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UrbanClimate23(2018)250–259 ContentslistsavailableatScienceDirect Urban Climate journalhomepage:http://www.elsevier.com/locate/uclim Performance standard for tropical outdoors: A critique of current impasse and a proposal for way forward RohintonEmmanuel GlasgowCaledonianUniversity,Glasgow,UK a r t i c l e i n f o a b s t r a c t Articlehistory: Climatechangewillbringmoreheatextremestothealreadywarm Received31May2016 tropicalareasinAsia,AfricaandLatinAmerica.Theresultingsurgein Receivedinrevisedform12December2016 coolingdemandwillonlymakethethermaldiscomfortintropicalcities Accepted5January2017 evenworse.Thispaperpresentsevidencetotheapproachingaircondi- tionedcoolingloaddelugeandshowswhytheairconditionedmanage- mentofcoolingloadisparticularlyproblematicinthetropics.Itthen Keywords: presentsthetechnical,institutionalandculturalchallengestopassive Tropicalurbanclimate climate-sensitivedesigninthetropicsandpositsthreeideasaspartof Urbandesign thewayforward:reformulationofthermalpleasureinthetropics, Thermalcomfort linkingthe‘in’andthe‘out’atneighbourhoodscaleandprovisionof Coolingload Urbanheatisland adaptiveopportunitiesvariedbyactivitypatterns.Researchapproaches toadvancetheseideasarealsodiscussed. ©2017ElsevierB.V.Allrightsreserved. 1.Introduction Unusual(N3standarddeviations[SD]abovethebaseclimateof1951–1980)andunprecedented(N5SD) heatextremesareexpectedtobethenorminmuchofAsiaandAfricaintheneartermevenastheseregions undergotransformationalsocialandeconomicchange(IPCC,2013).InSub-SaharanAfrica,unprecedented heatextremesareprojectedoveranincreasingpercentageoflandareaasglobalwarmingintensifiesfrom 2to4°C,resultinginsignificantchangesinvegetativecoveranddroughtevents(Lottetal.,2013).InSouth- eastAsia,heatextremesthatarevirtuallyabsentatpresentwillcovernearly60–70%oftotallandareainsum- mer,evenundera2°Cglobalwarmingscenario;with4°Cglobalwarming,summermonthsthatintoday's climatewouldbetermedunprecedentedwouldbethenewnormal,affectingnearly90%ofthelandarea (Sillmannetal.,2013).InSouthAsia,thesituationisevenmoreextreme,irrespectiveoftheglobalemission E-mailaddress:[email protected]. http://dx.doi.org/10.1016/j.uclim.2017.01.002 2212-0955/©2017ElsevierB.V.Allrightsreserved. R.Emmanuel/UrbanClimate23(2018)250–259 251 paths(Sillmannetal.,2013;Kumaretal.,2010).Reductionincolddays(Yanetal.,2002),increaseinbothcold andwarmtails(KleinTanketal.,2006),significantincreasesintheannualnumberofhotdaysandwarm nights,decreasesincolddaysandcoldnights(Mantonetal.,2001;Griffithsetal.,2005)andincreasesin warmextremesarealllikelyinmuchofAsiaandAfrica. ThemostpopulouspartsofthesecontinentsarewithintheTropicalbelt(fromapproximately23oNto23oS oftheequator).Consequently,tropicalcoolingload–muchofwhichiscurrentlylatentduetorelativelylow (albeitrapidlyrising)levelsofeconomicdevelopment–islikelytobethedominantcategoryofglobalenergy demand(IsaacandvanVuuren,2009).Inthecurrentparadigm,suchincreasesincoolingloadcouldonlybe metbyairconditioningmoreandmorebuildings(DavisandGertler,2015),exacerbatingthewarmingprob- lem.Atthesametime,deeptechnologicaldevelopmentandefficiencyimprovementsincoolingsystemsare yettobeachieved. Tomakemattersworse,contemporaryculturalpracticesandattitudeslimitadaptivepossibilitiesto warmertemperaturesastheimprovingsocioeconomicconditionsleadto‘thermalindulgence’(Hitchings