt in 1 year (CDFG 1995). If they only have one ocean year, as neighboring populations to the north do, then adults may be spawning as 2-year-olds (1/1) in this region.
| Life history (frequency) | Sample | |||||||
|---|---|---|---|---|---|---|---|---|
| Population | Run typea | Primary | Secondary | size | Reference | |||
| Alaska | ||||||||
| Karluk River | S | 3/2 | (0.42) | 2/2 | (0.36) | 62 | Sanders 1985 | |
| Anchor River | S | 3/2 | (0.61) | 3/1 | (0.23) | 80 | Sanders 1985 | |
| Copper River | S | 3/2 | (0.73) | 3/1 | (0.10) | 30 | Sanders 1985 | |
| Situk River | S/O | 3/2 | (0.43) | 3/3 | (0.32) | 211 | Sanders 1985 | |
| Sitkoh Creek | O | 3/2 | (0.38) | 3/3 | (0.27) | 497 | Sanders 1985 | |
| Karta River | O | 3/2 | (0.46) | 3/3 | (0.20) | 542 | Sanders 1985 | |
| British Columbia (mainland) | ||||||||
| Babine River | S | 3/2 | (0.62) | 3/3 | (0.17) | 100 | Narver 1969 | |
| Cheakamus River | O | 3/2 | (0.34) | 2/3 | (0.25) | 64 | Withler 1966 | |
| Capilano River | O | 3/2 | (0.40) | 2/2 | (0.26) | 70 | Withler 1966 | |
| Capilano River | S | 3/2 | (0.49) | 3/3 | (0.31) | 86 | Withler 1966 | |
| Seymour River | O | 3/2 | (0.38) | 3/3 | (0.22) | 58 | Withler 1966 | |
| Seymour River | S | 3/2 | (0.48) | 2/3 | (0.24) | 25 | Withler 1966 | |
| British Columbia (Fraser River Basin) | ||||||||
| Coquitlam River | O | 3/2 | (0.49) | 2/2 | (0.23) | 146 | Withler 1966 | |
| Alouette River | O | 2/2 | (0.32) | 2/3 | (0.32) | 131 | Withler 1966 | |
| Chilliwack River | O | 2/2 | (0.31) | 2/3 | (0.31) | 770 | Maher and Larkin 1955 | |
| Chehalis River | O | 3/3 | (0.34) | 3/2 | (0.33) | 111 | Withler 1966 | |
| Coquihalla River | O | 3/2 | (0.49) | 3/3 | (0.18) | 39 | Withler 1966 | |
| Coquihalla River | S | 3/2 | (0.63) | 2/2 | (0.15) | 150 | Withler 1966 | |
| Life history (frequency) | Sample | |||||||
| Population | Run typea | Primary | Secondary | size | Reference | |||
| British Columbia (Vancouver Island) | ||||||||
| Keogh River | O? | 3/2 | (0.40) | 3/3 | (0.19) | 1391 | Ward and Slaney 1988 | |
| Nanaimo River | ? | 2/1 | (0.41) | 3/1 | (0.26) | 228 | Narver and Withler 1974 | |
| Nahmint River | S | 3/2 | (0.71) | 2/2 | (0.19) | 58 | Narver 1974 | |
| Washington | ||||||||
| Skagit River | O | 2/2 | (0.48) | 2/3 | (0.33) | n/ab | WDFW 1994b | |
| Deer Creek | S | 2/1 | (0.95) | 3/1 | (0.05) | n/a | WDFW 1994b | |
| Snohomish River | O | 2/2 | (0.47) | 2/3 | (0.36) | n/a | WDFW 1994b | |
| Green River | O | 2/2 | (0.52) | 2/3 | (0.17) | 100 | Larson and Ward 1954 | |
| Puyallup River | O | 2/2 | (0.61) | 2/3 | (0.28) | n/a | WDFW 1994b | |
| Nisqually River | O | 2/2 | (0.51) | 2/3 | (0.28) | n/a | WDFW 1994b | |
| Hoh River | O | 2/2 | (0.74) | 2/3 | (0.14) | n/a | WDFW 1994b | |
| Quillayute River | O | 2/2 | (0.46) | 2/3 | (0.40) | n/a | WDFW 1994b | |
| Chehalis River | O | 2/2 | (0.66) | 2/3 | (0.15) | 100 | Larson and Ward 1954 | |
| Columbia River Basin | ||||||||
| Toutle River | O | 2/2 | (0.73) | 2/3 | (0.11) | 37 | Howell et al. 1985 | |
| Cowlitz River | O | 2/2 | (0.55) | 2/3 | (0.34) | 56 | Howell et al. 1985 | |
