Chauris I Karoui P Garreau H Wackernagel P Craneguy L Bertino Centre de Ge osciences Mines ParisTech 35 rue SaintHonore 77300 Fontainebleau France UMRSisyphe 7619 UPMC Paris France Ifremer Plouzane France Actimar Brest France Nersc Bergen Nor ID: 67096
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Thecirclettransform:ArobusttoolfordetectingfeatureswithcircularshapesH.Chauris,I.Karoui,P.Garreau,H.Wackernagel,P.Craneguy,L.BertinoCentredeGe Correspondingauthorat:CentredeGeosciences,MinesParisTech,35rue,77300Fontainebleau,France.E-mailaddress:herve.chauris@mines-paristech.fr(H.Chauris). Computers&Geosciences37(2011)331 342 extensionofwaveletswheretheelementsusedforthedecom-positionareelongatedalongoneaxisandoscillatingintheperpendiculardirection.WerefertoMaandPlonka(2010)forareviewoncurveletapplications.Boththewaveletandcurveletanalysisdonotrevealtheopticdisk.Theproposedherehasbeendesignedtodetectobjectswithcircularshapes.Asforwaveletsandcurvelets,itpreservesthemulti-scaleaspect.However,italsohasthepossibilitytofollowglobalstructuresasfortheHT.Theobjectiveofthenewtransformfordetectingcircularshapesshouldaddressthefollowingissues:(1)theusershouldbeabletospecifyarangeofradiifortheselection;(2)thesegmentationpartshouldbeavoidedformorerobustness;(3)thecircularshapeshouldbeanannulusofacertainwidthinordertohandlenon-perfectlycircularshapes.Thisisalsoawaytotakeintoaccounttheband-limitedaspectofthedata;(4)thetransformshouldbeperfectlyinvertible:ifallcoefcientsareselected,thentheinvertedimageshouldbethesameastheoriginalimage;(5)thetransformshouldbefastenoughtoenableiterativeprocessessuchasthesoft-thresholdingtechniqueforreducingthenumberofkeyelementsneededtorepresentthecircularstructuresintheimage(Donoho,1995Theoutlineofthepaperisthefollowing.Werstdescribetransform.Wethenpresentthealgorithmusedtoselectonlyafewrepresentativecoefcients.Weshowapplicationsinthreedifferentelds:ophthalmology,moonexplorationandcoastaloceanography,onmainlyrealimages.Theapplicationsrangefromthedetectionofasingleandclearcircularshapetothendingofaseriesofcircularshapeswithmorediffusecontours.Finally,wediscussthecurrentlimitationsofthemethodandwhatcouldbeimproved,inparticulartoremovesomespuriousdetections.2.TheIntheproposedapproach,thereisnoneedforbinaryimagesegmentation.Themethodconsistsofdecomposinganyimageintocircleswithdifferentradiiandacertainwidth,viaaseriesoffastFouriertransforms(FFTs).Thesecirclesarecalledtheycanbeseenastheconvolutionofacirclewitha1Doscillatoryfunction,possiblyawavelet,inthesamewayasrelatetowaves.However,thestrategyforcomputingthecoefcientsisratherdifferentfromtheclassicalapproachusedforwaveletdecomposition.Usually,waveletcoefcientsareobtainedviaaseriesofcascadedconvolutionsanddown-sampling(Daubechies,1992).Asexplainedbelow,thedecompositionisformulatedintheFourierdomainwiththedenitionofspeciclters,followingasimilarapproachastheoneproposedbyCandesetal.(2005)forcurvelets. Fig.1.Retinographyimage(left)andassociatedimagegradientmaps(right),with(A)opticdisk,(B)retinalbloodvessels,and(C)exudates.Localgradientvaluesarehigheraround(B)and(C).Onlytheopticdiskhasacircularshape. 