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Published byIsabel Haynes Modified over 9 years ago
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Hurricane Frances
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MODIS view of Hurricane Frances (Note that eye is present but clouds at base of eye make it look cloudy throughout)
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FRANCES TRACK
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Hurricane frequency Frances
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Hurricane Structure Major Components –Eye –Eyewall(s) –Rainbands (primary, secondary, outer) Regions –Core region –Outer region Other Components (not always present) –Eyewall mesovortices and swirls –Fine-scale rainbands
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From Willoughby (1988) Structure of a hurricane: View from the top
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Structure of a Hurricane in cross section
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Theta-e from Simulation (Liu et al 1997) Conceptual
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Light-shading: cloud and precipitation Dark regions: convective eyewall and spiral rainbands EIL: : Eye inversion layer (slash- hatched areas) OEA: occluded eye air with low e (cross-hatched regions) MTD: moist downdrafts between the convective bands SR: Spiral rainband updrafts RO: Return outflow SU: Sloping updraft of eyewall MI: Main inflow MO: Main outflow RI: Return inflow DF: Divergent flow VC: Forced vertical circulation LX: Lateral mixing GO: Gravity wave oscillations MD: Mean decent in eye Dashed line: Freezing level Schematic (radial–height) conceptual model of a mature hurricane in the inner-core region
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Types of eyewall structure observed in hurricanes with radar Symmetric single ring eyewall
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The double eyewall of Hurricane Gilbert (1988) (most intense Category 5 storm in western hemisphere)
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Asymmetric eyewall of Hurricane Georges
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From Willoughby et al. (1984) Inner Core Region: PGF balances Centrifugal acceleration Inside eye, Rankine vortex Approx. ( v(r) = V o R/r ). Outside gradient wind approx. is valid: (v 2 /r + fv –fv g = 0) Parcels orbit eye inside core region
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From Willoughby et al. (1984) Outside Core Region: Coriolis force Important Air passes around hurricane without orbiting Convergent airflow along the right flank relative to direction of motion (motion here to top of page)
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Principal Band: primary band of precipitation - typically extending southeast from eyewall toward perimeter of hurricane
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Connecting Band: Sometimes connects Eyewall to Principal Band
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Compare the conceptual model to Hurricane Frances
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Inner core of Frances Principal band
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Radial velocity from Hurricane FrancesConceptual diagram The inner core winds of Hurricane Frances
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Eyewall Mesovortices Wright and Bennett (1997) Bertha 1996 Isabel 2003
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No suggestion of vortices in eye of Frances from satellite
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Eye vortex
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Gall et al. (1998) Hurricanes also contain many fine scale bands Hurricane Andrew (1992)
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Hurricanes also contain many fine scale bands Hurricane Hugo (1989) Gall et al. (1998)
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Note the fine scale bands in Andrew
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Fine scale bands in Frances
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