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Introduction to data assimilation in meteorology - ForOT Optical ...

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Assimilated <strong>in</strong>formation : background<br />

Problems :<br />

– Lack of observation <strong>in</strong> some part of the atmosphere.<br />

– Observation<br />

number<br />

smaller than the numerical state dimension (for AROME 10 4 VS 10 7 ‏.(‏ Need of an other<br />

<strong>in</strong>f<br />

ormation Background source : a previous x b forecast of the atmospheric state.<br />

Observations y o Analysis at t 0

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