400 600 800 1400 400 600 800 400 600 800 1400 400 600 800 Fig.2.ReconstructedimageafterMeyerwavelet(left)andcurvelet(right)transforms.Ineachcase,onlycoefcientswithvalueshigherthan40%ofthemaximumvalueareselected.Othercoefcientsaresettozero.H.Chaurisetal./Computers&Geosciences37(2011)331 342 2.1.Generalframeworkelementsarecharacterizedbyacentralposition),aradiusandacentralfrequencycontentFig.3).Thisnitefrequencyprovidesacertainwidthtotheinthespatialdomain.ThisisthemaindifferencewiththeHoughtransform,beyondtheimplementationaspects.AllcanbededucedfromareferencecircletceitherbyashiftorbymodifyingtheradiusorthecentralfrequencycontentoftheFig.4,Eq.(1)).Theparametersfullycharacterizeeach.Formally,thefunctioncanbewrittenasistypicallyanoscillatoryfunc-tion,possiblyawaveletfunction,designedtodetectdisconti-nuities(Daubechies,1992).Fromapracticalpointofview,beexplicitlydenedinthe2DFourierdomain.2.2.ThecircletdecompositionTheforwardandinversetransformissimilarinessencetothecurvelettransform(CandesandDonoho,2004;Candesetal., y coordinate 50 100 150 200 250 300 50 100 150 200 250 300 x coordinatey coordinate 50 150 200 250 300 150 200 250 300 Fig.3.Representationofasingle(left)andits2DFouriertransform(right).Byconstruction,itiswell-localizedintheFourierdomain. x coordinate 100 200 300 50 100 150 200 250 300 x coordinatey coordinate 100 200 300 50 100 150 200 250 300 x coordinatey coordinate 100 200 300 50 100 150 200 250 300 Fig.4.Representationofthereference(left)andothercorrespondingtoadifferentradius(middle)andtoadifferentfrequencycontent(right).Artifactsvisibleontheimageinthemiddleareduetoanabrupttruncationintheshapeoflters(Fig.5 3210123 Frequency (rad)Amplitude Fig.5.Representationofasinglelter2determiningthefrequencycontentoftheH.Chaurisetal./Computers&Geosciences37(2011)331 342 ).Theobjectiveistodecomposeany2Dimage)intoasumofbasicfunctionsForcurvelets,thebasicelementshaveelongatedshapes,similartotherepresentationoflocalplanewaves(Candesetal.,).For,thebasicfunctionsarecircular.Theconstructionusesthepropertiesofatightframe,sothattheassociatedamplitudesareobtainedbyascalarproductFromapracticalpointofview,thecoefcientsaredenedintheFourierdomain,usingParsevalstheorem y coordinate 100 200 300 50 100 150 200 250 300 x coordinatey coordinate 100 200 300 50 100 150 200 250 300 x coordinatey coordinate 100 200 300 50 100 150 200 250 300 Fig.6.Simpleinputimage(left),imagereconstructedafterselectionofallcoefcientscorrespondingtoasingle2value,andradiusvaluesin[10,55]pixels(middle),andimageafterselectionof0.01%ofcoefcientswiththehighestamplitudes. 200400600800100012001400 200400600800100012001400 200400600800100012001400 200400600800100012001400 Fig.7.Imagesofeyefundus.Fordetection,radiusrangevariesfrom30to80pixels.H.Chaurisetal./Computers&Geosciences37(2011)331 342 denotesthe2DFouriertransformoftheconjugate.Withthisformulation,thetransformisconstructedinthe2DFourierdomain.Thekeystepconsistsofdening,theFouriertransformof.Thisisobtainedbydevelopingappropriatelterstoensurethatthebasicfunctionshavecircularshapes.2.3.DenitionofltersThelterconstructionisobtainedinatwo-stepprocess:rstwederive1Dltersandthen2Dlters.Bothltersaredenedinthefrequencydomainandformapartitionofit:for,wehaveThisconditionisimportanttoensureaperfectreconstructionscheme(Candesetal.,2005).Firstdeneisthenumberoflters.For,otherwise0.Notethattheltersaresymmetric(Fig.5).Onecaneasilycheckthattheltersformapartitionofthe1Dfrequencydomain.Theltersaredenedfromtheltersbyintroducingaphasedelayinordertocreateacircularshapeinthespacedomain,.Oncetheltersdened,Eq.(8)providesanexplicitformulationfortheFouriertransformofa)isthecentralpositionandwheretheradiusofthe.Bydenition,denotesthescalarproduct.Wethushave.TheindexcontrolsthefrequencycontentoftheFig.4).WithEqs.