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                    "recordDescription":"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\u2013WY 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.",
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                    "itemDescription":"This Technical Memorandum focuses on the development of daily open water evaporation rates and volumes from 13 lakes and reservoirs in the Klamath River Basin that have changed between predevelopment and current conditions. 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\u2013WY 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 largest source of uncertainty was the unknown fluctuations in pre-development water surface elevations as the uncertainty due to forcing data biases was greatly reduced through bias correction of the gridMET climate data. Results suggest that while evaporation rates were similar during WY 1981\u20132020 and pre-development conditions, annual mean pre-development evaporation volumes were 36 to 87 percent higher than current conditions volumes. Approximately 161 to 339 TAF more evaporation occurred annually under pre-development conditions than occurred from WY 1981\u20132020. This is primarily due to the drainage of pre-development large shallow lakes with high evaporation volumes. The modeling data associated with this report is available at https://data.usbr.gov/catalog/8500/item/133811. This work is part of a larger effort, the Klamath River Basin Revised Natural Flow Study. This study combines seven different hydrologic modeling tools to develop natural streamflow estimates for the Klamath River Basin from WY 1981 through WY 2020. The overarching purpose of the study is to apply current science, methods, and tools to develop natural streamflow estimates, while addressing known limitations of previous estimate and incorporating recommendations provided by the National Research Council.",
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                    "itemTitle":"Technical Memorandum No. ENV-2025-074: Upper Klamath River Basin Surface Water Hydraulic Modeling Report from the Klamath River Basin Revised Natural Flow Study",
                    "itemDescription":"This report documents the hydraulic analyses conducted in support of the broader Klamath Natural Flow Study. Components of the hydraulic analyses needed for the prediction of daily streamflow estimates include the surficial movement and storage of water across the landscape. Methods and results presented here include: (1) area-capacity relationships for Upper Klamath, Lower Klamath, and Tule Lakes, (2) rating curves (relationships between water surface elevation and discharge) at the downstream hydraulic control of Upper Klamath Lake under 1981\u20132020 and pre-development conditions, and (3) pre-development streamflow losses through the Lost River Slough and streamflow exchanges with Lower Klamath Lake. Results within this report are not actual daily predictions, but information to be used to calculate daily streamflow. Regarding water storage, surficial water area and storage have decreased greatly from pre-development to 1981\u20132020 conditions. The modeling of the hydraulic control at Upper Klamath Lake indicates that pre-development water surface elevations as compared to 1981\u20132020 conditions would be higher at low streamflow and lower at high streamflow. Finally, pre-development modeling between Link River and Keno, Oregon indicates that the Klamath River only diverted a portion of streamflow through the Lost River Slough to Tule Lake at flood discharges. The connection of the Klamath River with Lower Klamath Lake was dynamic and bi-directional, but streamflow exchanges were likely relatively small due to the self-regulating negative feedback preventing extreme streamflow exchanges in either direction. The results presented within this report were delivered to RiverWare as look-up tables to aid in the calculation of daily streamflow.",
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                    "itemTitle":"Upper Klamath River Basin Surface Water Hydraulic Modeling Data from the Klamath River Basin Revised Natural Flow Study",
                    "itemDescription":"The hydraulics component of the Klamath River Basin Revised Natural Flow Study focused on locations within the Klamath River Basin that are important to water storage and surficial exchange with other portions of the basin that may impact Klamath River streamflow. Key hydraulics components include area-capacity curves, lateral hydraulic connectivity, and engineered and natural hydraulic controls. These data detail the hydraulic modeling and topographic analyses that were used to inform the RiverWare mass balance modeling and natural streamflow estimates. Primarily those analyses include development of area-capacity (ACAP) relationships and hydraulic models that inform how water flows across certain locations of the landscape using rating curves and flow exchange relationships. Lakes and reservoirs where ACAP relationships were developed in Upper Klamath River Basin include Upper Klamath Lake, Lower Klamath Lake, and Tule Lake as well as inclusion of existing ACAP relationships at Rogue River basin reservoirs, PacifiCorp reservoirs, Gerber Reservoir, and Clear Lake. Reclamation developed hydraulic models at two main locations in the Upper Klamath River Basin: (1) from the downstream end of Upper Klamath Lake through the Link River; and (2) along the Klamath River reach between the Link River and Keno Dam. Predictions were developed using the Sedimentation and River Hydraulics \u2013 Two-Dimensional model. The Upper Klamath Lake products are rating curves that relate water surface elevation to a paired discharge flowing out of the lake for both 1981 to 2020 and pre-development conditions. The Link River to Keno pre-development modeling included results of flow exchange between the Klamath River and Lower Klamath Lake, as well as flow losses from the Klamath River to the Lost River Slough. This zip file contains hydraulic modeling data. To see the report associated with this dataset, please visit https://data.usbr.gov/catalog/8528/item/133876.",
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