andLee,2008;Hanetal.,2009;Indraganti,2010a;Karyonoetal.,2015).Thereisevidencethatlong-termex- posuretoairconditionedenvironmentmayevenhamperpeople'sphysiologicalacclimatizationandweaken thermaladaptability(Yuetal.,2012).Greateruseofairconditioningleadstoacycleofculturaldependency, andbreakingitappearsenormouslydifficult(ChangandWinter,2015).Onelikelyoutcomeofthesedevelop- mentsisanunrealisticthermalcomfortexpectationinthetropicsthatisindirectconflictwiththe‘global good’oflow/zerocarboneconomy.Acompromisehastobereachedbetweensocietalprioritiesandpersonal desirestoensurelowestenergyexpenditurewithoutconfiningtropicaldwellerstoan‘inferior’thermal comfort. Thispaperpresentsevidencetotheapproachingairconditionedcoolingloaddelugeinlightofthechang- ingclimatemadeworsebyurbanization,critiquesthecurrentinabilitytoeffectivelydealwiththeproblem andproposesanewwayofmanagingthecoolingloaddelugeby‘climate-sensitivecommons.’TheBackground sectionpresentssixreasonswhythecoolingloadprobleminthetropicsisuniqueandinneedofnewthinking. Inlightofthese,threeideasareputforwardforfutureurbanclimate-sensitivedesigninthetopics.Finally,five researchandknowledgetransferneedsarepositedasnecessarytorealisethesedesignideas. 2.Background Muchoftheclimatechangerisksinthetropicsareconcentratedinurbanareas.Theseincluderisingsea levelsandstormsurges,heatstress,extremeprecipitation,inlandandcoastalflooding,landslides,drought, increasedaridity,waterscarcityandairpollution(Revietal.,2014).Giventhecurrentlevelofurbangrowth andtheconcentrationofpopulationsinvolved,climatechangewillinteractwiththeurbanrisksinavarietyof ways,someofwhichwillexacerbatethelevelofclimaterisk(IPCC,2013).Furthermore,therearehealthin- equalities,especiallyindevelopingcitiesthatarefurtherexacerbatedbyurbanwarming(cf.Campbell- LendrumandCorvalán,2007). However,researchontheaugmentationofclimatechangeeffectsbylocalurbanwarming(characterised byurbanheatislands)remainsweak.Initially,eventheIntergovernmentalPanelonClimateChange(IPCC) overlookedtheroleofcitiesbothasaforcingfactoraswellasakeystakeholderinmanagingclimatechange (HebbertandJankovic,2013).Additionally,translatingfutureclimatechangeprojectionsatfinerspatialscales relevanttocitiestypicallyusestatisticaldownscalingtechniquestoglobalclimatemodelswithoutmodelling theurbanareasthemselves(Lemonsuetal.,2013).Furthermore,thepracticalimplementationofthelimited urbanwarmingknowledgeisrare. Butthingsarechanging:urbanheatislandmitigationisexplicitlymentionedinIPCCAR5WorkingGroup3 Chapter9(Luconetal.,2014).Explicitconnectionsbetweenclimatechangeandactionincitiesisincreasingly beingmade(forexample,Rosenzweigetal.,2015).Toolsandstrategiestoevaluatetheeffectivenessofheat islandmitigationmeasures,suchastheComprehensiveAssessmentSystemforBuildingEnvironmental Efficiency–HeatIslandTool(CASBEE-HI-http://www.ibec.or.jp/CASBEE/english/overviewE.htm)have beenproposed.However,theameliorationoftheheatislandeffectintheurbantropicsisparticularly weak.Ontheonehand,knowledgeoftropicalheatislandsremainspatchyandnumericallyweak (cf.Hungetal.,2006;Roth,2007).Ontheother,theproliferationofstrategiesfocusingonheating- onlyclimates(orthedual-modeheating-and-coolingloadclimates)doesnotreadilytranslateto cooling-onlyregions. 