(5)and(7),itisalsoeasytoseethatforanygivenvalues,theltersalsoformapartitionofthe2Dfrequencydomain.Byusingpolarcoordinates,weshowinAppendixAthatthe2DinverseFouriertransformofiscircular,meaningthatthebasisfunctionshavecircularshapes.2.4.PracticalimplementationTheforwardtransformconsistsof(1)a2DFouriertransformoftheoriginalimage)toobtain;(2)forallltersandforallselectedvalues,amultiplicationof;(3)theinverseFouriertransformoftheproductthatprovidesallthecoefcientsrelatedtoscaleandradius 200400600800100012001400 200400600800100012001400 200400600800100012001400 200400600800100012001400 Fig.8.Imagesofaneyefundus(top)andassociatedgradientmaps(bottom).Bloodvesselsandexudates(seeFig.1)havelargegradients.Forthedetection,radiusrangevariesfrom30to80pixels.H.Chaurisetal./Computers&Geosciences37(2011)331 342 Theinversetransformfollowsthesamerule.Firstapplya2DFouriertransformforallscalesandselectedradii,multiplybytheconjugateofandsumallresults.Thenalimageisobtainedbyapplyinga2DinverseFouriertransform.Becauseoftheconditionon(Eq.(6)),wehaveaperfectreconstructionschemeifallcircletcoefcientsarepreserved.Formoredetailsontheforwardandinversetransforms,werefertothecurvelettransform(Candesetal.,).Themaindifferencewiththecircletconstructionisthechoiceofthelters.Fromapracticalpointofview,weratherselectasinglescale(i.e.singlelter)andaseriesofradii,withexpectedvaluesfrommin0totopotentiallyemphasizecircularformswithsomespecicspatialsizes.3.ApplicationsWerstindicatehowtochoosethekeycoefcientsandthenpresentapplicationstodifferentelds. 300 400 100 200 300 300 400 100 200 300 Fig.10.Zoomfromthepreviousgure,whereonlyconsideredasartifactsarerepresented,superimposedontheimage(left)anditsgradient(right).Thesearetangenttoarclinesduetothecombinationofthesunshadowandthetopography. 200 300 400 500 100 200 300 400 500 200 300 400 500 100 200 300 400 500 Fig.9.Satelliteimagefromthemoon(left),withtherst13selected(right).Radiusrangevariesfrom25to60pixels.H.Chaurisetal./Computers&Geosciences37(2011)331 342 3.1.SelectionofrepresentativecircletsFig.6illustratesaverysimpleexample.Theinputimageconsistsofrectangularandcircularshapes.Thecoefcientswiththehighestabsoluteamplitudesareassociatedwithcircularshapes.Theselectionofthesecoefcientsleadstoanimagefreedfromtherectangles.Inthecircletdomain,thecoordinatesofthecoefcientsdirectlyindicatethecentersofcirclesandtheirassociatedradii.Formorecomplicatedcaseswherethecontoursarediffuse,weapplythefollowingstrategy.Asapre-processingstep,performaspatialgradient(discreteLaplacianoperator)totheoriginalimageinordertoemphasizethediscontinuitiesinthedata.Inthecaseofsatelliteimages,theyclassicallysufferfrommissinginforma-tionduetothepresenceofclouds.Wetheninterpolatethedatabyageostatisticallteringmethod(kriging)thatprovidesresultsspatiallyconsistentwiththeoriginaldata(Wackernagel,2003Forthedetectionofasinglecircularstructure,wesimplyselectthehighestcoefcient.Formorecircles,weusedthesoft-thresholdingapproachinaniterativeprocess(Donoho,1995First,weselectthehighestcoefcient.Thetransformisredundant,meaningthatthenumberofcoefcientsislargerthanthesizeoftheinputdata.Thenextcoefcientswithhighvalueshaveapproximatelythesameradiusandcentralpositions.Forthatreason,wesettozeroallcoefcientsassociatedtothesameradiusandspatiallyclosetotheselectedcoefcient.Byclose,wemeanadistancelowerthanhalfoftheradius.Itdoesnotpreventfromselectingacoefcientwithadifferentradiusaroundthesamecentralposition.Wethenrecompose/decomposetheimagetoobtainnewcoefcients.Theoperationisrepeateduntilthenumberofkeycoefcientsspeciedbytheuserisreached.Thecombinationofreconstructionanddecompositionisnotnecessa-rilyneeded.Itisusedherebecausethetransformisredundant, 100 150 200 50 100 150 150 100 150 Fig.12.SyntheticSSTmap.Radiusrangevariesfrom10to30pixels. 