| Kalama River | O | 2/2 | (0.65) | 2/3 | (0.18) | 1363 | Howell et al. 1985 | |
| Kalama River | S | 2/2 | (0.67) | 2/1 | (0.17) | 909 | Howell et al. 1985 | |
| Willamette River | O | 2/2 | (0.92) | 3/2 | (0.08) | 141 | Howell et al. 1985 | |
| Washougal River | S | 2/2 | (0.71) | 2/1 & 2/3 | (0.14) | 7 | Howell et al. 1985 | |
| Wind River | S | 2/2 | (0.58) | 2/3 | (0.26) | 19 | Howell et al. 1985 | |
| Klickitat River | S | 2/2 | (0.75) | 2/1 | (0.14) | 148 | Howell et al. 1985 | |
| Deschutes River | S | 2/1 | (0.35) | 1/2 | (0.22) | 100 | Howell et al. 1985 | |
| Yakima River | S | 2/1 | (0.47) | 2/1 | (0.42) | 64 | BPA 1992 | |
| Wenatchee River | S | 2/1 | (0.65) | 3/1 & 3/2 | (0.12) | 17 | Howell et al. 1985 | |
| Entiat River | S | 2/1 | (0.88) | 2/2 | (0.12) | 8 | Howell et al. 1985 | |
| above Wells Dam | S | 2/2 | (0.41) | 3/2 | (0.24) | 349 | Mullan et al. 1992 | |
| Life history (frequency) | Sample | |||||||
| Population | Run typea | Primary | Secondary | size | Reference | |||
| Snake River Basin | ||||||||
| Clearwater River | S | 2/1 | (0.34) | 2/2 | (0.25) | 510 | Whitt 1954 | |
| S.F. Salmon River | S | 3/3 | (0.49) | 2/3 | (0.31) | 65 | BPA 1992 | |
| Lemhi River | S | 2/2 | (0.86) | 2/1 | (0.09) | 353 | BPA 1992 | |
| Oregon | ||||||||
| Nehalem River | O | 2/2 | (0.73) | 2/3 | (0.08) | 310 | Weber and Knispel 1977 | |
| Alsea River | O | 2/2 | (0.52) | 2/3 | (0.22) | 978 | Chapman 1958 | |
| Siuslaw River | O | 2/2 | (0.67) | 2/3 | (0.16) | 125 | Lindsay et al. 1991 | |
| Rogue Riverc | O | 2/2 | (0.60) | 3/2 | (0.17) | 547 | ODFW 1990 | |
| California | ||||||||
| Klamath River | S | 2/1 | (0.52) | 1/1 | (0.19) | 391 | Kesner and Barnhart 1972 | |
| Mad River | O | 2/2 | (0.69) | 2/1 | (0.26) | 35 | Forsgren 1979 | |
| Jacoby Creek | O | 2/2 | (0.50) | 2/1 | (0.26) | 109 | Harper 1980 | |
| Van Duzen River | S | 1/2 | (0.62) | 1/3 | (0.29) | 58 | Puckett 1975 | |
| M.F. Eel River | S | 2/1 | (0.45) | 2/2 | (0.33) | 82 | Puckett 1975 | |
| Sacramento River | O? | 2/1 | (0.36) | 2/2 | (0.31) | 83 | Hallock 1989 | |
| Waddell Creek | O | 2/1 | (0.39) | 2/2 | (0.30) | 3,888 | Shapovalov and Taft 1954 | |
Determining total age at maturity for inland steelhead of the Columbia River Basin is complicated by variations in reporting methods. Generally, these fish spend a year in fresh water prior to spawning and this is not included in the age designation. Therefore, by adding 1 year after freshwater entry (indicated here as +1), most Columbia River inland steelhead are 4 years old at maturity (2/1+1). An exception is the Klickitat River; if these steelhead also spend a year in fresh water before spawning, they are dominated by 5-year-old spawners (2/2+1). Most of the available age data for Snake River steelhead are based on length frequency; smolt age is often assumed or not reported. The data that are available from scales show a high degree of variability in age structure, from 4-year-old spawners (2/1+1) in the Clearwater River (Whitt 1954) to 7 year-old spawners (3/3+1) in the South Fork Salmon River (BPA 1992).
