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<br />001735 <br /> <br />12 <br /> <br />passing the Grand Canyon gage, located 102 miles downstream of Glen Canyon Dam, exceeded total <br />estimated tributary inputs; except during the period of June through August 2000 (Low Summer <br />Steady Flow test), when dam operations were held constant at 8,000 cfs. Sand mass-balance data for <br />October 2000 through November 2001, do show evidence of some accumulation of sand upstream of <br />Phantom Ranch (river mile 87), in response to an approximate 1,000,000 metric ton input of sand <br />from the Paria River in October 2000, in combination with relatively low-flow releases from Glen <br />Canyon Dam throughout Water Year 2001. Additional sand inputs from the tributaries that occurred <br />during September of Water Year 2002, also accumulated in the channel bed under the low-flow <br />operations of September through December 2002. However, preliminary observations during <br />January through March 2003, suggest that experimental fluctuating flows exported 2002 sand inputs <br />from critical reaches above Phantom Ranch. Indeed, mass-balance calculations for Marble Canyon <br />and Upper Grand Canyon (Lees Ferry to Phantom Ranch) indicate that sediment export has exceeded <br />input since August 1999 (Figure 1.2). Further, Figure 1.2 indicates that significant export during the <br />winter experimental fluctuating flows is contributing to the negative mass-balance. Significant <br />tributary inputs during fall 2004, led to an experimental high-flow release from Glen Canyon Dam, as <br />discussed in a subsequent section updating experimental flows. <br /> <br />MASS-BALANCE SAND BUDGET <br />BElWEEN LEES FERRY AND THE GRAND CANYON GAGE <br /> <br /> 4.0 <br /> 3.0 <br />0;- <br />c: <br />00 2.0 <br />f-o <br />WE <br />>" <br />t=E <br />~g 1.0 <br /><>:= <br />IS <br />Uo> 0.0 <br />l1j81 <br /><>:~ <br />!f'!! -1.0 <br />(f)C) <br />(f)~ <br />..:..: <br />::Oz -2.0 <br />00 <br />zf- <br />;:j..: <br />I <br />f- -3.0 <br /> -4.0 <br /> <br />35,000 <br /> <br />- MASS-BALANCE UNCERTAINTY ENVELOPE <br />- WATER DISCHARGE 30,000 <br /> <br />25,000 <br /> <br />20,000 <br /> <br /> <br />15,000 <br /> <br />10,000 <br />5,000 <br />o <br /> <br />2000 <br /> <br />2001 <br /> <br />2002 <br /> <br />2003 <br /> <br />2004 <br /> <br />o <br />en <br />() <br />I <br />)> <br />;;0 <br />G) <br />m <br />)> <br />-l <br />-l <br />I <br />m <br />r <br />m <br />m <br />(f) <br />"T1 <br />m <br />;;0 <br />;;0 <br />-< <br />G) <br />~ <br />m <br />S <br />_w <br />.!!!- <br /> <br />Figure 1.2. Mass-balance of fine sediment between Lees Ferry and Grand Canyon since August 1999 <br />(data are provisional and subject to review and revision). <br /> <br />GCMRC FY2006 Annual Work Plan (Draft February 15,2005) <br />