Water Temperature
Importance to Salmonids
Cool water temperatures are required for salmon survival during all life stages. Water temperature is critical for spawning, egg development, the maturation of fry, juvenile growth, distribution, and survival. Temperatures also significantly influence smoltification, adult migration, and the reproductive health of spawning adults. The relationship of water temperature to salmonids is a function of interactions between temperature, available prey, acclimation, presence of thermal refugia, life stage, and species (CDFG 2002). These factors are site-specific and are best understood in the context of the specific streams in which the factors interact to produce sustainable, sublethal, or lethal conditions for salmonids.
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Riparian canopy cover provides shade to Scott Creek, which helps maintain cooler water temperatures for salmonids.
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For example, acutely lethal temperatures for coho salmon (Oncorhynchus
kisutch) are 28 – 30+° C
(Smith 2003). Sublethal temperatures can reduce or
eliminate coho populations by the metabolic effect
on food intake, increased dissolved oxygen demands,
or the effect on competitive relationships. While
coho are poor competitors at higher water temperatures,
at lower temperatures, they can outcompete steelhead.
Unless food is abundant, mean water temperatures
of about 16° C
with weekly maximums of up to 19° C
are the upper range of temperatures that can sustain
coho (Smith 2003). However, in Waddell Creek in very
productive pools, coho have been found at higher
temperatures (Smith 2003). Steelhead trout (O. mykiss) have
a greater ability to withstand high temperatures.
As long as food is available, steelhead can withstand
means of 20° C
with weekly maximums of up to 24° C. When the water is warm, steelhead
have been observed to use highly productive riffles
to feed in order to meet the increased metabolic
demands of the warmer water (Smith 2003).
Water temperature may be affected by a variety of factors including climate, riparian cover, flows, riparian vegetation, geomorphic features, and human impacts. Temperature becomes a limiting factor when it falls outside the ideal range for a particular life stage. Temperature regimes that support or are deleterious to coho and other salmonids vary across their northern Pacific ranges (CDFG 2002). Sustainable thermal regimes for central coast coho and steelhead probably differ from elsewhere in their respective ranges.
Human Impacts
Anthropogenic impacts affecting factors that affect stream temperatures
include the clearing of riparian and upslope vegetation, the modification
of channel configuration, and the manipulation of stream flow. Although
riparian canopy does not reduce temperatures, the shade provided by
the vegetative cover over the stream maintains the cooler water temperatures
that are so critical to salmonids. The shade from the canopy prevents
the sun from heating the water but does not cause a temperature decrease.
References
California Department of Fish and Game (CDFG). 2002. "Chapter
VI. Factors Affecting the Ability to Survive and
Reproduce. in Status Review of California Coho Salmon
North of San Francisco." Report
to the California Department of Fish and Game Commission.
79-133 pp. View
on-line document.
Smith, J. 2003. "Water Quality Concerns and Central Coast Steelhead
and Coho." 2 pp. View
on-line document.
Local References
Hatch, C.E., F.T. Andrew, J.S. Revenaugh, J. Constantz, C.R. Ruehl, M.
Los Huertos, and C. Shennan. 2002. Time-Series Analysis of Streambed
Thermal Records to Model Surface Water - Groundwater Interaction Within
a Coastal Watershed. Paper presented at American Geophysical Union, Fall
Meeting 2002, Abstract # H61A-0747.
Swolgaard, C. 2001. "Water Quality Monitoring - Chemical Constituents
of Streams." California State Parks Inventory, Monitoring, and
Assessment Program, Wilder Ranch State Park.
General Reference
Berman, C. 1998. "Summary of Temperature Preference Ranges
and Effects for Life States of Seven Species of Salmon and Trout
(Appendix A)." US EPA Region 10.
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