Oregon Coastal Salmon Restoration Initiative |
The 1982 ODFW Coho Salmon Management Plan identified production
goals for wild coastal coho. Because of a number of factors,
including unfavorable marine survival, these production levels
have never been realized. Much new information is now available
about the factors affecting production of coho salmon. For example,
extensive habitat inventory data are now available, a model has
been developed to estimate coho salmon smolt capacity from habitat
data, spawner numbers are estimated using statistically valid
methods, and there is a better understanding of the effects of
variability in climate on salmon production. New understanding
of the interactions between freshwater and marine survival of
coho salmon is of particular interest to the development of realistic
production goals for wild fish.
Research has demonstrated that the quality of freshwater habitat
(particularly over-winter habitat) has a direct influence on freshwater
survival rate. Habitat and population modeling has demonstrated
that to be equally productive, salmon inhabiting a stream with
poor quality habitat will require a higher rate of marine survival
than salmon inhabiting a stream with good quality habitat. As
a result of these interactions, marine survival plays a dominant
role in determining the productivity and sustainability of coho
salmon populations.
The modeling predicts that extended periods of low marine survival,
particularly combined with high fishery exploitation rates, cause
extirpation of coho salmon from all but the best freshwater habitats.
In fact, this is exactly what is observed today. A prolonged
period of poor marine survival has occurred for coho off Oregon
since the late 1970s. Harvest during this period was also excessive
until the most recent years. Random sampling of coho spawner
abundance indicates that very few stream reaches have large spawner
populations, and that most stream reaches have few or no spawning
coho salmon.
Thus, the concept of a single production goal has become obsolete.
The concept of production potential is more appropriate. Production
potential is the estimated number of adult salmon that might be
expected from a population under a particular set of natural environmental
circumstances. When estimating production potential, both the
quality of the freshwater habitat and the probable levels of marine
survival must be considered. Production potential and range of
coho salmon abundance within a basin would be expected to expand
and contract as marine survival increases and decreases.
The estimates of production potential presented in this chapter were developed based on actual measurements of habitat in individual stream reaches made during the period 1990-95 and two assumed levels of marine survival: 3% and 5% (see Table 1). Therefore, two tiers of freshwater habitat would be capable of supporting coho production, corresponding to the two levels of marine survival.
Table 1. Estimated Production Potential of Current Habitat for Coho Salmon in Oregon Coastal ESUs.
| Basin | Survival | potential | needed | 1992 | 1993 | 1996 | |||||
| Oregon Coastal ESU | |||||||||||
| Nehalem | 1,600 | 4,000 | 1,300 | 2,300 | 2,400 | 1,600 | 1,100 | ||||
| Tillamook | 300 | 3,000 | 300 | 900 | 900 | 300 | 700 | ||||
| Nestucca | 200 | 700 | 700 | 400 | 300 | 1,800 | 500 | ||||
| Siletz | 400 | 1,000 | 2,400 | 400 | 1,200 | 600 | 800 | ||||
| Yaquina | 400 | 400 | 600 | 500 | 2,400 | 5,700 | 4,600 | ||||
| Alsea | 1,200 | 1,600 | 7,000 | 1,100 | 1,300 | 700 | 1,600 | ||||
| Siuslaw | 2,700 | 3,700 | 3,400 | 4,400 | 3,000 | 6,100 | 8,800 | ||||
| Coastal Lakes | 4,400 | 7,300 | 2,000 | 10,100 | 5,800 | 11,200 | 13,500 | ||||
| Umpqua | 3,700 | 3,600 | 2,200 | 9,300 | 4,500 | 11,000 | 14,400 | ||||
| Coos | 2,300 | 3,800 | 15,600 | 15,300 | 14,600 | 10,400 | 12,100 | ||||
| Coquille | 2,700 | 5,600 | 2,100 | 7,400 | 5,000 | 2,100 | 16,200 | ||||
| Direct Ocean | 1,100 | 1,600 | 2,000 | 2,300 | 2,200 | 900 | 4,000 | ||||
| Tributaries | |||||||||||
| Total ESU | 20,900 | 36,300 | 39,700 | 54,400 | 43,700 | 52,400 | 78,300 | ||||
| Transborder ESU | |||||||||||
| Rogue | 2,800 | 800 | 1,900 | 200 | 5,300 | 4,200 | 5,800 | ||||
All estimates of production potential were derived with the assumption
of having fully seeded freshwater habitat, and should be viewed
as potentially achievable levels of production based on
current habitat condition. For the transborder ESU that includes
southern Oregon and Northern California, estimated production
potential was calculated for the Rogue Basin only. Production
potential for coho salmon is thought to be very small in other
Oregon streams in this ESU.
