One of the issues that stimulated the development of this workshop
is the straying of Umatilla River Hatchery fall-run chinook salmon
into the Snake River. I thought that it would be worthwhile
to provide a background on the history of the Umatilla fisheries
restoration program with specific relevance to the straying issue.
I believe this restoration program serves as a good example of
how conflicts can arise when we pursue management activities in
one subbasin that result in unexpected outcomes that conflict
with achievement of objectives in other subbasins--a case in which
we have conflicting cultural and societal demands.
The Umatilla River is located in the northeastern corner of the
State of Oregon and enters the Columbia River at rkm 465, 58 km
downstream from the confluence of the Snake and Columbia Rivers.
Historically, the Umatilla Basin supported populations of summer-run
steelhead, fall- and spring-run chinook salmon, coho salmon (O.
kisutsch), and possibly chum salmon (O. keta). Endemic
stocks of fall- and spring-run chinook and coho salmon are extinct
and summer-run steelhead are depressed.
As a result of these activities, an aggressive restoration and
supplementation program for fall- and spring-run chinook salmon,
coho salmon, and summer-run steelhead was initiated. To guide
this effort, a comprehensive plan for rehabilitation of anadromous
fish in the Umatilla Basin was developed. An extensive planning
and review process was completed under the Northwest Power Planning
Council's Fish and Wildlife Program prior to initiation of the
rehabilitation efforts. This process involved numerous agencies,
tribes, and fisheries experts from the Pacific Northwest to establish
management and research objectives and restoration strategies.
The plan identified specific management objectives to restore
the natural production of fall-run chinook salmon and to meet
tribal treaty obligations. Similar objectives were established
for summer-run steelhead. In both programs, efforts were made
to limit the influence of hatchery stocks on resident and endemic
populations. The reintroduction of anadromous salmon into the
Umatilla Basin, as well as the supplementation of summer-run steelhead,
was implemented only after a long, well thought-out planning process.
In addition, an array of other objectives in the areas of habitat
restoration, flow enhancement, and passage improvement were developed
to improve environmental conditions in the basin. Juvenile and
adult passage improvements have been made at several diversion
dams and ladders. Flow enhancement projects to pump water out
of the Columbia River to replace water diverted for irrigation
are nearing completion, and trap and haul programs are under way
to move adults and smolts up and down the river at times when
river conditions are not suitable for passage.
The largest investment in the rehabilitation effort has been in
the hatchery program, which is considered the cornerstone of the
program. Large-scale production goals were established to meet
the adult objectives that were developed in the rehabilitation
plan. The Umatilla Hatchery was constructed to meet the hatchery
production needs. This facility is located on the shore of the
Columbia River and is supplied with well water. The plan identified
the need for production and release of 7 million juvenile fall-run
chinook salmon annually; however, a full program has not been
achieved, and only about 3 million fall-run chinook salmon have
been released annually. One surprise outcome of the fall-run
chinook salmon hatchery program was the extensive degree of straying
that occurred among adult fall-run chinook salmon that should
have returned to the Umatilla River but returned instead to the
Snake River. Table 1 shows the total escapement to Lower Granite
Dam, and the composition of escapement including the number of
wild fish, numbers of Lyons Ferry Hatchery1 fish, and number of
Umatilla strays. The actual number of Umatilla fall-run chinook
salmon straying into the Snake River was greater than that depicted
in Table 1, because a substantial number entered the Snake River
but did not reach Lower Granite Dam. Several factors likely contributed
to and promoted straying of Umatilla River fall-run chinook salmon.
Early in the program, juveniles were released in the lower part
of the river near the confluence with the Columbia River and were
not acclimated prior to release. Low flows and warm water temperatures
occurred in the fall at the time adults should have entered the
Umatilla River and presumably discouraged adults from migrating
upstream.
We have made a substantial number of improvements in an attempt
to reduce the rates of straying: juveniles are released in the
upper part of the river and are acclimated prior to release; all
fish are marked with magnetized wire and with a unique fin clip
so the fish can be trapped and removed at dams on the Snake River;
and river flows have been increased in fall to provide improved
water quality, greater attraction, and better migration conditions
in the river. It is our belief that these changes will reduce
the straying to an acceptable level. However, only future information
will allow us to determine if we have reduced levels of straying
to acceptable levels.
Table 1. Origin of fall-run chinook salmon returning to Lower Granite Dam from 1990-93. Lyons Ferry = Lyons Ferry Hatchery fish; Umatilla = hatchery fish released in the Umatilla River.
| Number by origin | |||||
| Escapement to | |||||
| Year | Lower Granite Dam | Natural | Lyons Ferry | Umatilla | Other |
| 1990 | 575 | 101 | 308 | 158 | 8 |
| 1991 | 630 * | 318 | 232 | 76 | 4 |
| 1992 | 957 | 620 | 294 | 41 | 2 |
| 1993 | 1,209 | 777 | 227 | 195 | 10 |
Question: Bob Hayman (Skagit System Cooperative): Is there a
reason why you would assume that natural Umatilla chinook salmon
did not also stray into the Snake River before they went extinct?
Answer: Richard Carmichael: We have not assumed anything about historical levels of straying into the Snake River from the natural populations in the Umatilla River Basin. We do know that the Snake River populations are severely depressed and that there is probably an imbalance in these numbers relative to what may have been there historically when Snake River populations were large. Historically, Snake River production probably dwarfed Umatilla River production, and straying from the Umatilla River Basin into the Snake River was not important.
1. This hatchery was established to propagate Snake River fall-run
chinook salmon.