February 24, 2017 - 3:00 pm
February 24, 2017 - 4:00 pm
AddressNational Weather Center, 120 David L. Boren, Rm. 5600, Norman, OK 73072 View map
CategoriesConvective Meteorology (Mesoscale Dynamics)
SENSITIVITY OF ENSEMBLE FORECASTS OF SUPERCELLS TO INITIAL CONDITION UNCERTAINTY
The sensitivity of full-physics ensemble forecasts of supercells to initial condition (IC) uncertainty is investigated. The motivation for the study largely stems from the NOAA Warn-on-Forecast (WoF) program, where the primary objective is to develop a storm-scale ensemble prediction system that will generate probabilistic guidance for severe weather forecasts and warnings. The three sets of initial/boundary conditions for our simulations were generated from the real-time NSSL Experimental WoF System for Ensembles (NEWS-e) during the 2016 NOAA Hazardous Weather Testbed Spring Forecasting Experiment. In accordance with WoF, each ensemble was initialized with developing thunderstorms and integrated for 3 hours. Our primary goal was not to replicate observed supercell evolution, but rather to isolate the effect of IC uncertainty using a perfect- model assumption with a horizontal grid spacing that can resolve the storm’s mesocyclone reasonably well (1 km).
The forecast sensitivity to IC uncertainty is assessed by successively reducing the initial 3-km ensemble perturbations to 50%, 25%, and 10% of the original perturbations, which are downscaled to the 1-km grid. Forecast spread was substantially reduced with decreasing initial condition uncertainty. At the same time, however, spread growth accelerated, causing the spread curves to begin to converge toward the end of the 3-h forecast period and an intrinsic predictability limit would have been reached in the near future. The predictability of individual supercell features (e.g., updraft and low-level mesocyclone) was correlated; an indication that features organized on larger scales can enhance the predictability of smaller features.
Experiments were also run exploring the importance of uncertainty within vs. outside of the storm. Increased intra-storm certainty greatly reduced forecast spread early on while later in the simulations forecasts benefited more from increased environment certainty.