• Christina Morrisett

Winter on the Henry’s Fork: Flow, Temperature, and Trout

By Christina Morrisett and Rob Van Kirk


During the Thanksgiving Holiday, we received a number of calls from concerned anglers about low flows and ice formation on the Henry’s Fork downstream of Island Park Dam. There is no question about it—flows are low; that’s not unexpected following the driest water year since 1941 (see previous blogs and newsletters for details). However, flows are higher than expected given how dry it is, and temperatures have actually been fairly mild compared to other winters when flows were low.


But, your questions and concerns motivated us to dig into the scientific literature and data and provide information on relationships among winter flow, temperature, and trout survival on the Henry’s Fork. We spent most of this week putting together some information we hope will help answer questions and ease fears about the combined effects of low flows and cold temperatures on trout survival in the Henry’s Fork.

Our road-map for this extensive blog post is:

  1. Basic aspects of winter trout ecology.

  2. Winter ecology of trout in the Caldera reach of the Henry’s Fork.

  3. Relationship between winter flow and the size of the wild trout population in this reach of the river.

  4. Procedure used to determine management of Island Park Reservoir in the winter.

  5. River flows during the winter of 2015-2016.

  6. Temperature during last week’s cold spell and projections for the winter of 2015-2016.

And, if you do not have time to read the entire post, here is a summary of our primary conclusions.


Summary

  1. While the combination of flow and temperature that resulted in last week’s icing event was below average, it was not extreme in either magnitude or duration and should have little if any effect on the trout population.

  2. Winter flow is going to be much lower than average this year but nowhere near what would be expected based on the extreme drought we are experiencing.

  3. Although it is impossible to quantify how much water was used or saved by every single management decision and weather event that happened during 2015, extremely precise management and informed decision-making around the Chester turbine flow test increased winter flows by a whopping 34%, increasing projected trout recruitment in 2017 by 18%.

Read on to see how we came up with these!


The basics of winter trout ecology

Trout are what biologists call poikilotherms or ectotherms, meaning that trout cannot regulate their own body temperatures. Thus, their body temperature and metabolic rates are determined by water temperature. Because of this, trout become most stressed when temperatures are at their extremes—very cold or very warm. The effect of warm water temperatures is often compounded by low dissolved oxygen and presence of large numbers of active predators at that time of year, but that’s a topic for a future blog.


As water temperatures cool, a trout’s metabolism slows and it becomes less active. Smaller fish are affected first, becoming fairly inactive when water temperatures fall into the 40s (Fahrenheit). Larger fish will remain more active in cooler water but eventually will become less active as water temperatures fall into the 30s. When this happens, trout need very little food, which is a good thing, since food availability declines substantially during the winter. On the other hand, slow metabolic rates mean that fish cannot move quickly to avoid predators or rapidly changing flow and habitat conditions like they can in the summer. Despite the fact that many common avian (bird) predators migrate away from cold climates in the winter (e.g., osprey), numerous bird and mammal predators remain present and active throughout the winter in the Rocky Mountains. Generally, winter flows in Rocky Mountain trout streams are very stable, with two exceptions: during periods of rapid ice formation and break-up, and in regulated rivers when abrupt flow changes are made at dams or diversion points.


To minimize their vulnerability to predation and to rapidly changing flow conditions, trout move out of preferred summer-time feeding areas and to favorable winter habitat conditions during fall, as flows fall toward their winter baseflow levels, temperatures drop, and the last major insect hatches of the autumn wane. Adult trout seek slow, deep pools that contain large cobbles and boulders. Juvenile fish seek spaces within cobble-boulder substrate and spaces formed by woody vegetation and rocks along streambanks. Trout of all ages will also seek areas of the river where groundwater inputs moderate winter water temperatures and prevent ice formation. When fish are in good condition going into the winter and suitable and stable habitat is available to them, survival rates can be quite high for the individuals that find and claim this habitat. Fish that are in poor condition or are unable to compete with the more healthy fish for the best cover in a given river reach will generally just move out of that river reach in search of better habitat elsewhere. Fish that move or find themselves in less suitable habitat will experience higher mortality rates than the others, but this mortality is a natural feature of population dynamics in wild trout populations. For a detailed presentation of rainbow trout population dynamics and mortality in the Henry’s Fork (see Rob's blog). Fish that survive the winter in suitable winter locations will then move back into favorable habitat the following summer. In many trout streams, particularly those with abundant food supply and good spawning and rearing habitat, the amount of habitat available during the winter sets the carrying capacity for the fish population as a whole. This is what we call the “limiting factor” on the population.


Ice formation is a regular feature of seasonal cycles in habitat characteristics in most trout streams in high latitudes and high altitudes, and trout have evolved with this phenomenon. The physics of ice formation and its effect on habitat conditions are complex, but here we will just briefly discuss three kinds of ice. The first is surface ice, which is the most common type of ice seen on the Henry’s Fork and other streams in our area. Surface ice generally forms in low-velocity reaches of the river when air temperatures are cold for extended periods. Surface ice frequently forms on the Harriman Ranch and Pinehaven reaches but can extend upstream through Last Chance. Surface ice also frequently covers all or part of the stream channel on the Henry’s Fork in the Coffee Pot area, upstream from Ashton Reservoir, and in the St. Anthony area. Surface ice forms on the lower few miles of Fall River every winter. Surface ice is also common on reaches of the Madison, Gallatin, upper Snake, South Fork, and main Snake. Upon initial formation of surface ice, water continues to flow underneath the ice, and in fact, research has shown that trout actually use surface ice as cover from overhead predators. In small streams, snow that accumulates on top of surface ice can bridge the water surface, insulating the water from the atmosphere and providing stable overhead cover during the middle of the winter. In larger rivers, surface ice usually forms and melts in cycles throughout the winter as weather conditions change.


