Growth patterns of juvenile sockeye salmon in different thermal environments of Alaskan lakes

Abstract

Rearing conditions imposed on juvenile salmonids in lakes are important determinants of freshwater growth patterns. In Alaska, sockeye salmon (Oncorhynchus nerka) nursery lakes exhibit a wide range in thermal characteristics. Compared to clear lakes, stained lakes are warmer and have longer growing seasons, whereas glacial lakes are colder and have shorter growing seasons. In stained lakes, a shallow thermocline restricts most of the heat to the surface layers. Deep mixing in glacial lakes, concomitant with meltwater intrusion, keep much of the water column near 4 °C. Mean depth accounts for 77% of the among-lake variation in the seasonal average water temperature (TS). Length of growing season is dependent on latitude and altitude; however, water temperature is not. Taken together, the factors TS, zooplankton biomass, and sockeye fry density accounted for 70% of the variation in age-1 sockeye smolt size. This limnological information can be included in stock-recruit models of sockeye salmon to improve assessments for management.