Abstract
We show that the development can be forecast successfully with the current Australian limited-area prediction model, but that high resolution is needed to capture fully the intensity, structure and track of the system. We show also that both large- and small-scale processes contribute to the development of the east-coast cyclone. Large-scale moist baroclinic processes provide the favorable environment and initial development of a weak, synoptic-scale cyclone. Subsequent development of the intense, mesoscale system requires convective release of latent heat, local orographic forcing, and high resolution surface energy fluxes. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 3037-3053 |
| Number of pages | 17 |
| Journal | Monthly Weather Review |
| Volume | 115 |
| Issue number | 12 |
| DOIs | |
| State | Published - 1987 |
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