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<br />III. <br /> <br />EXAMPLE <br /> <br />ENTRY <br /> <br />To assist the user in understanding the forecast and adjustment lists, an <br />interpretation of a sample entry is provided below. <br /> <br /># name of location <br />avg oct naV <br />adj(+###,-###) <br /> <br />5 BEAR - HARER <br />ADJ(+010,+029,+lS3) <br />AVG 21 19.7 16.6 15.4 17.1 <br /> <br />dec <br /> <br />jan <br /> <br />feb <br /> <br />mar <br /> <br />apr <br /> <br />USGS id <br />may jun <br /> <br />NWS id <br />jul aug <br /> <br />sep <br /> <br />Apr <br />-Jul <br /> <br />10044000 HARIl <br /> <br />33 <br /> <br />68 <br /> <br />99 97 4S 19.0 16.7 <br /> <br />309 <br /> <br />5 <br /> <br />number of the forecast point (points are sorted alphabetically) <br /> <br />BEAR - HARER <br /> <br />forecast point name (river'- site) <br /> <br />10044000 <br /> <br />US Geological Survey station number <br /> <br />HARIl <br /> <br />National Weather Service 5 character station identifier <br /> <br />ADJ(+010, .., <br /> <br />List of numbered adjustments used with this point (see list of adjustments <br />for cross reference) <br /> <br />Starting with the observed (regulated) flow for Harer, <br />the scheme for calculating the llnaturalll flow for Harer is as follows: <br /> <br />+010 indicates to add adjustment # 010 from the adjustment list, that is: <br />add 10 BEAR - WOODRUFF NARROWS RES, WOODRUFF, NR RES STORAGE <br /> <br />+029 indicates to add adjustment # 029 <br />add 29 CHAPMAN CAN - EVANSTON, NR, STATELINE, AT <br /> <br />STREAMFLOW <br /> <br />+lS3 indicates to add adjustment # 146 <br />add 146 SULPHUR CK - SULPHUR CK RES <br /> <br />RES STORAGE <br /> <br />In English, the observed flow of the Bear River at Harer, Idaho is regulated or <br />affected by the change in storage at Woodruff Narrows Reservoir, the diversion of flow by <br />Chapman Canal, and the change in storage at Sulphur Creek Reservoir. When reservoirs are <br />filling (storing water), the adjustment made on the downstream point is positive (i.e, the <br />flow at Harer would have been higher if not for the reservoir). Conversely, when reservoirs <br />are being tapped or drained for use, the adjustment on the downstream point is negative (i.e, <br />the flow at Harer would have been lower at this time of the year if not for the reservoir) . <br />Diversions may also be negative adjustments, as in cases where water is diverted into th~ <br />basin from an adjacent watershed. In this example with Harer, the diversion adjustment is <br />positive. <br /> <br />AVG <br /> <br />21 19.7 ..... <br /> <br />12 monthly volume averages plus april-july total. <br />Period of calculation is 1961-90. <br /> <br />21 <br />19.7 <br /> <br />October average <br />November average <br /> <br />16.7 <br />309 <br /> <br />September average <br />April-July total average (commonly, this is the forecast period). <br /> <br />5 <br />