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model water balance errors, presence of wet and dry cells, comparison of historic <br />diversions, and locations of groundwater evapotranspiration. <br />Parameter weighting will be used to address measurement errors >IZ parameters used >IZ <br />calibration and to allow groundwater level and streaniflow data to be evaluated on a <br />sinular numeric basis even though they Have different measurement units and <br />mab zitudes. <br />Model calibration will be undertaken by varying aquifer hydraulic conductivity, <br />streambed conductance, recharge, well pumping, lateral boundary inflows and aquifer <br />specific yield. <br />Tl1e calibration process is expected to result in a model t11at can be used with confidence <br />to simulate historic and future groundwater inflows and outflows that are occurring <br />within the alluvial aquifer of the South Platte River basin. <br />6.0 Recommendations <br />The follow>lzg are recommendations from fl1e development of calibration targets and criteria: <br />• Continue current water level measurement programs, especially at wells that Have data <br />loggers and Have been surveyed. <br />• Use the targets and criteria presented in this TM for calibrating the alluvial groundwater <br />flow model in Phase 5. <br />P~ SPDSS T~8 2 Final TM 10-08-0t~.doc 19 <br />