A second type of ice is anchor ice, which forms when ice suspended in the water column (frazil ice or “slush”) freezes onto the stream bottom. This type of ice often forms in higher-velocity areas, where turbulence forces frazil ice that has formed at the surface down to the bottom of the stream. Anchor ice has a greater negative effect on available trout habitat than surface ice because anchor ice fills in the spaces among cobble-boulder substrate and woody debris that are preferred by juvenile trout.


A third type of icing phenomenon is ice damming, which generally occurs in shallow riffle areas and upstream of natural and artificial constrictions in the river channel. In this phenomenon, the river’s flow is physically dammed by ice in the channel, forcing water over the top of existing ice cover, out of the channel and up onto the floodplain. Ice dams in the Henry’s Fork region frequently form to thickness of 10 feet or more and affect several miles of stream for weeks at a time, until warm weather breaks up the dam and sends large blocks of ice and associated debris downstream. During formation of these dams, large amounts of water is tied up in ice formation, causing river flow downstream to decrease until the dam reaches its maximum extent or breaks up.


Extensive ice dams form every winter on lower Fall River, sometimes filling the channel and floodplain from the Highway 20 Bridge upstream as much as 5 miles. Large ice dams also routinely form upstream from Ashton Reservoir and in the town of St. Anthony. An ice damming event upstream from Ashton Reservoir in the early 2000s physically uprooted dozens of mature cottonwood trees along North River Road (Fisherman’s Drive), washed out a portion of the road, and tore the remaining portion of the deck off of the old bridge at the Ashton Reservoir county boat dock. Another ice dam during that same time period flooded the Salem-Parker Highway and destroyed the bridge over the Henry’s Fork on that road. Obviously, trout habitat is minimal to non-existent in reaches affected by formation and break-up of these ice dams. Although localized mortality of trout is probably higher in these reaches during the period of damming, trout move in and out of these reaches according to habitat conditions and weather.


On a personal, non-scientific note, we should mention that Rob fishes as much during the winter as during the summer, frequently fishing the reaches of the Henry’s Fork and Fall River affected by ice dams. He routinely catches fish in these reaches within a few days after break-up of ice dams, often wading in the river at the bottom of ice canyons with vertical walls 6-10 feet high.


Photo caption: Winter fishing on Fall River. Note 3-5 foot thick remnants of ice dams on the bank.


Winter trout ecology in the Caldera Reach of the Henry’s Fork

The winter ecology of rainbow trout in the Henry’s Fork has been thoroughly studied; in fact, much of the broader scientific literature on winter trout ecology was generated by research here on the Henry’s Fork. Dr. Jack Griffith and his graduate students studied winter trout ecology on the Henry’s Fork in the 1980s and 1990s. Other researchers have continued to add to that substantial body of knowledge since then. Although initially focused on summer habitat use, our recent research on seasonal habitat availability in the Ranch has provided a large amount of data complementing the winter research to explain how rainbow trout in the Henry’s Fork navigate large seasonal changes in habitat available to them in the reach between Island Park Dam and Riverside Campground. We could write an entire book just on this subject; here we will just provide the main points in bullet form. If you would like to see the scientific papers, reports, or data substantiating these items, please let us know.

  • Rooted aquatic plants (macrophytes) provide the vast majority of physical habitat for trout between Last Chance and Pinehaven. Regardless of flow or weather conditions, this habitat is present only from early June through early November, with some variations in quality, quantity and duration depending on sunlight and nutrient availability during a given growing season.

  • Fish move into areas dominated by macrophytes in June and move out in November. Very few juvenile trout persist through the winter in the Ranch and Harriman East under any weather or flow conditions. The few adult trout that remain in this reach during the winter are concentrated in a few deep pools and in areas where springs keep water temperatures warm.

  • Macrophyte cover is the single largest determinant of water depth in the Ranch. As an example, the difference between 80 cfs of discharge from Island Park Reservoir and 400 cfs (a huge difference, from a winter-flow perspective) results in a mean increase in depth of only 2.7 inches in the Ranch, whereas the difference across seasons due to changes in macrophyte abundance alone can be as much as 9 inches.

  • Adult trout will persist in the transition reaches at Last Chance and Pinehaven later into the fall and return earlier in the spring than in Harriman proper, depending on local habitat conditions and insect hatches.

  • Once in winter locations, trout of all ages move very little between mid-November and the onset of spawning migrations in late February.

  • Mid-winter water temperatures in Box Canyon are much warmer than in other reaches of the river because of the influence of the spring-fed Buffalo River and thermal stratification in Island Park Reservoir. This latter situation occurs because water is delivered from the bottom of the reservoir, and water is most dense at 39 degrees Fahrenheit. This means that water coming out of the dam during the winter is 39 degrees, compared with 32 degrees for water coming into the reservoir.

  • The population of wild rainbow trout in the Caldera reach of the Henry’s Fork is limited by winter habitat for juvenile fish.

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