200 300 400 500 100 200 300 400 500 200 300 400 500 100 200 300 400 500 Fig.11.Othersatelliteimagefromthemoon(left),withtherst16selected(right).Radiusrangevariesfrom15to75pixels.H.Chaurisetal./Computers&Geosciences37(2011)331 342 differentcombinationsofcoefcientsmayrepresentthesameimage.ThisiterativeapproachisfeasiblewiththeuseofFFTs.Forthedifferentapplications,wespecifytheradiusrangesinthecaptionofthegures.3.2.OphthalmologyThemotivationshavebeenpresentedintheintroductionpart.Intherstexample(Fig.7),theopticdiskisclearlydenedandthealgorithmeasilydetectsit.InFig.7(bottom),thebrightzonewithintheopticdiskisnotselectedastheminimumradiusissetto30px.Inaslightlymorecomplicatedexamplewiththepresenceofexudates(Fig.8),thealgorithmisstillabletodetecttheopticdisk.Itscircularshapecompensatesforalowervalueofthegradient.Weconcludeonthisexampletheabilityforthetodetectatleastasinglecircle.3.3.AstronomyCountingcratersisamethodforestimatingtheageofaplanetssurface(Kerr,2006).WeselectedtwozonesfromtheMoonimageanddetectedanumberofcratersinaspeciedradiusrange(Figs.9and11).Thesoft-thresholdingprocessas 100 150 200 50 100 150 200 50 100 150 200 50 100 150 200 50 100 150 200 50 100 150 200 50 100 150 200 50 100 150 200 Fig.13.SyntheticSSTmap(top)anditsgradient(bottom).Radiusrangevariesfrom15to40pixels.H.Chaurisetal./Computers&Geosciences37(2011)331 342 proposedhereallowstoremovecircleswiththesameradiiandslightlydifferentpositions.Withinthespeciedrange,thecratersareindeedwelldetected(Fig.9,right).However,somespuriouseventsarealsoselected(Fig.10).Theseareduetothecombinationoftheshallowsunandthetopography.Weindicateinthediscussionparthowtheartifactscouldberemoved.Theapplicationonasecondmoonimageleadstosimilarconclusions(Fig.11).Onthecrateronthebottomleftside,theshapeisratherelliptic.Inthatcase,twosignicantweredetected.3.4.OceanographyIncoastaloceanography,thedetectionofeddieswithasub-mesoscalestructure(20 100km)isakeyelementforabetterunderstandingofthesurfacecirculation.Onremotesensingimages,tracerssuchasthesea surfacetemperature(SST)orthechlorophyllmaps,areusedtorevealtheoceancirculation.Theunderlyingassumptionisastrongcorrelationbetweenthetracerandthevelocityeld(Sugimuraetal.,1984;BorisovandMonin,1989;Essen,1995).Theeddiesaregenerallydetectedeitheronspatialortemporalgradientmaps(AleksaninandAleksanina,2001;Yangetal.,2000).WerefertoCastellani(2005)andNascimento(2006)Haietal.(2008);DAlimonte(2009)foramorecompletereview.Classically,theHoughtransformandseveralothercircleorellipsettingalgorithmsareappliedtodeterminetheradiusandthecentralpositionofeddiesonbinaryedgemaps(PeckinpaughandHolyer,1994;FernandesandNascimento,2006Themaindifcultyfordetectingeddiesiscertainlyduetotheweakandblurrycontours.Weapplythetransformonbothsyntheticandsatelliteimages.Intherstexample,themaincircularfeatureisextractedfromanSSTimagecomputedfromamodelinaturbulentow(Fig.12limitthespiralshape.Onalargerimage,thesoft-thresholdingprocesscoupledwiththetransformisabletodetectaseriesofturbulentstructures(Fig.13).Furtherrene-mentsareindicatedinthediscussionpart.Remotesensingimagesareusuallymoreblurry(Figs.14 