Catalog Record

Upper Klamath River Basin Open Water Evaporation Modeling Report and Data from the Klamath River Basin Revised Natural Flow Study

As part of the Klamath River Basin Revised Natural Flow Study, the Daily Lake Evaporation Model was used to simulate daily open water evaporation on water bodies throughout the Upper Klamath River Basin. Modeling methodology, results, and analysis are documented in a technical memorandum. Daily evaporation rates and volumes were estimated for all large waterbodies in the upper Klamath River Basin that have significantly changed between pre-development and water years (WY) 1981–WY 2020. A large effort was made to quantify the uncertainties related to the estimated evaporation rates and volumes which arose from biases in forcing data and unknown waterbody mean depths. The overarching purpose of the Klamath River Basin Revised Natural Flow Study is to apply current science, methods, and tools to develop natural streamflow estimates, while addressing known limitations of previous estimates and incorporating recommendations provided by the National Research Council. The natural streamflow estimates may be used for habitat suitability studies, drought planning, streamflow forecasting, water operations studies, and other water resource investigations. Furthermore, this study provides numerical modeling tools that can be used for future assessments.
Generation Effort Klamath River Basin Revised Natural Flow Study
Themes Water
Tags Modeling, Natural Flow Study, Open Water Evaporation, Pre-Development
Reclamation Project Klamath Project
Reclamation Program

Location Information

Location Name Klamath River Basin
Location Description The Klamath River flows northeast to southwest from its headwaters near Crater Lake in southern Oregon to its outflow at the Pacific Ocean in northern California. The Klamath River Basin is typically divided into two regions: The Upper Klamath River Basin and Lower Klamath River Basin. The Upper Klamath River Basin drains all catchments above the former Iron Gate Dam (lowest former dam on the Klamath River) in California. Located in the rain shadow on the eastern side of the Cascade Mountain Range, the Upper Klamath River Basin has an arid climate. The Upper Klamath River Basin features Oregon’s largest natural lake by surface area—Upper Klamath Lake—and relatively high urban and agricultural development. In contrast, the Lower Klamath River Basin, which is in the Pacific Coastal Range and encompasses the watershed downstream of former Iron Gate Dam, receives more precipitation than the Upper Klamath River Basin. The Lower Klamath River Basin encompasses large areas of northern California and Pacific Northwest conifers and hardwoods. The Lower Klamath River Basin has no major natural lakes and less urban and agricultural development than in the Upper Klamath River Basin.
Location Tags Klamath Basin
Location Parent
State(s) California, Oregon
Unified Region(s) California-Great Basin
Timezone
Elevation [ N/A ]
Vertical Datum [ N/A ]
Coordinates (lat, long) See Location Details
Horizontal Datum WGS84