Hurricane Bonnie (1998) was particularly well observed during CAMEX-3. Figure 1 shows a juxtaposition of radar reflectivity (from EDOP), passive microwave brightness temperatures (from AMPR), and electric fields (from LIP). These are taken from a flight leg extending from near the center of the eye (at left) to the stratiform region (with embedded convective rainbands) on the southwest side (at right). Some relationships between these fields are apparent from the cross section. These relationships can be refined with the addition of other fields observed by the aircraft for this cross section along with consideration of the four dimensional nature of the storm.
In CAMEX-4, Hurricane Humberto seems especially suited for such investigation. Hurricane Erin is also a candidate. Observations from one or both of these storms, in addition to a more detailed look at Hurricane Bonnie, will be presented at the conference.
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