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                    "recordDescription":"Yellowtail Dam closed in 1966, changing the hydrologic, sediment, and temperature regimes for the Bighorn River in southeast Montana, allowing a cold-water trout fishery to thrive over the following decades. Reclamation conducted a series of studies to investigate the loss of habitat, geomorphic diversity, and river hydraulics in 35 kilometer reach of the Bighorn River immediately downstream from Yellowtail Dam, located near Fort Smith,  Montana. The most recent project, S&T project 19306, conducted more recent geomorphic mapping from 2011 and 2017 to compare with earlier mapping and related studies. We observed large losses in geomorphic diversity between 1939 and 1980.",
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                    "itemTitle":"S&T Project 19306 Final Report: Side channel evolution, geomorphic diversity, and sediment transport on the Bighorn River following larger dam releases between 2008 and 2018",
                    "itemDescription":"Yellowtail Dam closed in 1966, changing the hydrologic, sediment, and temperature regimes for the Bighorn River in southeast Montana, allowing a cold-water trout fishery to thrive over the following decades. However, fishermen recently reported a loss in habitat. We conducted a series of geomorphic and hydraulic studies to assess changes in the Bighorn River, including geomorphic mapping and hydraulic modeling. The first studies in 2008-2010 followed a period of drought marked by lower releases from the dam. In 2019, we reassessed the river following a wetter decade with prolonged high flow releases. Our overall findings are that: (1) the Bighorn River lost significant geomorphic diversity between 1939 and 1980; (2) the rate of loss in geomorphic diversity slowed between 1980 and 2019; and, (3) high flows did remove vegetation and aggraded sediment at some channel entrances, but not all. Through time, many side channels require increasingly higher flows to connect to the main channel or are disconnected. The entrance to one channel was manually excavated in 2012 and remains open and flowing; this type of adaptive management approach offers promise. While the river is unlikely to achieve the spatial extent of geomorphic diversity observed prior to the closure of Yellowtail Dam, it may be possible to restore and maintain many of the side channels that existed into the 1980s.",
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                    "itemTitle":"S&T Project 19306 Geospatial Data: Bighorn River Geomorphology",
                    "itemDescription":"We present in this geospatial data the work that was conducted of a series of geomorphic and hydraulic studies to assess changes in the Bighorn River, including geomorphic mapping, tracing the displacement of RFID-tagged gravels, and hydraulic modeling. The first studies in 2009-2010 followed a period of drought marked by lower releases from the dam; findings include: (1) the Bighorn River lost significant geomorphic diversity following dam closure, indicated by loss of active channel area, side channels, islands, and unvegetated bars; (2) the Bighorn River was not incising; (3) the frequency of moderate peak flows (&lt;10,000 cfs) likely aggraded side channel entrances; and (4) modeled flows of the maximum allowable release were unlikely to excavate aggraded material at side channel entrances. In 2019, we reassessed the river following a wetter decade with prolonged high flow releases. The high flows resulted in bank and mid-channel island erosion,\u00a0which provide the only source of gravel to the river.\u00a0The majority of gravel tracers seeded at the entrances to four side channels were found close to the seeding location, or completely flushed through the channel. One possibility is that it is more difficult to mobilize gravels at the crest of side channel entrances than it is to mobilize farther downstream. High flows did remove vegetation and aggraded sediment at many channel entrances, most often reopening overflow channels. However, many side\u00a0channels continued to become disconnected from the main channel- requiring higher flows on the Bighorn River to form a connection.\r\n",
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                    "itemTitle":"Bighorn River Side Channel Investigation: Geomorphic Analysis",
                    "itemDescription":"Geomorphic analysis of vertical and lateral historical changes on the Bighorn River from Yellowtail Dam to St. Xavier Bridge was conducted in order to investigate the loss of side channels in recent decades. Vertical changes were investigated by examining bed elevation changes at the USGS gage (station no. 06287000, Bighorn River near St. Xavier, MT) and by resurveying historical cross sections established during the Montana Fish, Wildlife and Parks (FWP) wetted perimeter study in 1997 (Frazer, 1997). Lateral changes were investigated through detailed geomorphic mapping on seven sets of historical aerial photography from 1939 to 2006.",
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                    "itemTitle":"Bighorn River, Montana Flushing Flows Analysis",
                    "itemDescription":"A special high-flow release from Yellowtail Dam on the Bighorn River is being considered to flush sand-size sediment from the gravel bed. Releases from Yellowtail Dam are typically in the 3,000 to 4,000 cfs range and, in the past, these flows have been sufficient to prevent sand from depositing on the gravels. However, flow releases in the past 3 to 4 years have been reduced to 1,200 to 1,500 cfs because of drought conditions and sand is thought to have accumulated in the channel. Fishery biologists and others have requested that Reclamation make a greater release to flush sand-size sediment from the gravel. The Sedimentation and River Hydraulics Group was asked to do an initial study to help determine the magnitude and duration of a special high-flow release that would be sufficient to flush sand from the gravel over a 13-mile reach of the Bighorn River downstream from Yellowtail Dam.\r\n\r\nThe study approach was to review the master\u2019s thesis by Wiley (1995) on flushing flows, perform the hydraulic modeling, determine sediment transport capacity and make future recommendations for flows and monitoring.",
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