252 R.Emmanuel/UrbanClimate23(2018)250–259 2.1.Uniquenessofcoolingload Thetaskofcoolingisverydifferentfromtheactofheatingduetophysical,socialandeconomicreasons.A keydifferencebetweenheatingandcoolingisintherespectiveloadstructures.Coolingrequiresthetackling oftheincreasesinboththesensibleaswellasthelatentloads(Kalvelageetal.,2014).Inthehumidtropics, thiswouldtranslatetodehumidificationandcooling,doingbothofwhichwithoutover-compensatingfor oneortheotherisextremelychallenging(Sekhar,2016). Second,increaseduseofairconditioninginawarmingworldwillonlymaketheurbansituationworse. Whileontheonehandtemperaturerisewouldleadtogreateruseofairconditioners(e.g.forevery1°C riseambienttemperaturerise,theelectricityconsumptioninHongKongwasestimatedtoincreaseby9.2%, 3.0%,and2.4%indomestic,commercialandindustrialsectors,respectively–Fungetal.,2006)arecent studyinMalaysiafoundthatevery1°Cincrementinoutdoortemperaturewillcausea2%dropinthecoeffi- cientofperformanceofsplit-typeairconditioners(YauandPean,2014).Thisisinsharpcontrasttoheatingin urbanareas,where,wastedheattendstoreducetheheatingloadforsurroundingbuildings(Futcheretal., 2013).Thecurrentincreaseintemperatureduetoairconditionerusewasestimatedtobe0.5°Cbutcould beupto2°Ciftheairconditioneruseistodouble(deMuncketal.,2013:210). Third,evenwhenrunonfossilfuels,heatingcouldbeprovidedbyavarietyoffuels(gas,oil,etc.)thathave lowercarbonfootprintsthanelectricity(especiallycoal-firedelectricity)whichisthepredominantsourceof powerformostairconditioners.Thus,evenasmallincreaseincoolingloadcouldvastlyinflateglobalcarbon emissions. Fourth,muchoftheglobalheatingdemandisalreadymanifestwhilemuchofthecoolingdemandisstill latent.Ürge-Vorsatzetal.(2015)foundthatregionsdominatedbyheatingloadwillseereducedorstagnant growthinenergyusewhilewarmregionsdominatedbycoolingloadwillseeexponentialincreaseincooling loads(seeFig.1andTable1).Thiswillbefurtherexacerbatedbytrendswithincountrieswithheatingand coolingdemand–forexample,USA(Kalvelageetal.,2014)whereheatingdemandisexpectedtodecrease whilecoolingdemandwillsoar.Currentlyheatingloaddominatedcountriestoo,areexpectedtohavesignif- icantcoolingloadsinthecomingdecades. Fifth,coolingitselfispotentiallymoreharmfulfromaglobalwarmingperspectivethanheatinginthatthe refrigerantsusedintheprocess(mostlyhydro-fluorocarbons–HFCs)havegreaterglobalwarmingpotential thanCO .HFCs'contributiontoglobalwarming,muchofwhichisfromairconditioningandrefrigeration,is 2 expectedtobe9–19%(CO equivalentbasis)ofglobalCO emissionsin2050underbusiness-as-usualscenario 2 2 (Veldersetal.,2009). Finally,whilethephysicsandthepracticalitiesaremorecomplexthanheating,cooling–especiallythe mechanisedvariety–isalsohardertodivestof,givenitssocialconstruct.Thecomfortof‘coolth’isoften seenasasignofprogress,initiallyasignofluxurybuteventually,thefulfilmentofdesire.Heatingdoesnot havethisassociationwith‘luxury’sincewarmthwasalwaysseenasaprimordialneed(cf.Sivak,2009). Theassociationbetween‘coolth’andluxuryorprogressisnotuniquetothetropics:thereisevidence(e.g. Ackerman,2002)tosuchassociationintheUnitedStatesduringtheearlyyearsoftheintroductionofair Fig.1.Incomevscoolingloadcomparison(Source:Emmanuel,2016). R.Emmanuel/UrbanClimate23(2018)250–259 253 Table1 Trendsinglobalresidentialspaceheatingandcoolingdemand(kW/m2)(Source:Ürge-Vorsatzetal.,2015). 