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Prediction of Frontogenetically Forced Precipitation Bands

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Frontogenesis (definition)<br />

F<br />

=<br />

D<br />

Dt<br />

∇pθ<br />

(S. Petterssen 1936)<br />

‣ The 2-D scalar frontogenesis function (F ) – quantifies the change in<br />

horizontal (potential) temperature gradient following air parcel motion :<br />

F > 0 frontogenesis, F < 0 frontolysis<br />

‣ Conceptually, the local change in horizontal temperature gradient near<br />

an existing front, baroclinic zone, or feature as it moves.

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