Lake Roosevelt is a large reservoir (243 km long with 334.9 km 2 surface area) on the upper Columbia River. Grand Coulee Dam holds Lake Roosevelt and is operated for multiple uses including power production, flood control, irrigation, and recreation. There is a mitigation and sport fishery in Lake Roosevelt important to the region. Monitoring of the fishery and ecosystem within the reservoir were conducted in 1999 to assist in balancing the management of the reservoir for multiple uses.Precipitation accumulation was 107 % of normal in the basin above Grand Coulee Dam.This resulted in outflows at Grand Coulee Dam that were 23 % above the 15 year average (1983)(1984)(1985)(1986)(1987)(1988)(1989)(1990)(1991)(1992)(1993)(1994)(1995)(1996)(1997)(1998). The annual (1999) inflow, outflow, and water retention time in Lake Roosevelt were 130.7 kcfs, 127.4 kcfs and 32.1 days respectively. The higher river flows contributed to an annual mean total dissolved gas saturation of 110 %. Total dissolved gas surpassed the 110 % standard established by Washington state, 51 % of the year at the monitoring station near the U.S./Canadian border, and 37 % of the year at Grand Coulee Dam forebay.Most of the dissolved nitrogen in Lake Roosevelt was present in the NO 3 -form where the annual average was 0.119 mg/L across all locations. Phosphorus in Lake Roosevelt was relatively scarce with an annual average total phosphorus (TP) concentration of 0.006 mg/L across all locations. Annual average total nitrogen and TP ratios (36:1) reflect the limiting nature of phosphorus in Lake Roosevelt. Carlson's trophic state index places Lake Roosevelt in the meso-oligotrophic range (overall annual mean TSI=34).Mean phytoplankton chlorophyll a concentrations over the entire year were low at 1.9 mg/m 3 . Annual phytoplankton densities and biovolumes averaged 147 organisms/ml and 0.046 mm 3 /L respectively. Phytoplankton density and biovolume peaked in the summer.Phytoplankton average density and biovolume was significantly greater at Porcupine Bay than most other sampling locations.Inflow to Lake Roosevelt was positively correlated with phytoplankton density. This was in part, driven by increased nutrients available to phytoplankton for assimilation. Since phosphorus is limiting, increasing inflow brings particulates with adhering phosphorus that supply phytoplankton growth. Total phosphorus was negatively correlated with water 3 retention time, which also supports this assertion. Reduced inflow can lessen phosphorus available to phytoplankton reducing total primary production available to higher trophic levels alternately; holding the water in Lake Roosevelt can reduce entrainment of zooplankton and fish. Further, investigation is needed to balance the benefits of flow yet reduce the entrainment of sport fish.Littoral production is limited by changing reservoir elevation. Although limited by the hydraulics of the reservoir, the littoral zone has shown increased productivity. The trophic state index (TSI) that uses phytoplankton chlorophyll a, Secchi...