Numerical Weather Prediction and Atmospheric Dynamics
Atmospheric numerical models are based on the physical/dynamical equations that govern the atmospheric flow, written as a computer code. The model initial conditions are obtained by combining short model forecasts with new observations (a process called data assimilation). When a model is integrated in time (i.e., the model codes are run) starting from the observed initial conditions, the output is a numerical weather forecast. Numerical forecasts provide the guidance to human forecasters and are the basis of all the National Weather Service and media weather forecasts. In the last two decades weather forecasts have become much more skillful and reliable. For example, today's 3-day forecasts are about as accurate as the one-day forecasts used to be twenty years ago. This is mostly due to the improvements that have taken place in these computerized weather forecasts, through the better use of the observations, and the use of more advanced models and of more powerful computers. Current developments in Numerical Weather Prediction include the use of very high resolution, non-hydrostatic models (mesoscale meteorology), new methods for discretizations of the dynamical equations, inclusion of more sophisticated physical processes, ensemble forecasting, coupled ocean-atmosphere-land forecasting to forecast El Nino, etc. Our Department is involved in several projects related to these advances. In addition, atmospheric models are used to understand better the nonlinear dynamics of the atmosphere and the internal structures and evolution of storms (e.g., hurricanes, squall lines, mesoscale convective complexes, and snow storms.
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