2010 2020 2030 2040 2050 PacificOECDa 126.1 122.4 119.1 116.0 113.4 NAmerica 147.5 138.4 131.0 124.9 119.7 WEurope 128.3 123.1 118.4 114.2 110.4 Central&EEurope 152.6 148.1 144.8 141.8 139.1 FormerSovietUnion 205.1 198.4 194.5 191.6 189.0 LatinAmerica 63.3 60.2 59.5 59.3 59.6 Sub-SaharanAfrica 56.2 53.4 52.9 53.0 53.4 MiddleEastandNAfrica 55.6 55.1 56.0 57.4 58.0 CentrallyPlannedAsiab 37.4 41.2 43.8 46.8 47.5 SouthAsia 60.1 77.1 85.0 89.2 88.2 OtherPacificAsiac 46.4 45.5 45.6 45.9 46.5 Note(seehttp://www.iiasa.ac.at/web/home/research/researchPrograms/Energy/MESSAGE-model-regions.en.htmlfornamingconven- tionsofworld'sregions). a Cambodia,China(incl.HongKong),Korea(DPR),Laos(PDR),Mongolia,Vietnam. b SoutheastAsiaandthePacificIslandstates. c Australia,Japan,NewZealand. conditioners.However,whatisuniqueaboutthetropicalcoolingloadanditsassociationwithluxuryisthe scaleofthecoolingchallengemadeallthemorepressingbytherapideconomicprogresscurrentlyunderway intheregionandthesizeofthetropicalpopulationthatwilldemandgreatercoolingintheyearstocome. 2.2.Currentimpasseinclimate-sensitivedesigninthetropics Inspiteofthechangestotropicalclimatebothatglobal/regionallevelaswellasatcitylevelthereislittle evidencethatclimatesensitivedesignhasreceivedanygreaterattentionthanithadeverhad.Threebroad categoriesofbarriersneedtobeovercometoenhancethereputationofpassiveclimate-sensitivedesign andembeditintoeverydayurbanlife:technical,institutionalandcultural. 2.2.1.Technical Climateswithclearseasonalityhavethepossibilitytocontroltheindoorsatbuildingenvelopelevel,bya clearseparationofthe‘in’fromthe‘out.’However,giventherelativelysmalldeviationoftypicaloutdoortem- peraturesfromthecomfortrange,tropicalbuildingenvelopesaremoreporous;the‘in’andthe‘out’areoften indistinguishable.Butthiswouldonlyworkiftheoutdoorconditionsareclosetothecomfortrange.Thecrux oftheproblemisthattropics(especiallytheurbantropics)havewarmedtoanextentthatpassive,building- levelstrategiesthatbenefitfromporousbuildingenvelopes(suchascrossventilationandnighttimecooling) areunabletoprovideadequatecomfortbythemselves.Suchpassive‘traditional’approachestoclimate-sen- sitivedesignappearslesseffectiveunderachangingandextremeclimate(Nguyenetal.,2011)especiallyin urbanareas(PozasandGonzález,2016;Rubio-Bellidoetal.,2015;FoudaziandM'Rithaa,2013).Inother words,thepassiveclimate-sensitivedesignoptionsatthebuildinglevelareapproachingthetechnicallimits oflowenergydesigninthetropics,asthebackgroundclimatecontinuestowarm.Weneedagreementonthe ‘what’(i.e.thescope)ofclimate-sensitivedesign. 2.2.2.Institutional/governanceissues Equallyimportantly,the‘how’ofclimatesensitivedesign,too,needsattention.Urbandesign,unlikethe designofindividualbuildings,concernsthatwhichbelongstoallandisthereforesubjecttothe‘tragedyof thecommons’(Hardin,1968).Thepromotionofgoodurbandesignthereforeneedsstronginstitutionalun- derpinning.Onitsown,climatesensitivedesignlacksthecloutandcapacitytograbandholdtheattention ofkeydecisionmakers.Thisisespeciallythecaseintropicalcitieswheretheproblemofovercrowdingand themoreimmediaterisksassociatedwithclimate-change(suchasflooding,coastalerosion,duststorms anddrought)areevermorepressing.Overcrowdinginparticularleadstosmallerbuildingplotsizes,resulting eversodiminishingabilitytocoolbuildingsduetothethermalinterferenceofneighbouringstructures.The embedding of climatesensitivedesign into everyday planning decisions will be important to success. 