Hurricane Frances
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Transcript of Hurricane Frances
Hurricane Frances
MODIS view of Hurricane Frances(Note that eye is present but clouds at base of eye make it look cloudy throughout)
FRANCES TRACK
Hurricane frequency
Frances
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
From Willoughby (1988)
Structure of a hurricane: View from the top
Structure of a Hurricane in cross section
Theta-e fromSimulation(Liu et al 1997)
Conceptual
Light-shading: cloud and precipitationDark regions: convective eyewall and spiral rainbandsEIL: : Eye inversion layer (slash- hatched areas)OEA: occluded eye air with low e
(cross-hatched regions)MTD: moist downdrafts between the convective bandsSR: Spiral rainband updraftsRO: Return outflowSU: Sloping updraft of eyewallMI: Main inflowMO: Main outflowRI: Return inflowDF: Divergent flowVC: Forced vertical circulationLX: Lateral mixingGO: Gravity wave oscillationsMD: Mean decent in eyeDashed line: Freezing level
Schematic (radial–height) conceptual model of a mature hurricane in the inner-core region
Types of eyewall structure observed in hurricanes with radar
Symmetric single ring eyewall
The double eyewall of Hurricane Gilbert (1988)(most intense Category 5 storm in western hemisphere)
Asymmetric eyewall of Hurricane Georges
From Willoughby et al. (1984)
Inner Core Region:
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onacceleratiCoriolis
onacceleratilcentrifuga
fv
rv
fr
v
1/2
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onacceleratilcentrifuga
fv
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vRo
PGF balancesCentrifugal acceleration
Inside eye, Rankine vortexApprox. (v(r) = VoR/r).
Outside gradient wind approx. is valid: (v2/r + fv –fvg = 0)
Parcels orbit eye inside core region
From Willoughby et al. (1984)
Outside Core Region:
Coriolis force Important
Air passes around hurricane without orbiting
Convergent airflow alongthe right flank relativeto direction of motion(motion here to top ofpage)
1~/2
onacceleratiCoriolis
onacceleratilcentrifuga
fv
rv
fr
vRo
Principal Band: primary band of precipitation - typically extendingsoutheast from eyewall toward perimeter of hurricane
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fv
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fr
v
1/ 2
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Connecting Band: Sometimes connects Eyewall to Principal Band
Compare the conceptual model to Hurricane Frances
Inner core of Frances
Principal band
Radial velocity from Hurricane FrancesConceptual diagram
The inner core winds of Hurricane Frances
Eyewall Mesovortices
Wright and Bennett (1997)
Bertha 1996
Isabel 2003
No suggestion of vortices in eye of Frances from satellite
Eye vortex
Gall et al. (1998)
Hurricanes also contain many fine scale bands
Hurricane Andrew (1992)
Hurricanes also contain many fine scale bands
Hurricane Hugo (1989)Gall et al. (1998)
Note the fine scale bands in Andrew
Fine scale bands in Frances