Figure 16. (A) Total rate of replacement in Goose Bay and Tulana in Upper Klamath Lake, Oregon, (B) partial replacement rate of water in Goose Bay and Tulana with Williamson River water, and (C) theoretical replacement time of the water in Goose Bay and Tulana, as a function of lake elevation, as calculated with multi-variate regression models. To obtain results shown, wind conditions were set to strong northwesterly winds as observed on May 22, 2008, and the Williamson River inflow was set to 60 cubic meters per second. Elevations are in feet above Bureau of Reclamation datum.


First posted March 29, 2012