254 R.Emmanuel/UrbanClimate23(2018)250–259 However,climate-sensitiveplanningisscale-dependentandneedstobelinkedtothebroaderurbansustain- abilityagendassuchaspovertyalleviation,economicdevelopmentandurbanregeneration(Mills,2006; Georgescuetal.,2015). Furthermore,innovativeinstitutionalarrangementsareneededtolinkon-the-groundscientificexpertise totheneedsandrequirementsoflocaldecision-makersatcitylevel(cf.Rosenzweigetal.,2010).Plannedeco- cities(suchastheMarinaBayFinancialCentredistrictinSingapore-https://www.ura.gov.sg/uol/master- plan/View-Master-Plan/master-plan-2014/master-plan.aspx)provideearlyexamplesofsuchinnovative andintegratedinstitutionalarrangements.Additionally,thegovernancearrangementsincitiestooneedcon- sideration:whowillchampionclimate-sensitivedesign?Whoseprioritiesaredominantinurbancontexts; andwhataretheimplicationsofthistoclimatesensitivedesign?Finally,how‘autonomous’arecitiesin beingabletocharttheirownadaptationdestiny? 2.2.3.Culturalbarriers “Themostimportantpointisthateventhemosttradition-minded,nature-orientedorenvironmental- ly-concernedfamilywouldhavedifficultylivinginamodernTrivandrum(capitalofhumidtropical SouthernIndianStateofKerala)homewithoutair-conditioning.(Wilhite,2009,p.193)” Perhapsthegreatestchallengetoclimate-sensitivedesigninthetropicsiscultural.Opennesstopassive climatesensitivedesigndependsonthesocioeconomicstatus.Thosewhocanaffordtheenergyexpenditure onairconditioningtendtobe‘thermallyindulgent’tothepointoflowtoleranceforthermaldispleasure (Indraganti,2010a).ThisleadstowhatChangandWinter(2015)called‘Thermalmodernity.’Additionally, culturalpracticesandpreferences/attitudesleadto“restrainedadaptiveopportunity”(Indraganti,2010b), resultingfromthewayalternatechoicesarepresentedandmadepossible(Wilhite,2009).Examplesof suchculturalpracticesandpreferencesincludethepracticeofairconditioningallpublicplaces(Hitchings andLee,2008),increasedindoordwellingasclimatewarms(ZivinandNeidel,2014),enjoyingthecoolcom- fortofexcessivelycooledshoppingmallsinIndiaandSingapore(Chua,2003)andwinterwearinSingaporeas ‘culturallyexpressiveformsofclothing’(HitchingsandLee,2008). Astropicalcountriescontinuetheirmarchtowards‘middleincome’statusgreatercomfortisdemandedby moreandmoreoftheircitizens.Animmersioningreatercomfort(i.e.greaterpleasure)appearstohyper-sen- sitizehumanstoapointofinabilitytocopewithnaturalvariationsintemperature.Whiletheuseofaircon- ditioningundoubtedlyleadsto‘superior’comfort(andhascometobeseenasasignof‘progress’inthetropics –see,Lee,2009)italsodiminishesthecopingmechanismsoftropicaldwellers. Climate-sensitivedesigncouldhelp,but,unfortunatelyithadhithertolargelyremainedaneliteprojectin thetropics,wherethevastmajorityofbuildingscontinuetoberelegatedtotheintolerable-to-barely-passable margins.Nocontextexistsfortheenjoymentofanotherwisepleasantclimatebyamajorityofcitizens. 3.Wheredowegofromhere? Itissaidthatthermalcomfort(intemperateclimates)needstobe‘re-contextualised’inlightofclimate change(Coleetal.,2008).Thisoftenmeansamoreinclusive,inhabitant-controlled,flexiblenotionofthermal comfortthatallowsfor‘inhabitantagency’(Coleetal.,2008)butquestionsremainastoitsapplicabilityinthe high-density,rapidlygrowingandgenerallyresource-poorurbantropics.Thenatureoftropicalthermalcom- fort,especiallyinlightofchangingurbanclimate,isnotalwaysachievableevenwith‘inhabitantagency,’at leastnotmostofthetime.Whatthereforemustwedointhetropics? Creatingaclimate-sensitiveurbanrealmisastrongpossibilityinthetropicsthatwouldenablethe‘condi- tioning’ofindividualbuildingseasier.Thusitisproposedthatthechangingtropicalclimate,especiallyinthe