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> Weather Prediction, Frontogenesis and Ensemble Forecasting

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Weather Prediction, Frontogenesis and Ensemble Forecasting

Since the 1950s numerical models atmospheric dynamics have allowed improved weather prediction. Since the 1960s numerical models of the coupled ocean-atmosphere system have been developed to predict climate changes of longer time scales. These models have nonlinear dynamics and have been shown to be sensitive to initial conditions. This sensitivity is not constant, however, but depends on the state of the model. It is described as state-dependent or flow-dependent predictability.

Since the early 1990s operational weather centres have used a technique called ensemble forecasting in an attempt to estimate the flow-dependent predictability of the atmosphere. More recently this type of ensemble approach has been introduced into climate modelling in an effort to establish the sensitivity of these models to parameters and initial conditions.

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This page last modified by A. Shabala
Tuesday, 01-May-2007 10:08:56 BST
Email corrections and comments to shabala@maths.ox.ac.uk