Because estimates of potential production are based on modeling
of freshwater habitat capacity, which relies heavily on winter
habitat conditions, these estimates may be optimistic in some
cases - especially for areas where high summer water temperatures
may occur such as the Umpqua and Rogue basins. Temperature may
be a more severe constraint than winter habitat on populations
in some streams in these basins and limit production below the
maximum levels estimated (see Table 1). Consequently,
current estimates of potential production should be viewed as
giving general guidance. Undoubtedly, this guidance will be revised
in the future as population models are improved and more habitat
data are collected.
To assess the status of a population relative to its potential,
it is necessary to consider its history of relative marine survival.
Potential production levels vary as marine survival changes.
Thus, because marine survival for the last two decades has been
poor and escapement has been reduced by over-fishing, attaining
the production potential of the higher levels of marine survival
will occur only after achieving adequate spawner abundance in
the poor habitat that currently has few, if any, spawners. Achieving
adequate spawner abundance in these poorer habitats may require
that several generations experience improved marine survival and
that the more restrictive harvest controls proposed in this plan
are implemented (see Fish Management Measures in Chapter 17B).
For current habitat conditions, the modeling predicts that wild
coho salmon production could range approximately from 168,000
in 800 miles of habitat to 430,000 in 2,100 miles of habitat in
the Oregon Coastal ESU. Spawner needs are in the range of 126,000
to 235,000. Similarly, production potential for the Rogue Basin
ranges approximately from 7,000 to 29,000 with spawner needs of
5,000 to 14,000.
Recent Population Trends
Since 1990, coho salmon spawner populations in the northern Oregon
Coastal ESU have been estimated using statistically-designed,
stratified random surveys. From 1950 to 1990, populations were
monitored using standard survey sites. Whereas the standard surveys
provided an index of abundance from year-to-year, the new methods
provide actual population estimates. In the Rogue Basin, population
estimates are made from ratios of unmarked fish to marked hatchery
fish collected in a seining operation at Huntley Park in the lower
river.
The populations estimated for each major coastal basin since 1990 are listed in Table 1. Abundance of spawners in the Coos and Coquille basins have been relatively strong since 1992, the first year of substantial harvest reduction on the south coast. In 1995, and especially in 1996, spawning populations in the coastal lakes, and the Umpqua, Siuslaw, and Yaquina basins have also seen substantial increases in abundance. The preliminary estimates for 1996 show a significant increase in total abundance for all but the northern third of the Oregon Coastal ESU. The stronger spawner returns in the southern two-thirds of the ESU do not appear to be due to better habitat quality. For example, based on our habitat modeling, the Coos and Coquille basins have habitat of similar quality to that in the Nehalem and Nestucca basins, respectively, yet had a 15- to 20-fold greater density of spawners in 1996.
Total production of the coastal populations can be estimated by
dividing escapement estimates by one minus the exploitation rate.
Figures 2 and 3 show these estimates for the Oregon Coast ESU
and for the Rogue Basin, respectively. In five of the last seven
years, coastal basins as a whole have been producing coho salmon
at about one-half of their estimated potential, given the poor
marine survival conditions. The primary reason for this reduced
production is lack of adequate spawners. Figure 2 clearly demonstrates
the effects of high exploitation rates during periods of poor
marine survival. In hindsight, exploitation rates of 50% to 70%
experienced by some coastal coho stocks as late as the early 1990s
were clearly too high given the poor marine survival conditions
experienced by the fish. As harvest has decreased, spawner abundance
has increased. Since 1990, there has been a fairly steady increase
in spawner abundance despite a generally flat trend in total production.