citiescouldonlybemadecomfortable(andplacesforhumanthriving)byclimate-sensitizingtheurbanrealm. Itisnotexpectedthatdoingsowilleliminatetheneedforairconditioning.Farfromit;climate-sensitiveurban designisacrucialenablerofoutdoorliving,eveninthefaceofclimatechange.Thiscouldcreatethecondition foralternatewaysofenhancingurbanqualityoflifewhileindividualbuildingsmayormaynotneedaddition- alcoolth. R.Emmanuel/UrbanClimate23(2018)250–259 255 Thisendeavoriswiderthanwhataplanningoranurbandesignremitwouldallow.Weneedanewwayof being,whichhasimplicationstothewaytropicaldwellersperceiveclothing,furniture,foodandindeedtheir bodies.Whilethisisfartoowideasubjecttobecoveredinthispaper,threeideasarepositedascentraltothe achievementofthermalcomfortinthetropicsasastartingpointforclimate-sensitivedesign: Reformulationofthermalpleasureinthetropics. Linkingthe‘in’andthe‘out’atneighbourhoodscale. Provisionofadaptiveopportunitiesvariedbyactivitypatterns. 3.1.Reformulationofthermalpleasureinthetropics Thermalpleasureinahotenvironmentisverydifferenttothatinacoldenvironment:coolnessisonly ‘skindeep’(i.e.wefeelevaporativeandconvectivecoolingonthesurfaceoftheskin,asopposedtowarmth, whichisinternal–cf.Heschong,1979).Itisalsoaboutcalmingthesensesinahighly-(almostover-)simu- latedenvironmentwheredeepshade,vegetationandwaterindividuallyorcollectivelyplayaroleincreating asereneandcalmingeffect. Attheheartofthisformulationofthermalpleasureisanurbanasymmetricalthermalenvironmentdom- inatedbycoolspotsthatenablesgreaterenjoymentoftheoutdoors–aformofspatialalliesthesia(Parkinson anddeDear,2015),thusenablinglow-energycoolingintheindoors.Anurbanasymmetricalthermalenviron- mentcouldbeachievedinanumberofdifferentways,allaimingtocreateclimatically‘cool’urbanpublic spaces: Partiallyshadedpathways. Strategicallyplacedandadequatevegetationcover. Watermisting(seeEmmanuel,2016forfurtherdetails). 3.2.Linkingthe‘in’and‘out’atneighbourhoodscale Theachievementofthermalcomfortinthetropicsisaboutthe“integrationofmicroclimate,formandfab- ricofthebuilding”(RajapakshaandHyde,2012).Airconditioningleadsto“hardeningofthephysicalandso- cialboundariesbetweenhomeandsurroundings”(Wilhite,2009).Substantialimprovementinindoor thermalcomfortispossibleonlyifeffortstodosobeginattheneighbourhoodscale(i.e.outsidethebuilding). Examplesoflinkingthe‘in’andthe‘out’atneighbourhoodscaleinclude,arcadedstreetfrontswrapping aroundallbuildinginanurbanblock,tree-linedbuildingfrontagethatactaporousintermediarybetween the‘in’andthe‘out’andshadingoftheinterstitialspacesbyajuidiciouscombinationofthree-dimensional geometryof buildings andtheirsolarorientation (asexemplifiedbythe‘shadowumbrella’concept– Emmanuel,1993).Suchmanipulationofsettlementgeometry,streetorientationandexternalfactorssuch asstreettreescreate‘environmentaldiversity’(SteaneandSteemers,2004)thatwouldbecentraltoachieving thermalcomfortinthetropicsbyclimaticallylinkingtheinsideofbuildingswiththeoutside. Thelinkingofthe‘in’andthe‘out’oughttoreflectthepurposeforwhichthermalcomfortstandardsare beingpromulgated.Lenzunietal.(2009)suggestdifferentiationofthermalstandardsalongthefollowing: thesubject'sthermalsensitivity,accuracyrequiredforcarryingoutthetaskandthepracticalityofthermal control.Wesuggestafourth,thedifferencebetweentheindoorandtheoutdoorconditionsthatneedtobe achieved. 