Difference between revisions of "The HFE Page"
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*Spring HFEs increase productivity of the [http://gcdamp.com/index.php?title=FOOD_BASE aquatic foodbase]. Fall HFEs do not appear to affect the long-term composition of the [http://gcdamp.com/index.php?title=FOOD_BASE aquatic foodbase] and may scour the foodbase prior to the winter non-growing season. | *Spring HFEs increase productivity of the [http://gcdamp.com/index.php?title=FOOD_BASE aquatic foodbase]. Fall HFEs do not appear to affect the long-term composition of the [http://gcdamp.com/index.php?title=FOOD_BASE aquatic foodbase] and may scour the foodbase prior to the winter non-growing season. | ||
*HFEs do not appear to directly affect [http://gcdamp.com/index.php?title=Humpback_Chub_Page humpback chub] or the [http://gcdamp.com/index.php?title=FISHERY rainbow trout fishery] but there may be indirect affects tied to foodbase and trout production. | *HFEs do not appear to directly affect [http://gcdamp.com/index.php?title=Humpback_Chub_Page humpback chub] or the [http://gcdamp.com/index.php?title=FISHERY rainbow trout fishery] but there may be indirect affects tied to foodbase and trout production. | ||
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*[[GCDAMP Rapid Response Learning Page| Rapid Response HFE Page]] | *[[GCDAMP Rapid Response Learning Page| Rapid Response HFE Page]] | ||
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|style="color:#000;"| | |style="color:#000;"| | ||
| + | *[[A 2026 Spring HFE]] was not conducted because the mixed support expressed by the PI Leadership Team | ||
| + | *[[A 2025 Fall HFE]] was not conducted because of the government shutdown | ||
*[[A 2025 Spring HFE]] was not conducted because of timing conflicts with the renovation of the -12 Mile Slough | *[[A 2025 Spring HFE]] was not conducted because of timing conflicts with the renovation of the -12 Mile Slough | ||
*[[A 2024 Fall HFE]] was "deferred" for possible implementation in the Spring of 2025 | *[[A 2024 Fall HFE]] was "deferred" for possible implementation in the Spring of 2025 | ||
*A 2023 Fall HFE was not conducted for lack of sediment | *A 2023 Fall HFE was not conducted for lack of sediment | ||
| − | *[[The 2023 Spring HFE| The 2023 Spring HFE]] | + | *[[The 2023 Spring HFE| The 2023 Spring HFE: 39,500 cfs for 72h]] |
*[[A 2022 Fall HFE| A 2022 Fall HFE]] was not conducted due to the discovery of [http://gcdamp.com/index.php/Smallmouth_Bass_Page smallmouth bass] in Glen Canyon (1,600,000 mt) | *[[A 2022 Fall HFE| A 2022 Fall HFE]] was not conducted due to the discovery of [http://gcdamp.com/index.php/Smallmouth_Bass_Page smallmouth bass] in Glen Canyon (1,600,000 mt) | ||
*[[A 2022 Spring HFE| A 2022 Spring HFE]] was not conducted for lack of sediment | *[[A 2022 Spring HFE| A 2022 Spring HFE]] was not conducted for lack of sediment | ||
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*[[The 2020 Spring HFE| A 2020 Spring HFE]] was not conducted for lack of sediment | *[[The 2020 Spring HFE| A 2020 Spring HFE]] was not conducted for lack of sediment | ||
*[[The 2019 Fall HFE| A 2019 Fall HFE]] was not conducted for lack of sediment | *[[The 2019 Fall HFE| A 2019 Fall HFE]] was not conducted for lack of sediment | ||
| − | *[[The 2018 Fall HFE]] | + | *[[The 2018 Fall HFE]]: 38,100 cfs for 60h |
*[[The 2017 Fall HFE| A 2017 Fall HFE]] was not conducted for lack of sediment | *[[The 2017 Fall HFE| A 2017 Fall HFE]] was not conducted for lack of sediment | ||
| − | + | *[http://gcdamp.com/index.php?title=GCDAMP-_HFE_2015 A 2015 Fall HFE] was canceled due to the discovery of [http://gcdamp.com/index.php?title=Green_Sunfish_Page green sunfish] in Glen Canyon (1,168,000 mt) | |
| − | *[http://gcdamp.com/index.php?title=GCDAMP-_HFE_2015 A 2015 Fall HFE] was canceled due to the discovery of [http://gcdamp.com/index.php?title=Green_Sunfish_Page green sunfish] in Glen Canyon | + | *[http://gcdamp.com/index.php?title=GCDAMP-_HFE_2014 The 2014 Fall HFE]: 37,500 cfs for 96h |
| − | *[http://gcdamp.com/index.php?title=GCDAMP-_HFE_2014 The 2014 Fall HFE] | + | *[http://gcdamp.com/index.php?title=GCDAMP-_HFE_2013 The 2013 Fall HFE]: 34,100 cfs for 96h |
| − | *[http://gcdamp.com/index.php?title=GCDAMP-_HFE_2013 The 2013 Fall HFE] | + | *[http://gcdamp.com/index.php?title=GCDAMP-_HFE_2012 The 2012 Fall HFE]: 42,300 cfs for 96h (slow downramp) |
| − | *[http://gcdamp.com/index.php?title=GCDAMP-_HFE_2012 The 2012 Fall HFE] (slow downramp) | + | |
*The 2011 Equalization flows | *The 2011 Equalization flows | ||
*[http://gcdamp.com/index.php?title=Near_Shore_Ecology_(NSE)_Study The 2009-11 Fall Steady Flow Experiment] | *[http://gcdamp.com/index.php?title=Near_Shore_Ecology_(NSE)_Study The 2009-11 Fall Steady Flow Experiment] | ||
