Extended Abstract (300K)7.8
Results from the Winter Storm Reconnaisance Program 2002-2003
Lacey D. Holland, NOAA/NWS/NCEP, Washington, DC; and Z. Toth, J. Moskaitis, S. Majumdar, C. H. Bishop, and R. Smith
It is well known that for numerical weather prediction forecasts, meso- and larger scale errors in the initial condition amplify rapidly. This generally leads to the degradation of forecast guidance with increasing forecast lead time. In the Winter Storm Reconnaissance (WSR) program, operationally implemented at the NWS in 2001, adaptive observations are taken over upstream areas sensitive to the development of critical winter weather events, selected in real time by operational forecasters. The Ensemble Transform Kalman Filter (ETKF) technique is used to estimate the effect of a specific set of additional observations on reducing forecast error within a preselected geographical region of interest by reducing errors in the initial conditions.
During the WSR 2002-2003 programs (22 Jan - 20 March; 19 Jan - 15 March), GPS dropsondes were adaptively released by the NOAA G-IV and the USAF C-130 planes along one of 56 preselected flight tracks, promising the largest forecast error reduction. All dropsonde data were assimilated operationally in the ETA and Global Forecast System (GFS; formerly MRF and AVN systems) at NCEP.
The impact of the adaptive observations is evaluated by running a parallel analysis/forecast cycle of the GFS system. Forecast fields initialized from analyses including and excluding the dropsonde data are verified. A comparison of verification results for the parallel cycles reveals the impact of the adaptive observations on surface pressure, temperature, humidity, and quantitative precipitation forecasts. Results averaged over all cases will also be presented to show the impact of the adaptive observations on the prediction of winter storms.
Session 7, Field Experiments (Room 618)
Thursday, 15 January 2004, 8:30 AM-11:31 AM, Room 618
Previous paper
Recorded presentation