ContentslistsavailableatScienceDirect
Landscape
and
Urban
Planning
j o ur na l h o me p a g e:w w w . e l s e v i e r . c o m / l o c a t e / l a n d u r b p l a n
Carbon
dioxide
balance
assessment
of
the
city
of
Florence
(Italy),
and
implications
for
urban
planning
Francesco
Primo
Vaccari
a,∗,
Beniamino
Gioli
a,
Piero
Toscano
a,c,
Camilla
Perrone
b aInstituteofBiometeorology(IBIMET),NationalResearchCouncil(CNR),ViaG.Caproni,8,50145Florence,ItalybDepartmentofUrbanandRegionalPlanning(DUPT),UniversityofFlorence,ViaP.A.Micheli,2,50121Florence,Italy cDepartmentofAgriculturalandEnvironmentalSciences,UniversityofUdine,ViadelleScienze,206,33100Udine,Italy
h
i
g
h
l
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g
h
t
s
•Florence’sgreenareasoffsetCO2emissionsfrom2.6%(winter)to16.9%(spring).
•SpatiallyCO2emissionsdecreaseby92%alonganurbantorurallandscape.
•Carbondioxidebalanceprovidesinnovativeinformationtoolforurbanplanning.
a
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f
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Articlehistory: Received9August2012
Receivedinrevisedform9August2013 Accepted10August2013
Keywords:
Carbondioxidefluxes Eddycovariance Urbandesign Urbantransect
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ThecarbondioxidebalancefortheMunicipalityofFlorence(102.3km2),with29.1km2ofgreenspace withinthebuilt-upcityand46.6km2inthesemi-ruralperi-urbanarea,showsthatcollectivelythegreen spacesoffset6.2%ofthedirectcarbonemissions.Howeverthegreenspacesinthedenselybuilt-upcity onlyoffset1.1%oftheemissions.13.5ktCO2y−1aretakenupbyvegetationinthebuilt-upareasand 58.7ktCO2y−1byvegetationintheperi-urbanarea.Urbangreenspacesaremostefficientinoffsetting anthropogenicCO2emissionsduringtheperiodMarchtoJunewhenplantgrowthratesarehighand emissionratesarerelativelylow.Landscapefragmentationishighlypositivelycorrelatedwithtotal CO2 emissionsandnegativelycorrelatedwithCO2uptake.Thedetailedinformationproducedduring thisinvestigationshowsthatpoliciesaimedatreducingCO2emissionsinwintermonthswillhavea greateroveralleffectontotalCO2releasetotheatmospherethanthoseaimedatincreasingCO2uptake. Nevertheless,urbandesignersshouldconsiderallthebenefitsofurbangreenspacesandseektoensure thatnewsuburbandevelopmentconservesgreenspacesandaimsatsustainableurbandesign.
© 2013 Elsevier B.V. All rights reserved.
1. Introduction
Urbanareas, defined asdensely developed residential,
com-mercialandothernon-residentialareas,cover aminuteportion
of the Earth’s land surface (<3%), but host more than 50% of
thepopulation(CIESIN,2004), thuscontributing significantlyto
globalanthropogenicemissionsofgreenhousegases(GHG)tothe
atmosphere(Dhakal,2010).To mitigatesuchemissions,several
strategiesaimedatimprovingtheurbanenvironmentecological
performance have beenproposed and adopted duringthe past
decade:improving the energy efficiency of buildings (Aydin&
Cukur,2012);reducingroadtraffic(Reckien,Ewald,Edenhofer,& Ludeke,2007);managinganddesigningexistingandnewurban
greenspaces(Patakietal.,2011).
∗ Correspondingauthor.Tel.:+390553033711;fax:+39055308910. E-mailaddresses:f.vaccari@ibimet.cnr.it(F.P.Vaccari),b.gioli@ibimet.cnr.it (B.Gioli),p.toscano@ibimet.cnr.it(P.Toscano),camilla.perrone@unifi.it(C.Perrone).
Therole of urbangreenspaces, defined asallareas covered
bylawns,shrubsandtrees,inhighlyhumanalteredecosystems,
iswellrecognized(Dobbs,Escobedo,&Zipperer,2011).Thereis
asignificantamountofscientificliteratureunderliningthe
ben-efitsofurbangreenspacesinreducingtheurbanheatislandby
creatingacoolingeffect(Hu&Gensuo,2010;Ng,Chen,Wang,&
Yuan,2012;Oliveira,Andrade,&Vaz,2011;Onishi,Cao,Ito,Shi, &Imura,2010;Petralli,Massetti,&Orlandini,2011;Steeneveld, Koopmans,Heusinkveld,vanHove,&Holtslag,2011),orinterms
ofavoidedcarbonemissionsandenergyuseduetothecoolerair
temperature(Lin,Wu,Zhang,&Yu,2011);reducingairpollution,
particulatesandgases(Morani,Nowak,Hirabayashi,&Calfapietra,
2011;Nowak,Crane,&Stevens,2006;Paoletti,Bardelli,Giovannini, &Pecchioli, 2011; Tallis, Taylor,Sinnett, & Freer-Smith,2011);
filteringnoiseandenhancingthequalityoflife,intermsof
psycho-logicalwell-beingofthecitizenswholiveclosetothegreenareas
(Chiesura, 2004; Gidlöf-Gunnarsson & Öhrström, 2007; Hartig, Evans,Jamner,Davis,&Garling,2003).
