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Assessment of Salmonids and Their Habitat Conditions in the Walla Walla River Basin within Washington: 2000 Annual Report
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Assessment of Salmonids and Their Habitat Conditions in the Walla Walla River Basin within Washington: 2000 Annual Report
Glen Mendel, David Karl, and Terrence Coyle

Executive Summary

Concerns about the decline of native salmon and trout populations have increased among natural resource managers and the public in recent years. As a result, a multitude of initiatives have been implemented at the local, state, and federal government levels. These initiatives include management plans and actions intended to protect and restore salmonid fishes and their habitats.

In 1998 bull trout were listed under the Endangered Species Act (ESA), as “Threatened”, for the Walla Walla River and its tributaries. Steelhead were listed as “Threatened” in 1999 for the mid–Columbia River and its tributaries. These ESA listings emphasize the need for information about the threatened salmonid populations and their habitats.

The Washington Department of Fish and Wildlife (WDFW) is entrusted with “the preservation, protection, and perpetuation of fish and wildlife....[and to] maximize public recreational or commercial opportunities without impairing the supply of fish and wildlife (WAC 77.12.010).” In consideration of this mandate, the WDFW submitted a proposal in December 1997 to the Bonneville Power Administration (BPA) for a study to assess salmonid distribution, relative abundance, genetics, and the condition of their habitats in the Walla Walla River basin.

The primary purposes of this project are to collect baseline biological and habitat data, to identify major data gaps, and to draw conclusions whenever possible. The study reported herein details the findings of the 2000 field season (March to November, 2000).

Background

The Walla Walla River and its major tributaries, including the Touchet River, comprise a watershed of 1,758 square miles (ACOE 1997) and 2,454 major stream miles (Knutson et al. 1992). The majority of the watershed (73%) lies within Washington State, with the remainder in Oregon (Figure 1). The Walla Walla River originates from a fine network of deeply incised streams on the western slopes of the Blue Mountains. The Touchet River originates from similar streams on the northwestern slopes of the Blue Mountains, and also from seasonal streams draining Palouse hillsides to the north. The Walla Walla River drains into the Columbia River near Wallula Gap, about 21 miles above McNary Dam and 6 miles above the Oregon border. The Touchet River drains into the Walla Walla River just west of the town of Touchet, WA.

Historic and contemporary land–use practices have had a profound impact on the salmonid species abundance and distribution in the watershed. Fish habitat in area streams has been severely degraded by urban and agricultural development, grazing, tilling, logging, recreational activities, and flood control structures. Agricultural diversions have severely impacted stream flows in the Walla Walla River since the 1880s (Nielson 1950). Nearly all (99%) of the surface water diversions within Washington are for the purpose of irrigation (Pacific Groundwater Group 1995). The reduced stream flows created by irrigation withdrawals adversely impact salmonid survival within the basin. Additionally, many unscreened or partly screened diversions and fish passage barriers exist within the basin.

Out-of-basin impacts to local fish populations have been substantial. Salmon migrating to or from the ocean must pass through four dams and reservoirs on the Columbia River before reaching their destination. Juvenile and adult salmonid mortalities occur as they pass through each reservoir or dam. Other impacts include over-harvest, habitat destruction in the lower Columbia River and estuaries, predation, and industrial pollution. Historically the basin probably produced substantial runs of both spring chinook and summer steelhead. The last substantial run of wild chinook took place in 1925; thereafter chinook populations continued a precipitous decline, and the species is considered extirpated in the basin (Nielson 1950, ACOE 1997). Anecdotal accounts and reports of historic fisheries in adjacent basins, indicate that chum and coho could have occurred in substantial numbers in the Walla Walla Basin (Pirtle 1957), but little written documentation exists. Endemic steelhead persist throughout much of the basin, but the population is considered depressed (WDF and WDW 1993). Annually, approximately 200,000 non-endemic hatchery steelhead (Lyons Ferry stock) are released in the middle Touchet and lower Walla Walla rivers under the Lower Snake River Compensation Program (LSRCP) to provide harvest mitigation for the four lower Snake River dams.

Not all native salmonids in the basin are anadromous. Whitefish, bull trout and rainbow/redband trout exist within the basin. However, only rainbow/redband trout retain a wide distribution. In the past, bull trout are thought to have been widely distributed in the basin. Currently, bull trout distribution is generally limited to montane upper tributaries of the Touchet River, Walla Walla River, and Mill Creek (Mongillo 1993). However, bull trout are known to migrate into the middle or lower reaches of these rivers during the winter months. Many factors have led to the decline of bull trout in southeast Washington. Damaged riparian vegetation, increased sedimentation, and decreased water flows have resulted in elevated water temperatures beyond the tolerance of this cold water species (Mongillo,1993). Introduced rainbow trout or brown trout may have increased competition or predation for bull trout.

Several non-native fish species have been introduced to support recreational fishing, or they have strayed into the basin. The Washington Department of Game (now WDFW) began stocking brown trout (Salmo trutta) in the Touchet River in the July, 1965. Stocking was discontinued in 1999 due to concerns about competition, hybridization, and predation with native bull trout, steelhead, or rainbow/redband trout. Carp were introduced as early as 1884 (Walla Walla Daily Journal 1884). Channel catfish, smallmouth bass, and bluegill are some of the warm water fish that now occur in the lower basin. Additionally, in 1999, three-spine stickleback (Gasterosteus aculeatus) were found in the Walla Walla river by WDFW personnel involved with this project.


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