16transformisabletodetectthemaineddyonSSTimages.Forthechlorophyllmap,therstfourelementsarerelatedtospiralfeatures:thechlorophylllamentistrappedinacycloniceddy(Fig.16).Theuserhastospecifythenumberof.Abroaderselectionsimplyconsistsofresumingtheiterativethresholdingprocess.4.DiscussionThroughaseriesofapplicationsonsyntheticandrealimages,wehaveshownthecapabilityforthetransformtodetect 100 150 50 100 50 100 150 50 100 50 100 150 50 100 50 100 150 50 100 Fig.14.RemotesensingSSTimageintheGulfofLion,NorthWesternMediterraneanSea(top),andimagegradientmaps(bottom).Radiusrangevariesfrom10to20H.Chaurisetal./Computers&Geosciences37(2011)331 342 50 100 150 200 50 100 50 100 150 200 50 100 150 200 50 100 50 100 150 200 Fig.15.RemovesensingSSTimage(top)anditsgradient(bottom),stillintheGulfofLion.Radiusrangevariesfrom10to20pixels. 100 150 200 250 300 50 100 150 200 250 300 50 100 150 200 250 300 50 100 150 200 250 300 Fig.16.Gradientimageofthechlorophyllmap(left),withtherstfourmoresignicantcircularstructures(right).Fortheselection,theradiusrangevariesfrom5to20pixels.ThespiralshapeonthebottomleftisdetectedbytwoH.Chaurisetal./Computers&Geosciences37(2011)331 342 circularshapes.Theapplicationsarecertainlynotrestrictedtotheeldspresentedhere.Thewidthoftheisimportanttohandleblurryandweakcontrasts.Theusermayeasilychangetheshapeofthe1DwaveletundertheconditionthatEq.(5)issatised.Theexibilityalsocomesfromthepossibilitytospecifyradiusranges.Thelargeredundancyofthetransformisduetotheselectionofmanyradii.Withthesoft-thresholdingapproachpresentedhere,thisisnotreallyanissue,exceptforapplicationsonverylargeimages.Inpractice,theseimagescouldbesplitintosmallerimages.Thesizeoftheoverlappingzoneshouldbetwicethemaximumspeciedradiustoavoidedgeeffects.Wehaveobservedsomespuriousdetections(e.g.Fig.10Therstpossibilitywouldbetomeasurethelocalcoherencyalongarcsfortheselected.Thiswouldremoveartifactsrelatedtotheshadowonthemoonimage.Theotherpossibilitywouldbetodetectcircularstructuresonasequenceofimagesandtrackthem.Applicationsincoastaloceanographywouldbeinteresting,inparticularforremotesensingimageswithweakcontrasts(Maetal.,2006).Otherinvestigationscoulddealwiththemulti-scaleapproachprovidedby.Currently,wehaveselectedasinglescaleandvariousradii.Thesameanalysiscouldberepeatedfordifferentscales.Thiscoulddeliveramorerobustapproachifcircularshapesarestableatdifferent5.ConclusionWehavepresentedaexiblemethodfordetectingdisconti-nuitieswithcircularshapeson2Dimages.Thekeypropertyofthetransformiscertainlythenitefrequencyaspectofthebasisfunctions.ThetransformisefcientduetoitsimplementationintheFourierdomain.Combinedwithasoft-thresholdingalgorithm,itappearstosuccessfullydetectcircularstructuresonaseriesofimagesfromdifferentelds.Thenextstepistotrackthesestructuresonasequenceofimages.Thisisalsopotentiallyawaytoremovesomespuriousdetections.Theauthorsaregratefultothetworeviewersforconstructivecomments.TheyacknowledgepartialfundingfromthePRECOCprojectfromtheFranco-NorwegianFoundation.TheythankJianweiMa(TsinghuaUniversity,China)fortheapplicationontheimagefromthemoon.TheyalsothankEtienneDecenciereandJean-ClaudeKlein(MinesParistech)forthemedicalimages.TheeyeimageswerekindlyprovidedbytheMessidorprogrampartners(seeAppendixA.CircularshapesWeaimatprovingthatwiththedenitionofEq.(7),thehavecircularshapes.Inotherterms,thefunctionsexpressedinpolarcoordinatesshouldnotdependon.Bydenition,wehave.TheinverseFouriertransformof 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