Hurricane Frances

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Hurricane Frances

description

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 - PowerPoint PPT Presentation

Transcript of Hurricane Frances

Page 1: Hurricane Frances

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 fromSimulation(Liu et al 1997)

Conceptual

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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

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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:

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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

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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)

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Principal Band: primary band of precipitation - typically extendingsoutheast 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