Extended Abstract (376K)P1.43
Impact of abridged atmospheric data in mesoscale modeling
Christopher L. Franks, South Dakota School of Mines and Technology, Rapid City, SD; and W. J. Capehart and M. R. Hjelmfelt
Incident meteorology requires detailed, time-sensitive forecasts to aid incident management and emergency response teams during episodic hazardous events. Numerical weather prediction (NWP) has become more economical over the years due to the availability of more powerful, low-cost computing. However, incident meteorological scenarios present short lead times for forecasts. In addition, operations at incident sites may have limited bandwidth to acquire data and limited computing resources.
We seek to compare “best practices” in initializing models against those scenarios applicable to incident meteorology. This study examines the impact of decreased data ingested into models so less information has to be transferred across the NWP system. A hierarchical series of simulations has been designed to test the sensitivity of forecasts as the amount of information used to initialize the model is gradually scaled back. The best practices simulations are designed to emulate what is typically done in research and operational settings. The simulations using abridged meteorological data are more representative of the type of information that would be available on site during incident scenarios.
Two 24-hr periods during the April 1999 Upper Missouri Basin Pilot Project (UMRBPP) are simulated to test the sensitivity of model forecasts as first guess (FG) fields and observations are scaled back. We confirm that forecasts are highly sensitive to the type of FG field used to initialize the model. The largest differences occur when changing from the best practices research setting to the operational setting. The differences between the best practices operational setting and the abridged scenarios show less disparity. Furthermore, altering the initial field by including or excluding observational soundings can create perturbations that linger within the modeling domain well into the simulation. These perturbations propagate through the model domain in the direction of the prevailing winds.
Poster Session 1, Monday Poster Viewing
Monday, 25 June 2007, 4:35 PM-6:30 PM, Summit C
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