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The strengthening East Australian Current, its eddies and biological effects - an introduction and overview
journal contribution
posted on 2023-05-17, 06:06 authored by Suthers, IM, Young, JW, Baird, ME, Roughan, M, Everett, JD, Brassington, GB, Byrne, M, Condie, SA, Hartog, JR, Hassler, CS, Hobday, AJ, Neil HolbrookNeil Holbrook, Malcolm, HA, Oke, PR, Thompson, PA, Ridgway, KThe polewardflowingEastAustralianCurrent(EAC)ischaracterisedbyitsseparationfromthecoast, 100–200nauticalmilesnorthofSydney,toformtheeastwardflowingTasmanFrontandasouthward flowingeddyfield.Theseparationzonegreatlyinfluencescoastalecosystemsfortherelativelynarrow continentalshelf(only15–50kmwide),particularlybetween32–341S. Inthisregionthecontinental shelfhasamarkedshiftintheseasonaltemperature-salinityrelationshipandelevatedsurfacenitrate concentrations.ThiscurrentparallelstheportionofthecoastwhereAustralia’spopulationis concentratedandhasalonghistoryofscientificresearch.However,understandingofphysicaland biologicalprocessesdrivenbytheEAC,particularlyinlinkingcirculationtoecosystems,islimited.In this specialissueof16papersontheEAC,weexaminetheeffectsofclimaticwind-stressforcedocean dynamicsonEACtransportvariabilityandcoastalsealevel,fromENSOtomulti-decadaltimescales; eddy formationandstructure;finescaleconnectivityandlarvalretention.Comparisonswiththe poleward-flowingLeeuwinCurrentonAustralia’swestcoastshowdifferencesinecosystem productivitythatcanbeattributedtotheunderlyingphysicsineachregion.Onaveragethereis double thechlorophyll a concentrationontheeastcoastthanthewest.IncomparisontotheLeeuwin, the EACmayhavelesslocalretentionoflarvaeandactasapartialbarriertoonshoretransport,which may alsoberelatedtothelocalspawningandearlylifehistoryofsmallpelagicfishoneachcoast.Inter- annualvariationsintheEACtransportproduceadetectablesea-levelsignalinSydneyHarbour,which could provideausefulfisheriesindexasdoestheFremantlesealevelandLeeuwinCurrentrelationship. The EAC’seddystructureandformationbytheEACareexamined.Aparticularcold-coreeddyisshown to havea‘‘tilt’’towardsthecoast,andthatduringarotationtheflowofparticlesmayriseuptothe euphoticzoneandthendownbeneath.Inawarm-coreeddy,surfacefloodingisshowntoproducea new shallowersurfacemixedlayerandpromotealgalgrowth.Anassessmentofplanktondatafrom 1938–1942showedthatthelocal,synopticconditionshadtobeincorporatedbeforeanycomparison with thepresent.ThereareusefulrelationshipsofwatermasscharacteristicsintheTasmanSeaand separationzonewithlarvalfishdiversityandabundance,aswellaswithlong-linefisheries.These fisheries-pelagichabitatrelationshipsareinvaluableforfisheriesmanagement,aswellasforclimate changeassessments. There isfurtherneedtoexaminetheEACinfluenceonrainfall,stormactivity,dustdeposition,and on themovementsbyfish,sharksandwhales.TheAustralianIntegratedMarineObservingSystem (IMOS)hasprovidednewinfrastructuretodeterminethechangingbehaviouroftheEACandits bio-physicalinteractionwiththecoastsandestuaries.Theforecastingandhindcastingcapability developedundertheBluelinkprojecthasprovidedanewtoolfordatasynthesisanddynamical analysis.TheimpactofastrengtheningEACandhowitinfluencesthelivelihoodsofoverhalfthe Australianpopulation,fromBrisbanetoSydney,HobartandMelbourne,isjustbeingrealised.
History
Publication title
Deep-Sea Research IIVolume
58Issue
5Pagination
538-546ISSN
0967-0645Department/School
School of Geography, Planning and Spatial SciencesPublisher
Pergamon-Elsevier Science LtdPlace of publication
The Boulevard, Langford Lane, Kidlington, Oxford, England, Ox5 1GbRights statement
The definitive version is available at http://www.sciencedirect.comRepository Status
- Restricted