Handout (2.3 MB)
Axisymmetric structure analysis revealed expanded tangential wind field, enhanced inflow, and clear maximum in reflectivity and vertical motion during the secondary eyewall formation. Results support the presence of a mesoscale descending inflow (MDI) in the upshear left quadrant of the storm during the ERC of Ivan, upwind of enhanced precipitation in the upshear half. In addition, the secondary tangential wind maxima were present in the upshear right quadrant, downwind of the upshear rainband. The more upshear positioning of the MDI relative to the shear direction in Ivan compared to previous literature suggests that more analyses of this feature should be conducted in more ERC events.
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