Thus, on face value, our result supports the conclusion of the other studies that found that the upper-level trough was not important to the intensification of Opal. As we noted, however, in order to evaluate the contribution of the trough itself, the technique of piecewise potential vorticity (PV) inversion is required. Given a balance condition and an appropriate basic state, this technique allows the association of a given PV anomaly with a unique wind and height distribution. In the present study, as in our previous study, the asymmetric balance (AB) formulation is applied and the basic state is the symmetric hurricane vortex. The PV anomaly is selected so as to isolate, among other asymmetric features, the contribution of the upper-level trough to the balanced asymmetric winds and heights. These winds and heights are then used (again as in our previous study) to drive the secondary circulation in a symmetric (Eliassen) balance formulation, so that the contribution of the PV anomaly itself to the intensification of the model Opal vortex can be evaluated. Results from the GFDL forecast of Hurricane Opal as well as other cases will be shown as available.
Supplementary URL: