Prescribed by ANSI Std Z39-18 Performance Metrics: Population Structure, Life History Diversity, and Growth 8. Different genetic stock groups of Chinook salmon exhibit characteristic patterns of temporal and spatial distribution in the lower estuary. Genetic stock groups in the lower estuary were not uniformly distributed but exhibited distinct temporal and spatial patterns. Fall-run juveniles from the West Cascade and Spring Creek Group stocks (both from the Lower Columbia River Chinook Salmon ESU) dominated shallow habitats of the lower estuary. Whereas the Spring Creek Group fall stocks were widely distributed and abundant primarily during spring, proportions of the West Cascade fall stock generally increased with distance from the estuary mouth and were well represented from spring through fall. Representatives from the Upper Columbia River summer/fall stock group were distributed throughout the estuary, but few appeared in our samples until summer and fall. No consistent differences in stock composition were apparent at finer scales (i.e., habitat scales). To determine restoration priorities for at-risk salmon, further investigation is needed on stock-specific patterns of estuary habitat use, particularly in the poorly studied tidalfluvial reaches between rkm 100 and Bonneville Dam. 9. Most Chinook salmon Evolutionarily Significant Units (ESUs) are capable of expressing subyearling life histories. Both lower and upper Columbia River stock groups can produce subyearlings that reside in the estuary for several months. Subyearling Chinook salmon from all ESUs occupied shallow-water habitats of the lower estuary, except for spring run groups from the interior Columbia River basin. Otolith collections from Pt. Adams Beach indicated that subyearlings from a diverse subset of these ESUs expressed estuary-resident life histories. Back-calculations using otolith chemical analyses indicated that size at saltwater entry for lower Columbia River fall stocks (West Cascade and Spring Creek Group) averaged near 60 mm FL. Mean residence times in the saltwater portion of the estuary were estimated at between 1 and 2 months. Although the average back-calculated size at entry for Upper Columbia River summer/fall collections (n = 9) was much larger (88 mm FL), the estimated period of estuary residency averaged 2 months or more. Estimates from otolith analyses indicated positive growth rates for estuary-rearing salmon during all seasons, including maximum mean values of 0.55 mm day-1 during late summer (August). However, by this time, water temperatures in much of the estuary had increased to high levels, and salmon abundance had declined substantially. We have no measure of the daily rations or water temperatures that supported our growth rate estimates, which were back-calculated from otolith increment widths for individuals xiii captured near the river mouth (Pt. Adams Beach). Bioenergetic modeling may offer the best tool to investigate further the interactive effects of water temperature, salmon densities, and prey availabil...