A41G-0144
Payette River Basin Project: Improving Operational Forecasting in Complex Terrain through Chemistry

Thursday, 17 December 2015
Poster Hall (Moscone South)
Melvin L Kunkel1, Derek Blestrud1, Shaun Parkinson1, Vincent Patrick Holbrook1, Shawn G Benner2 and James Fisher2, (1)Idaho Power Company, Boise, ID, United States, (2)Boise State University, Boise, ID, United States
Abstract:
Idaho Power Company (IPC) is an investor owned hydroelectric based utility, serving customers throughout southern Idaho and eastern Oregon. The University of Arizona (UA) runs an operational 1.8-km resolution Weather and Research Forecast (WRF) model for IPC, which is incorporated into IPC near and real-time forecasts for hydro, solar and wind generation, load servicing and a large-scale wintertime cloud seeding operation to increase winter snowpack. Winter snowpack is critical to IPC, as hydropower provides ~50% of the company’s generation needs. In efforts to improve IPC’s near-term forecasts and operational guidance to its cloud seeding program, IPC is working extensively with UA and the National Center for Atmospheric Research (NCAR) to improve WRF performance in the complex terrain of central Idaho. As part of this project, NCAR has developed a WRF based cloud seeding module (WRF CS) to deliver high-resolution, tailored forecasts to provide accurate guidance for IPC’s operations. Working with Boise State University (BSU), IPC is conducting a multiyear campaign to validate the WRF CS’s ability to account for and disperse the cloud seeding agent (AgI) within the boundary layer. This improved understanding of how WRF handles the AgI dispersion and fate will improve the understanding and ultimately the performance of WRF to forecast other parameters. As part of this campaign, IPC has developed an extensive ground based monitoring network including a Remote Area Snow Sampling Device (RASSD) that provides spatially and temporally discrete snow samples during active cloud seeding periods. To quantify AgI dispersion in the complex terrain, BSU conducts trace element analysis using LA-ICP-MS on the RASSD sampled snow to provide measurements (at the 10-12 level) of incorporated AgI, measurements are compare directly with WRF CS’s estimates of distributed AgI. Modeling and analysis results from previous year’s research and plans for coming seasons will be presented.