Spawner-to-spawner ratios have ranged from 1.2 to 2.6 during
the past four years. Estimated spawner abundance has increased
by about four-fold in two generations (1990-96).
In the Rogue basin, the population has been much more variable
(Figure 3). However, marine survival of hatchery fish has greatly
improved since 1994. Abundance of wild spawners has also increased
dramatically.
Prospects for the Future
The improved survival of coho salmon in the Rogue Basin and in the south and mid-coast basins in recent years are hopeful signs. We know that climate is cyclic and strongly influences marine survival. We have been in a poor survival cycle since 1977. The improved marine survival of coho from the Rogue Basin since 1994, and apparent improved survival in mid-coast basins in
1996 may be precursors of better survival in the near future.
Climatologists predict a return to a wetter climate similar to
that experienced in the 1960s, a period of good survival conditions
for Oregon coho salmon.
So, what trends in production are populations likely to experience
in the future? One possible answer has come from a simple model
of projected populations that would result from the proposed OCSRI
Harvest Strategy. If we consider two assumptions -- that marine
survival will remain poor (average 3%), or that marine survival
will improve (average 5%) -- we can develop a range of possible
outcomes. Starting with the average spawner abundance of 50,000
fish for 1993-95, the model predicts an expected rebuilding trajectory
for spawner abundance in the Oregon Coast ESU at 3-year intervals
(Figure 4) while following the proposed harvest strategy. The
typical cycle of Oregon coho salmon populations is three years
from spawner-to-spawner. Thus, the values for 1998 in Figure
4 represent populations in 1996-98. Based on the model, the spawner
population would be expected to be between 56,000 and 94,000 after
one generation, and between 75,000 and 216,000 after four generations.
The estimated returns for 1996 fall near the upper boundary of
this predicted range after one generation.
A second answer to the question of where populations are likely
to go in the future comes from a more sophisticated habitat-based,
life cycle model. This model is based on the reach-level habitat
data used to estimate production potential and incorporates a
range of probable variation in survival at each life stage. The
model also includes factors for straying of spawners, multiple
spawning periods, sex ratio, redd failure, and loss of genetic
fitness at low population size. Populations were modeled for
ten generations using average marine survival rates and for 33
generations using a cyclic pattern of marine survival. (A detailed
description of the model and results are presented in ODFW Attachment
1.)
Populations in the Yaquina, Coos, and Tillamook basins were analyzed
using the model. These basins have the best, an intermediate
level, and poorest habitat in the northern Oregon coast ESU, respectively.
Results suggest that future population abundance will be heavily
influenced by marine survival and by exploitation rate when marine
survival is low. Only the habitats with high productivity remained
viable when marine survival was low. Therefore, distribution
and abundance of fish was a function of long- and short-term variability
in marine survival and long-term patterns of habitat quality.
Within a reach, populations were resilient, unless numbers dropped
to a level where demographic risk factors became more important
than density dependent population dynamics. Persistence of populations
in a basin during periods of poor marine survival depended on
the highest quality reaches.
The model predicts that there is a high probability of persistence
of coho populations in all major basins of the northern Oregon
coast ESU for the next century if habitat condition remains as
it is today. The model was also used to predict risk of extinction
assuming future declines in habitat quality ranging from 10% to
60%.
Based on these analyses, the model predicts that there would be
a substantial increase in the risk of extinction (population of
< 50 spawners occurring at any time) in basins with
poor quality habitat, such as the Tillamook if habitat quality
over the next century declines by 30-60%. This would probably
also be the case in the Nestucca, and Coquille, based on an evaluation
of habitat quality (see Figure 1). Similar declines in the quality
of habitat in the remaining major basins in the northern Oregon
coast ESU would not result in an appreciable decrease in the probability
of persistence of coho salmon populations in those basins. However,
decreased habitat quality would result in smaller populations.
Summary
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