In three HWRF-simulated tropical cyclones, rapid intensity changes are dominated by baroclinic energy conversion and eddy-eddy cross-scale transfers, not by barotropic mean-eddy exchanges.
A., 1972: Development of asymmetries in a three-dimensional numerical model of the tropical cyclone
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Characterizing the energetics of multi-scale asymmetries during tropical cyclone rapid intensity changes
In three HWRF-simulated tropical cyclones, rapid intensity changes are dominated by baroclinic energy conversion and eddy-eddy cross-scale transfers, not by barotropic mean-eddy exchanges.