See
also:
Addressing Sediment as a Limiting Factor
Flow Regimes
as a Limiting Factor
While the specific flow requirements of salmonids vary for each species,
local populations of salmon and steelhead have additionally evolved the
necessary physiological and behavioral characteristics for them to survive
the dynamic flows encountered during each phase of their life history
at a specific time of the year. Flow regimes are one of the most important
drivers of habitat structure at micro-, reach, and riverscape scales.
During critical stages while eggs incubate, young fry forage or drift,
and adults struggle to return to spawn, the relationship between flow
volume and velocity demonstrates the importance of a variable flow pattern
over daily, seasonal, and annual time periods that is critical for the
long-term persistence of salmonid populations. A critical review by Bjornn
and Reiser (1991) summarized a majority of the known literature concerning
flow regimes and their relationship to salmonid habitat.
Predation, fishing, and disease are pressures facing most local salmon
and steelhead populations, yet the potential difficulty of finding preferred
spawning habitat is also a significant limiting factor. The volume and
velocity of water within a watershed is often a cue for initiating spawning
migration, and is the fluid boundary which limits redd construction. Culverts
present difficulties for adult and juvenile salmonids migrating upstream,
though the extent to which this is a barrier to passage often depends
upon a particular species leaping ability. Flows can be problematic in
streams and rivers even when the watercourse does not pass through culverts.
A shift in the peak flows may strand salmonids in the wrong portion of
a watershed preventing them from reaching spawning habitatand potentially
subjecting them to predation while waiting for additional flows to pass
further into the watershed or forcing them to spawn in lower reaches where
egg survival is limited. Although there appears to be little observational
data about minimum depths necessary for passage, a minimum depth of 12
cm for trout, 18 cm for steelhead and coho salmon, and 24cm for Chinook
salmon are considered necessary for passage (Bjornn and Reiser 1991).
FishXing (http://www.stream.fs.fed.us/fishxing/resources.html)
is an awesome resource, in both English and Spanish, which allows the
user to evaluate and design fish passable culverts.
The
timing and velocity of flows during spawning are critical characteristics
of spawning reaches, and poor flow conditions can limit the survival of
eggs and alevins. In locations like Butte Creek, redd imposition may limit
the survival of earlier spawning Spring Run Chinook salmon, which are
an important genetic component of this distinct stock of California Chinook
salmon. With adequate management of flows released from upstream hydroelectric
facilities, the quantity of spawning gravels available to Butte Creek
Spring Run Chinook could be increased and egg survival potentially increased.
Most salmonids need water depths of at least 15cm, though this is also
variable and dependent on spawner density and possible upwelling and hyporeic
flows. Smith (1973) described the depth and velocity characteristics of
1,170 redds of 10 species of salmonids, including all the species in California.
Regardless, flows need to be sufficient to not limit the velocity of oxygen-rich
water through the stream’s hyporeic zone. Kondolf (2000) suggested
a unified approach for assessing the impacts of sediment during the critical
spawning, incubation, and emergence stages and incorporated a life-stage
specific evaluation of gravel and flow requirements.
Flow and water depth are also critical determinants of rearing habitats
for fry, parr, and adult residents and together comprise the amount of
habitat available to salmonids in streams. High flows can be responsible
for side-and off-channel habitat formation, which provide critical micro-habitat
for rearing. Flow regime is one of the factors dictating salmonids emigration
from freshwater to the ocean. While long-term flow increases are likely
necessary to support a steady rate of out-migration of populations far
from the ocean, even small short-term increases can be an important stimulus
for coho and Chinook salmon. Beechie et al. (1994) determined that 73%
of summer habitat loss and 91% of winter habitat losses for a coastal
Washington population of coho salmon were associated with hydromodifications
associated with agriculture and urban lands. NMFS (PCSRF 2005) ranked
degraded freshwater habitats and flows as moderate limiting factors to
coho salmon recovery. The return of a dynamic, natural flow regime
will be critical to minimize the threats of these limiting factors. Roni
et al (2002) reviewed strategies for restoration and suggested a tiered
watershed approach that first restored connectivity, then returned natural
hydrologic and geologic variability and processes, before finally focusing
on instream restoration that is necessary for salmonid recovery.
Bjornn, T.C. and Reiser, D.W. 1991. Habitat Requirements of salmonids
in streams. Pages 83-138 in W.R. Meehan, editor. Influences of
forest and rangeland management on salmonid fishes and their habitat.
Special Publication 19. American Fisheries Society, Bethesda, MD.
Beechie, T.J., Beamer, E. and Wasserman, L. 1994. Estimating coho salmon
rearing habitat and smolt production losses in a large river basin, and
implication for habitat restoration. North American Journal of Fisheries
Management 14:797-811.
Kondolf, G.M. 2000. Assessing salmonid spawning gravel quality. Transactions
of the American Fisheries Society 129: 262-281.
PCSRF (Pacific Coast Salmonid Restoration Fund). 2005. 2005 Report to
Congress, 2000-2004.
Roni, P, Beechie, T.J., Bilby, R.E., Leonetti, F.E., Pollock, M.M., and
Pess, G.R. 2002. A review of stream restoration techniques and a hierarchical
strategy for prioritizing restoration in Pacific Northwest Watersheds.
North American Journal of Fisheries Management 22:1-20
Smith, A.K. 1973. Development and application of spawning velocity and
depth criteria for Oregon salmonids. Transactions of the American Fisheries
Society 102:310-316.