Data assimilation impact of in situ and remote sensing meteorological observations on wind power forecasts during the first Wind Forecast Improvement Project (WFIP). Issue 7 (26th March 2019)

• Record Type: Journal Article
• Authors: Wilczak, James M.; Olson, Joseph B.; Djalalova, Irina; Bianco, Laura; Berg, Larry K.; Shaw, William J.; Coulter, Richard L.; Eckman, Richard M.; Freedman, Jeff; Finley, Catherine; Cline, Joel
• Is Part Of: Wind energy. Volume 22:Issue 7(2019)
• Page Start: 932
• Page End: 944
• Publication Date: 2019-03-26
• Subjects: data assimilation -- forecasting -- observations -- wind power; Wind power -- Periodicals; 621.312136
• DOI: 10.1002/we.2332
• Languages: English
• ISSNs: 1095-4244

Abstract

Abstract: During the first Wind Forecast Improvement Project (WFIP), new meteorological observations were collected from a large suite of instruments, including wind velocities measured on networks of tall towers provided by wind industry partners, wind speeds measured by cup anemometers mounted on the nacelles of wind turbines, and wind profiles by networks of Doppler sodars and radar wind profilers. Previous data denial studies found a significant improvement of up to 6% root mean squared error (RMSE) reduction for short‐term wind power forecasts due to the assimilation of all of these observations into the National Oceanic and Atmospheric Administration (NOAA) Rapid Refresh (RAP) forecast model using a 3D variational data assimilation scheme. As a follow‐on study, we now investigate the impacts of assimilating into the RAP model either the additional remote sensing observations (sodars and radar wind profilers) alone or assimilating the industry‐provided in situ observations (tall towers and nacelle anemometers) alone, in addition to routinely available standard meteorological data sets. The more numerous tall tower/nacelle observations provide a relatively large improvement through the first 3 to 4 hours of the forecasts, which diminishes to a negligible impact by forecast hour 6. In comparison, the sparser vertical profiling sodars/radars provide an initially smaller impact that decays at a much slower rate, with a positive impact present through the first 12 hours of the forecast. Large positive assimilation impacts for both sets of instruments are found during daytime hours, while small or even negative impacts are found during nighttime hours.