Extended Abstract (532K)J1.7
Observation-quality estimation and its application in NCAR/ATEC real-time FDDA and forecast (RTFDDA) system
Yubao Liu, NCAR/RAP, Boulder, CO; and F. Vandenberghe, S. Low-Nam, T. Warner, and S. Swerdlin
In last three years, NCAR/RAP and the Army ATEC Program have been developing a multi-scale (with grid sizes of 0.5 - 45 km) rapidly cycling real-time FDDA and forecasting system. By August, 2003, 12 such RTFDDA systems were customized and deployed to five Army test ranges and 7 other regions to support specific missions of three other US government agencies. A "station-nudging" approach, a Newtonian nudging method by which observations are incorporated into a continuously running MM5, is employed to accomplish forward four-dimensional data assimilation with full use of all observations available in real-time. Since the system could weight each observation according to its time and location, it allows the system to ingest both conventional and unconventional observations that are available observed at regular and irregular times. This flexibility allows us to incorporate the traditional hourly surface (METAR, ship, special) reports and upper air (twice-daily) rawinsondes. Also used are high-frequency measurements from various mesonets and special field experiments, wind profiler networks (NOAA/FSL NPN profilers and CAP-Cooperative Agency Profilers), NOAA/NESDIS hourly GOES winds derived from IR, visible and water-vapor images in experimental rapid-scan mode, the high-quality aircraft reports (ACARS/AMDAR) processed and disseminated by NOAA/FSL, and other non-conventional data sources.
The RTFDDA "station nudging" approach, in combination with diverse data sources having good coverage in time and space, can greatly alleviate the well-known problem in mesoscale data assimilation and NWP where observations are excessively sparse and the dynamics and cloud/precipitation "spin-ups" associated with "cold-starts" can severely affect the accuracy of the short-term (0 - 12 hour) forecasts. Nevertheless, data from different platforms have different instrument, sampling and processing errors and the error in the observations from one platform may vary in time and space. Furthermore, when these data are applied to a common data assimilation model grid, the representativeness error relative to the grid resolution can be a crucial factor affecting the analyses and forecasts. How to estimate and make use of the integral of these errors (referred as to total observation error) is a critical and challenging problem in data assimilation.
In conjunction with the "spin-up-free" FDDA analyses and forecasts, the high accuracy 0 - 3 hour model forecasts are available at all times, in real-time. These forecasts provide an ideal three-dimensional weather state that can be used to estimate the total observation error of each observation, without regard to the platform from which it was observed. In this paper, statistical comparison studies were conducted to confirm the accuracy of these 0 - 3 hour model forecasts. An advanced and efficient data quality control (QC) procedure is developed by making use the 0 - 3 hour forecasts and the error information of two reliable high-quality observation platforms (rawinsondes and METAR). The QC procedure not only defines appropriate error tolerance criteria to eliminates bad observations, but also calculate and assign a generalized quality flag to each observation. By scaling the quality flag between 1 (the best) to 0 (the worst), the QC flags of the observations are applied in the nudging process as a confidence weight that is unique to each observation. Numerical experiments were conducted, and the results show that the use of the observation error estimate leads to significant improvement in the RTFDDA analyses and short-term forecasts.
Joint Session 1, Data Assimilation and Observational Network Design. Part I (Joint between the Symposium on Forecasting the Weather and Climate of the Atmosphere and Ocean and the 20th Conference on Weather Analysis and Forecasting/16th Conference on Numerical Weather Prediction) (ROOM 6A)
Monday, 12 January 2004, 9:00 AM-12:15 PM, Room 6A
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