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*[https://pubs.usgs.gov/fs/2011/3012/ The 2004 Fall HFE] | *[https://pubs.usgs.gov/fs/2011/3012/ The 2004 Fall HFE] | ||
*[[The 2000 Low Summer Steady Flow Experiment| The 2000 Low Steady Summer Flow Experiment (LSSF)]] | *[[The 2000 Low Summer Steady Flow Experiment| The 2000 Low Steady Summer Flow Experiment (LSSF)]] | ||
| − | *The 1997 | + | *[[The 1997 Habitat Maintenance Flow (HMF)]] |
| − | *[[The 1996 Spring HFE]] | + | *[[The 1996 Spring HFE| The 1996 Beach/Habitat-Building Flow (BHBF)]] |
*The 1990-91 Experimental Flows | *The 1990-91 Experimental Flows | ||
*[http://www.riversimulator.org/Resources/GCDAMP/GCDAMPchronicle/1983FloodGCDhannon.pdf The 1983-86 Floods] | *[http://www.riversimulator.org/Resources/GCDAMP/GCDAMPchronicle/1983FloodGCDhannon.pdf The 1983-86 Floods] | ||
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|style="color:#000;"| | |style="color:#000;"| | ||
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| + | '''2026''' | ||
| + | *[https://www.usbr.gov/uc/progact/amp/twg/2026-02-05-twg-meeting/uc-gcdamp-arm-riverbed-sandbarresponse-508-20260205.pdf Riverbed and Sandbar Response to Glen Canyon Dam Operations and High-Flow Experiments] | ||
| + | |||
| + | '''2025''' | ||
| + | *[https://www.usbr.gov/uc/progact/amp/amwg/2025-08-21-amwg-meeting/uc-gcdamp-amwg-ltempupdate-508-20250821.pdf LTEMP Experiments Update] | ||
| + | *[https://www.usbr.gov/uc/progact/amp/twg/2025-04-10-twg-meeting/uc-gcdamp-twg-ltempflowexperiments-508-20250410.pdf LTEMP Flow Experiments] | ||
'''2024''' | '''2024''' | ||
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'''2008''' | '''2008''' | ||
| − | *[[Media:2008 BHBF minority report.pdf| | + | *[[Media:2008 BHBF minority report.pdf| Grand Canyon Trust Minority Report - TWG motion regarding a 2008 experimental BHBF]] |
'''1997''' | '''1997''' | ||
Latest revision as of 17:24, 28 September 2026
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High-Flow Experimental (HFE) ReleasesPurpose and GoalThe purpose of HFEs is to determine if sandbar building during HFEs exceeds sandbar erosion during periods between HFEs, such that sandbar size can be increased or maintained over several years. LTEMP HFE ProtocolAs described in the LTEMP ROD, HFEs are experimental in nature and are designed to achieve a better understanding of whether, how, and when to incorporate high releases into future dam operations in a manner that maintains or improves beaches, sandbars, and associated habitat. The LTEMP HFE Protocol establishes a decision-making framework consisting of three components: (1) planning and budgeting, (2) modeling, and (3) decision and implementation. Under the LTEMP, HFE releases are restricted to limited periods of the year when the highest volumes of sediment are most likely available for building sandbars. Sediment-triggered HFEs may be made in spring (March to June) or fall (October to November; Figure 1). Fall extended-duration HFEs range from greater than 96 hr to 250 hr. Spring and fall HFEs that are not extended-duration range from less than 1 hr to 96 hr. Proactive HFEs may be implemented in spring or early summer (April, May or June), and have a duration range up to 24 hr. HFE magnitudes range from 31,500 cubic feet per second (cfs) to 45,000 cfs. The frequency of HFEs is determined by tributary sediment inputs, annual release volumes, resource conditions, and decisions of the Department. Extended-duration fall HFEs are limited to a frequency of 4 times total in the 20-year LTEMP period. HFE Sand Budget ModelThe LTEMP HFE Protocol uses predictive models to make recommendations for the magnitude and duration of potential HFEs using real-time measurements and models of sand inflow from the Paria River and forecasted hydrologic data to determine whether suitable sediment and hydrology conditions exist for a high-flow experimental release. A sand transport/budget model (Wright et al. 2010) is used to predict the mass of sand that would be transported by an HFE and to estimate if a proposed HFE would transport more or less sand than had been delivered from the Paria River to the Colorado River during the sediment accounting period (July 1 to June 30). Only HFE durations that result in a “positive sand balance” are considered. Output of the modeling runs provides the initial recommendation for the magnitude and duration of the HFE. However, because modeling only considers a simple range of possible HFE peak magnitudes and durations, the Protocol includes a review of the model output that may modify the recommended HFE to benefit relevant resources. (2018 HFE Tech Team Report) |
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