As noted above, most species of Oncorhynchus die after spawning, whereas O. mykiss may spawn more than once. The frequency of multiple spawnings is variable both within and among populations (Table 7). For North American steelhead populations north of Oregon, repeat spawning is relatively uncommon, and more than two spawning migrations is rare. In Oregon and California, the frequency of two spawning migrations is higher, but more than two spawning migrations is still unusual. The largest number of spawning migrations for which we found data was five, from the Siuslaw River, Oregon (Bali 1959). Iteroparous steelhead are predominately female.
| Spawning migration | Sample | |||||||
|---|---|---|---|---|---|---|---|---|
| Population | Run typea | 1 | 2 | 3 | 4 | 5 | size | Reference |
| British Columbia (mainland) | ||||||||
| Babine River | S | 0.97 | 0.03 | -- | -- | -- | 121 | Narver 1969 |
| Cheakamus River | O | 0.69 | 0.26 | 0.05 | -- | -- | 64 | Withler 1966 |
| Capilano River | S | 0.94 | 0.06 | -- | -- | -- | 99 | Withler 1966 |
| Seymour River | O | 0.95 | 0.05 | -- | -- | -- | 41 | Withler 1966 |
| Seymour River | S | 0.96 | 0.04 | -- | -- | -- | 45 | Withler 1966 |
| British Columbia (Fraser River Basin) | ||||||||
| Coquitlam River | O | 0.95 | 0.03 | 0.02 | -- | -- | 148 | Withler 1966 |
| Coquihalla River | O | 0.94 | 0.03 | 0.03 | -- | -- | 31 | Withler 1966 |
| Coquihalla River | S | 0.94 | 0.06 | <0.01 | -- | -- | 158 | Withler 1966 |
| Washington | ||||||||
| Skagit River | O | 0.92 | 0.07 | 0.01 | -- | -- | n/ab | WDFW 1994b |
| Snohomish River | O | 0.92 | 0.06 | 0.01 | -- | -- | n/a | WDFW 1994b |
| Green River | O | 0.93 | 0.07 | <0.01 | -- | -- | n/a | WDFW 1994b |
| Puyallup River | O | 0.89 | 0.10 | <0.01 | -- | -- | n/a | WDFW 1994b |
| Nisqually River | O | 0.93 | 0.06 | 0.01 | -- | -- | n/a | WDFW 1994b |
| Quillayute River | O | 0.91 | 0.07 | 0.01 | -- | -- | n/a | WDFW 1994b |
| Columbia River Basin | ||||||||
| Cowlitz River | O | 0.96 | 0.04 | -- | -- | -- | 56 | Howell et al. 1985 |
| Toutle River | O | 0.89 | 0.05 | 0.05 | -- | -- | 37 | Howell et al. 1985 |
| Kalama River | O | 0.93 | 0.06 | <0.01 | <0.01 | -- | 1,363 | Howell et al. 1985 |
| Kalama River | S | 0.94 | 0.06 | <0.01 | -- | -- | 909 | Howell et al. 1985 |
| Klickitat River | S | 0.97 | 0.02 | 0.01 | -- | -- | 148 | Howell et al. 1985 |
| Oregon | ||||||||
| Alsea River | O | 0.89 | 0.09 | 0.02 | -- | -- | 1,223 | Chapman 1958 |
| Siuslaw River | O | 0.86 | 0.11 | 0.02 | -- | 0.01 | 125 | Lindsay et al. 1991 |
| Rogue River | S | 0.79 | 0.17 | 0.04 | -- | -- | 4,058 | ODFW 1994d |
| California | ||||||||
| Mad River | O | 0.77 | 0.17 | 0.06 | -- | -- | 35 | Forsgren 1979 |
| Jacoby Creek | O | 0.83 | 0.17 | -- | -- | -- | 109 | Harper 1980 |
| Sacramento River | O | 0.83 | 0.14 | 0.02 | 0.01 | -- | n/a | Hallock 1989 |
| Waddell Creek | O | 0.83 | 0.15 | 0.02 | <0.01 | -- | 3,888 | Shapovalov and Taft 1954 |
aO = Ocean maturing; S = Stream maturing.
bSample size not indicated in reference.
Although we have defined steelhead as anadromous O. mykiss, there are areas where the separation between rainbow or redband trout and steelhead is obscured. In areas where anthropogenic barriers have isolated populations of O. mykiss, these landlocked populations could conceivably residualize (footnote 5) and, therefore, continue to exist in the nonanadromous form. Similarly, the mouths of some rivers in Oregon and California close seasonally, forming lagoons (during droughts, these rivers may remain closed for extended periods of time--even years). Again, landlocked O. mykiss in these systems could residualize. In some inland populations, growth rate can cause O. mykiss to residualize (Mullan et al. 1992); this apparently involves both fish that grow too quickly and those that grow too slowly.