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<br />002iL 4 <br /> <br />steady flow (20k cfs, for example) was not evaluated beyond the patterns associated with the <br />current operations since February 1997. <br /> <br />The process associated with the matrix and accompanying supporting citations involved <br />contacting researchers that had been directly involved with the 1996 BHBF (attachment a) as <br />well as researchers recommended by program managers. Because funds limited the ability to <br />bring researchers together for a workshop and the time of year also limited people's ability to <br />participate, we decided to compile researcher opinions via fax and mail. A mailing was sent out <br />in November 13, 1997 and researchers were asked to reply by December 3, 1997. <br /> <br />Comments from scientists were received and scores for the matrix were averaged and <br />provided to the TWO in their December 1997 meeting with a review provided by Barry Oold. <br />The scientists rated effects to resources in a range from -3 (negative) to +3 (positive). The TWO <br />recommended that that matrix be sent out again to the researchers for review and evaluation with <br />a revised matrix availablel:?Y.!.lI!1u~l~Ll ~~8 to TWO and AM\\:'O. It \V~_ c1iscusse.c!,thata <br />'-'meetingof the- scientistS providing information might be required to fully describe potential <br />effects on resources. <br /> <br />The matrix was sent out again prior to winter holidays with a request that evaluations be returned <br />by January 9, 1998. Revised scores and comments were incorporated into the matrix and <br />accompanying text. Included in the text were concerns voiced by researchers that pertain to <br />resources such as sediment, the aquatic food base, Kanab ambersnail, and vegetation. The <br />revised matrix, comments, notes and a summary of details were provided to the TWG in the <br />January meeting by Barbara Ralston. Barbara explained how the values for the resources were <br />obtained--via average scores and provided comments to the TWO member from the researchers <br />regaroing specific resources. Among the comments by the researchers was vagueness of the scale <br />associated with the matrix and a desire by the researchers to have an idea of what the anticipated <br />flow volumes following a high flow event might be. The TWO and OCMRC agreed that <br />researchers should be gathered to discuss the scale and to further develop the assumptions <br />associated with the matrix. <br /> <br />Researchers in areas that had negative impacts (-lor greater) associated with the resource were <br />requested to come to OCMRC to discuss the rating scale and to clarify the assumptions. Prior to <br />the meeting, the researchers were provided the previous matrices and text as well as a copy of the <br />hydrologic trigger document, "BHBF Triggering Criteria" developed by the TWO Spike Flow <br />Subgroup. Three groups of researchers were convened: sediment, aquatic biology, and terrestrial <br />biology. In these discussions, the following assumptions were developed for the resources. <br /> <br />Assumptions <br /> <br />. A high flow would occur in the event that hydrologic triggering criteria were met. <br /> <br />. A high flow would likely only be triggered in high water years so that flows <br />preceding and flows following a BHBF would be high (e.g., 20-25,000 cfs). <br /> <br />Directions to Developers of the Resource Matrix <br /> <br />. The primary intent of the BHBF is sediment conservation with no harm to other <br />resources. In effect, if sediment criteria are not met, then it is unlikely that a <br />