An Axisymmetric View of Concentric Eyewall Evolution in Hurricane Rita (2005)
NAVAL POSTGRADUATE SCHOOL MONTEREY CA
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Multiplatform observations of Hurricane Rita 2005 were collected as part of the Hurricane Rainband and Intensity Change Experiment RAINEX field campaign during a concentric eyewall stage of the storms life cycle that occurred during 21-22 September. Satellite, aircraft, dropwindsonde, and Doppler radar data are used here to examine the symmetric evolution of the hurricane as it underwent eyewall replacement. During the approximately 1-day observation period, developing convection associated with the secondary eyewall became more symmetric and contracted inward. Latent heating in the emergent secondary eyewall led to the development of a distinct toroidal overturning circulation with inertially constrained radial inflow above the boundary layer and compensating subsidence in the moat region, properties that are consistent broadly with the balanced vortex response to an imposed ring of diabatic heating outside the primary eyewall. The primary eyewalls convection became more asymmetric during the observation period, but the primary eyewall was still the dominant swirling wind and vorticity structure throughout the period. The observed structure and evolution of Ritas secondary eyewall suggest that spinup of the tangential winds occurred both within and above the boundary layer, and that both balanced and unbalanced dynamical processes played an important role. Although Ritas core intensity decreased during the observation period the observations indicate a 125 increase in areal extent of hurricane-force winds and a 19 increase in integrated kinetic energy resulting from the eyewall replacement.