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.
In the Oxford Environmental Mathematics Group we are investigating methods
for constructing and interpreting ensemble forecasts. We also study
experimental design and interpretation for climate modelling experiments.
Collaborators on these projects include the
European Centre for Medium Range Weather
Forecasting
and climateprediction.com.
People working in this area within OCIAM
are
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