3.3.Provisionofadaptiveopportunitiesvariedbyactivitypatterns Giventheyear-roundpossibilitytousetropicaloutdoorsfordailyliving,urbanthermalcomfortgains greaterimportanceintheovercrowdedtropicswhereroomoccupancyratesareunhealthy(cf.Correa, 1989).Acriticalneedistospecifyoutdoorthermalstandardsintermsofurbanactivitiesthatfacilitatecom- fortablemovementintheoutdoor,leadingtohigherquality-of-life. Suchextensiontothecomfortzonecouldbegreatlyfacilitatedbytheprovisionofadaptiveopportunities thatareorganisedaroundactivitypatternsoftropicalurbanlife.Emmanuel(2005)suggestedfoursuchadap- tiveopportunitiesorganisedaroundtropicalactivitypatterns(SeeFig.2): 256 R.Emmanuel/UrbanClimate23(2018)250–259 Fig.2.Conceptualsketchesoutlining(a)Gatheringplaces,(b)shoppingstreetsand(c)pedestrianpathsandnodesthatalsofacilitateeve- ninglife(Source:Emmanuel,2005). a. ShoppingStreets–createcanyon-likeshoppingstreets,wherethestreetitselfisnorth/southrunning,with buildingsonthewestbeingslightlytallerthanthoseontheeast.Linebothfacadesofstreet-facingbuild- ingswitharcades,soastoprovideadequateprotectionfromrainandsun. b. GatheringPlaces–surroundurbanwaterbodieswithabuiltformedgedbyarcades.Locatepublicactivities alongthearcade,overflowingintothecommons.Dissuadeallactivitiesthatdonotdirectlybenefitfrom water'sedgefromlocatingonurbanwaterfronts. c. Provisionsforeveninglife–Eveningsaretropics'winter(Rao,1981).Streetcornersareespeciallyattrac- tivetobeincorporatedintotheeveninglife,particularlyiftheyintersectnortherlyandeasterlyorienta- tion. d. PedestrianPathsandNodes–Establishanetworkofpedestrianlinksindependentofcitystreetnetwork. Pathswithincityblockscouldbetheprimarycarriersofcoolair(sayfromapond).Whereverthepedes- trianpathcrossesthevehicularpath,establishaplacetopause. 4.Researchandknowledgetransferneeds Beforetheabovethreearegivenconcreteurbanform,itisnecessarytoconductfurtherresearchonthe tropicalurbanwarmingproblem.Thesepertainto“data,technicalandscientificneeds”(suchasrelative meritsofshadevs.ventilationtotropicalthermalcomfort),“socio-physiologicalandhabitualneeds”(such R.Emmanuel/UrbanClimate23(2018)250–259 257 asthermalcomfortintheoutdoors,performancestandardsfordifferentactivitypatterns)and“politicaland institutionalneeds”(implementationandmonitoring,urbanclimate↔globalclimatefeedback): 4.1.Shadevsventilation Thecoolingeffectofventilationinthetropicsisnowpartoftheconventionalwisdom.Whatisnotwell acknowledgedarethethermalcomforteffectsofwindinawarmingcity.Thecombinedradiantcoolingeffect ofshadetogetherwiththeconvectivecoolingofwindontropicalthermalsensationneedsfurthersystematic study.Theseasonalityofwind(asaffectedbythemonsoons)inconjunctionwiththeannualvariationsin temperatures(highscoincidingwithweakwindpatternsduetothepassageofintertropicalconvergence zone)needstobereflectedinfieldstudies.Thesubstantialbodyofresearchonshade-orientedplanningin hot,dryclimatesandtheknowledgeofwindinhot,humidclimatesneedtobebroughttogethertounder- standthepracticalpossibilitiesofboth,inwayssimilartothatattemptedbyBalslevetal.(2015). 4.2.Thermalcomfortinoutdoorswithavarietyofmorphologies Closelyrelatedtothisisthecollectionofempiricalevidencetotheeffectofavarietyofurbanmorphologies onoutdoorcomfortintheurbantropics.Thiswouldbenefitfromastandardizationofmeasurementprotocols foroutdoorcomfort(cf.Johanssonetal.,2014).AkeyrequirementistheaccurateestimationofMeanRadiant Temperature(T )whichismorecriticalinawarm,humidcontextthaninacold,dryone.Integralradiation MRT measurementsandthecalculationofangularfactorsasproposedbyThorssonetal.,2007isneeded.Johansson etal.