Atmospheric Physics
4D-Var, or four-dimensional variational data assimilation, is a mathematical technique used to improve the accuracy of numerical weather predictions by combining model data and observations over a specific time window. This method optimizes the initial conditions of a forecast model by minimizing the difference between the model outputs and real-world observations, effectively integrating both spatial and temporal information. By doing this, it enhances the model's ability to accurately represent atmospheric phenomena.
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