cyclogenesis - University of Utah · 2019. 11. 21. · Cyclogenesis: The formation of a cyclone....

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1 Cyclogenesis Jim Steenburgh University of Utah [email protected] 801-581-8727 Suite 480/Office 488 INSCC Suggested reading: Lackmann (2011), Section 5.3 Motivation We need a dynamically based conceptual framework to understand and diagnose the development and decay of surface cyclones and anticyclones. Definitions Cyclogenesis: The formation of a cyclone. Cyclolysis: The decay of a cyclone. Relationship between pressure, height, and vorticity tendencies Conceptual frameworks for cyclogenesis are often based on vorticity rather than pressure. Pressure tendencies, height tendencies, and geostrophic vorticity tendencies are coupled through the geostrophic wind relationship so that: ! % & ! % ) * - . & * - . ) Thus, pressure, height, and geostrophic vorticity tendencies are intrinsically linked An increase in surface vorticity is associated with height and pressure falls A decrease in surface vorticity is associated with height and pressure rises

Transcript of cyclogenesis - University of Utah · 2019. 11. 21. · Cyclogenesis: The formation of a cyclone....

Page 1: cyclogenesis - University of Utah · 2019. 11. 21. · Cyclogenesis: The formation of a cyclone. Cyclolysis: The decay of a cyclone. Relationship between pressure, height, and vorticity

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Cyclogenesis

JimSteenburgh

UniversityofUtah

[email protected]

801-581-8727

Suite480/Office488INSCC

Suggestedreading:Lackmann(2011),Section5.3

Motivation

Weneedadynamicallybasedconceptualframeworktounderstandanddiagnose

thedevelopmentanddecayofsurfacecyclonesandanticyclones.

Definitions

Cyclogenesis:Theformationofacyclone.

Cyclolysis:Thedecayofacyclone.

Relationshipbetweenpressure,height,andvorticitytendencies

Conceptualframeworksforcyclogenesisareoftenbasedonvorticityratherthan

pressure.Pressuretendencies,heighttendencies,andgeostrophicvorticity

tendenciesarecoupledthroughthegeostrophicwindrelationshipsothat:

!𝜕𝑝𝜕𝑡%&

∝ !𝜕𝑍𝜕𝑡%)

∝ *−𝜕𝜁-𝜕𝑡 .

&∝ *−

𝜕𝜁-𝜕𝑡 .

)

Thus,pressure,height,andgeostrophicvorticitytendenciesareintrinsicallylinked

• Anincreaseinsurfacevorticityisassociatedwithheightandpressurefalls

• Adecreaseinsurfacevorticityisassociatedwithheightandpressurerises

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Vorticityperspective

Diagnosescyclogenesisusingthevorticityequation,whichignoringfriction,tilting,

andsolenoidaleffectscanbewritten

𝐷(𝜁 + 𝑓)𝐷𝑡 = −(𝜁 + 𝑓) !

𝜕𝑢𝜕𝑥 +

𝜕𝑣𝜕𝑦%

or,basedoncontinuity

𝐷(𝜁 + 𝑓)𝐷𝑡 = (𝜁 + 𝑓) !

𝜕𝑤𝜕𝑧 %

Thus,lowertroposphericstretching(i.e.,ascent)isamechanismforvorticity

generationandcyclogenesis.

TheexamplebelowfromLackmann(2011)showsanupper-leveltroughand

associatedareaofCVAandascentovertakingalow-levelfrontalzone.Thelow-level

frontalzoneischaracterizedbyhighinitialabsolutevorticity.Stretchingassociated

withtheupper-leveltroughmosteffectivelygeneratesvorticityalongthefront(due

totheabsolutevorticitymultiplierinthevorticityequation),leadingtocyclogenesis.

Pressureperspective

Assuminghydrostaticbalance,pressureissimplytheweightoftheoverlying

atmosphere.Surfacepressurechangesarethusduetointegratedmassdivergence

(orconvergence).Cyclogenesisoccurswhendivergencealoftexceedsconvergence

atlowlevels,resultinginnetmassdivergenceandsurfacepressurefalls.