(2014)provideacomprehensiveoverviewofthemanytechniquestomeasureT . MRT 4.3.Performancestandardsbyactivitypatterns/landuse Theabovetwoareasofresearchshouldleadtoperformancestandardsforoutdoorurbanspaces.Asdiscus- sioninSection3,itwouldbeidealifthesecouldreflectthemanyactivitypatternsappropriatefortropicalcit- iesandhighlightedinthediscussionsabove. 4.4.Neighbourhoodscaleimplementationandmonitoring Ultimately,theproofofthepuddingisintheeating.Aconsiderablebodyofknowledgealreadyexistson approachesbasedontropicalventilation(Ng,2016),shade(Lin,2016)andvegetation(Duarte,2016).Both traditionalsettingsand‘newtowns’developedpostWWIIcouldberipeforempiricalmeasurementsofout- doorthermalcomfortconditionsunderthesethreeapproachesinthetropics. 4.5.Urbanclimateameliorationandregionalclimatefeedback Astropicalcitiesgrow(andturnintomegapolii)moredirectfeedbackbetweenurbanland-coverandre- gionalandperhapsglobalclimatemaybeforeseen.Althoughcitiescurrentlyoccupyonlyatinyfractionof globallandcoverthismaychangedramaticallyinthetropicssoastohavearegionalclimateimpact.Thecli- matetransformationofPearlRiverDeltaisacaseinpoint(Wangetal.,2014).Itisnecessarytostudysuch regionalfeedbacksingreaterdetail.However,thenotoriouslywickedproblemofreliablelanduse/land coverdatainthetopicsneedtobetackledfirst.Inthisregard,currentinitiativessuchastheWorldUrbanDa- tabaseandAccessPortaltools(WUDAPT,Seeetal.,2015)andlanduse/landcoverparameterizationschemes suchasLocalClimateZone(LCZ,StewartandOke,2012)couldofferpromisingheadstart.WUDAPTisacom- munity-driveninitiativeamassingdataonurbanformandfunctiontohelpcitiesworldwidetodeveloptheir ownheat-adaptationplans.Thiscouldprovideastandardizedcharacterizationoftheworld'smajorcitiesand detailedinputdataforurbanclimatemodels.ApplicationofaversionofLCZfordata-poortropicalcitieshas beenrecentlydemonstrated(PereraandEmmanuel,2016). 258 R.Emmanuel/UrbanClimate23(2018)250–259 5.Concludingremarks AmeliorationofUHIprovidesalocalnarrativewithinwhichstrategiesfortheenhancementofurbanqual- ity-of-lifecanfindacceptanceandevenactivesupport.Apoliticaldifficultywithactionagainstglobalclimate changeistheinabilitytoseeresultsinthehereandnow.Tacklingtheurbanclimatechangeoffersimmediate andtangiblebenefitssincethenegativeconsequencesofhaphazardurbanizationisplaintosee.Thisisin- creasinglybeingrecognisedininternationalefforts.Examplesincludegreaterfocusonurbanclimatebythe WorldMeteorologicalOrganisation(suchasthe“WMOUrbanAgenda”–http://public.wmo.int/en/our- mandate/focus-areas/urban-development-megacities/wmo-and-new-urban-agenda); World Health Organisation's(WHO)greaterattentiontopublichealth–especiallyageinginthechangingclimate(http:// www.who.int/globalchange/en/), and UN-Habitat III's smart city and quality of life agenda (http:// unhabitat.org/wp-content/uploads/2015/04/Habitat-III-Issue-Paper-21_Smart-Cities-2.0.pdf).Rapidlygrow- ingtropicalcitiesneedtoparticipateinsuchinternationaleffortstoenhancetheirlocalenvironmentalcondi- tionsevenastheycontributetotheglobalclimatechangeadaptationagenda.Experiencegainedinsuch endeavourscouldenabletropicalcitiestopositivelycontributetothetwo-wayknowledgetransfer(between thedevelopedanddevelopingworlds)oflivinginawarmingworld. 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