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Ultimately,thevorticityandpressureperspectivesareconsistent

FigureadaptedfromLackmann(2011)coursenotes

QGperspective(omegaequation)

QGascentresultsinstretchingandpressurefalls.Ignoringfriction,thefollowing

cancontributetoascent,pressurefalls,andcyclogenesis:

• Vorticityadvectionbecomingmorecyclonic(orlessanticyclonic)withheight

o TypicallylookforCVA@500mb

• Alocalmaximumintemperatureadvection

o Typicallylookforwarmadvection,suchasalongawarmfrontor

occludedfront

• Alocalmaximumindiabaticheating

• Theseeffectsaremostpronouncedwhenthestaticstabilityislow

o e.g.,anupper-leveltroughcaninducecyclogenesismoreeasilyifthe

staticstabilityislowthanhigh

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Synopticexperience(cyclogenesis):

1. CVAdownstreamofanupper-leveltroughcontributestopressurefallsand

cyclogenesis

2. Warmadvectionalongawarmoroccludedfrontcontributestopressurefalls

andcyclogenesis

3. Diabaticheatingcontributestopressurefallsandcyclogenesis

4. Infrontalcyclonedevelopment,allthreeprocessescontributetoamutual

amplificationofthesurfacecycloneandupperlevelwave

5. Yougetmorebangforthebuckifthestaticstabilityislow

6. Stretchingdownstreamoftopographycanalsocontribute

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Idealizedexample(fromLackmann2011coursenotes)

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Synopticexperience(anticyclogenesis):

1. AVAdownstreamofanupper-levelridgecontributestopressurerisesand

anticylogenesis

2. Alocalminimumincoldadvectioncontributestopressurerisesand

anticyclogenesis

3. Diabaticcooling(e.g.,radiationalcooling)contributestopressurerisesand

anticyclogenesis

4. Compressionupstreamoftopographycanalsocontribute

Classactivity:

UsingtheIDVGlobal-10daydiagnostic,examineanddescribeacyclogenesis

andananticyclogenesiseventsfromaQGperspective.

PVperspective

Cyclogenesisresultsfromthecouplingandmutualamplificationofsurface

temperatureandupper-levelcyclonicPVanomalies,withcontributionsfrom

diabaticallygeneratedPVcyclonicanomalies.

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PVAnomalies(fromThorpe1985viaHoskinsetal.1985)

AsurfacewarmanomalyactslikeacyclonicPVanomalyandasurfacecoldanomaly

actslikeananticyclonicPVanomaly(fromThorpe1985viaHoskinsetal.1985)

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CyclogenesisfromaPVperspective:

1. Upper-levelcyclonicPVanomalyovertakesalow-levelfrontalzone

2. Cycloniccirculationassociatedwithupper-levelPVanomalyinducesawarm

tonguealongthefrontalzone

3. WarmtongueactslikeacyclonicPVanomaly,inducingacycloniccirculation

thatextendsupwardandfurtheramplifiestheupper-levelcyclonicPV

anomaly

4. Theupper-levelandsurfacethermalanomaliesbecomephaselockedand

mutuallyamplify,resultingincyclogenesis

5. DiabaticallygeneratedPVcanbeathirdbuildingblockinthisprocess

FigurefromHoskinsetal.(1985)

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Anotherperspective:

FigurefromLackmann(2011)lecturenotes

TypicalPVdistributioninanextratropicalcyclone

FigurefromLackman(2011)lecturenotes

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Example:1979President’sDayStorm

DynamicTropopausePotentialTemperature(fromLackmann2011lecturenotes)

SLPandSfcPotentialTemperature(fromLackmann2011lecturenotes)

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Diabaticlower-troposphericPV(fromLackmann2011lecturenotes)

Crosssection(greenlineinabove,fromLackmann2011lecturenotes)

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Classactivity:

UsingtheIDVGlobal-10daydiagnosticand/ortheweather.utah.eduGFSDT

andSurfacediagnosticforaselectedregion,examineanddescribeacyclogenesis

andananticyclogenesiseventsfromaQGperspective.