Themagnitudeoftheseeffectsdependsmainlyonintrinsic
fac-torsrelatedtourbangreenspacessuchas:surfacearea,vegetation
0169-2046/$–seefrontmatter © 2013 Elsevier B.V. All rights reserved. http://dx.doi.org/10.1016/j.landurbplan.2013.08.004
structure(woody,shrubs,herbaceous),speciescomposition and
locationoftreesinrelationtothebuildings(Akbari,2002;Mirzaei&
Haghighat,2010),andonextrinsicfactorssuchaslatitude,climate,
weatherandtypicalurbanforms ofthecities(Sproken-Smith&
Oke,1998;Upmanis&Chen,1999).
Onewell-recognizedeffectofurbangreenspacesistheir
contri-butiontomitigateGHGemissionsbymeansofatmosphericcarbon
dioxide(CO2)uptakethroughplantphotosynthesis.Several
stud-ieshavequantifiedtheCO2sequesteredandstoredbyurbangreen
spaces(Escobedo,Kroeger,&Wagner,2011;Jo&McPherson,1995;
McHale,McPherson,&Burke,2007;Nowak&Crane,2002;Zhao, Kong,Escobedo,&Gao,2010),andthelong-termdirect
measure-mentsofCO2 fluxesareacknowledgedtoolstoassessthespatial
and temporal variability of CO2 uptake and emission in cities
(Grimmond,King,Cropley,Nowak,&Souch,2002).
Eddycovarianceisamicrometeorologicaltechniquethat
meas-ures the surface-atmosphere exchange of mass, energy and
momentum,and is utilized since decades toassess the carbon
exchange of natural and cultivated areas, contributing toward
understandingthespatialandtemporalvariabilityofecosystems
productivity and their role in theglobal carbon cycle (Keenan
etal.,2012).Theeddycovariancetechniquehasbeenalsorecently
applied in urban and suburban areas (Crawford, Grimmond, &
Christen,2011;Giolietal.,2012;Helfteretal.,2011;Kordowski &Kuttler,2010;Patakietal.,2009;Pawlak,Fortuniak,&Siedlecki, 2010;Velasco&Roth,2010),allowingdirectcarbonfluxesofcities
withdifferentlandscapeorurbancharacteristicstobeassessed.
InthisarticlewecomputetheCO2balanceofthe
Municipal-ityof Florence(emissions-uptakes)byassessingthecapacity of
urbangreenspacesofoffsettingthedirectanthropogenicCO2
emis-sionsthroughcarbonuptake.Florencewaschosenasacasestudy,
becausehighspatialresolutioninventorialdataareavailableand
CO2 emissionsofthecitycenteraremeasuredwitheddy
covari-ancesince2005(Matese,Gioli,Vaccari,Zaldei,&Miglietta,2009).
The total direct CO2 emissions of thecity have been obtained,
combiningmeasuredCO2 emissionswiththeRegionalEmission
Inventory(IRSE).Moreover,usingdifferentweb-GISdatabaseswe
determinedthesurfaceareasofthevariouscategoriesofurban
greenspacesinthecity,andapplyingtheIPCCmethodology(IPCC,
2003,2006)weassignedanannualCO2uptakefactortoeachurban
greenspacecategory.Therelativeimportanceofabsorbedvs.
emit-tedCO2hasbeenassessedbothtemporally,bymeansofseasonal
patternsprovidedbydirecteddycovariancefluxmeasurements
inurban(Florence)andinaMediterraneanforest(Lecceto,Siena)
environments,andspatially,bycomputingtheCO2 balanceover
differentareasrangingfromdenselyurbantorurallandscapes.
Thepaperaimsto:(i)estimatethemagnitudeofthe
anthro-pogenicCO2emissionsoftheMunicipalityofFlorenceandofthe
urbangreenspacesCO2uptake;(ii)investigatesourceandsink
spa-tialvariabilityathightemporalresolutionandtheirimplicationsfor
urbanplanning.
2. Materialsandmethods
2.1. Studyarea
Florence(Lat43◦46N;Long11◦ 15 E)(Fig.1),hasatypical
medievalheartandtherenaissancecitywasbuiltontheruinsofa
Romantown,inarivervalleysurroundedbyhills.The
Municipal-ityextendsover102.3km2,withatotalsurfaceareaofurbangreen
spacesof75.7km2formedbytwomaincategories:thoseindensely
built-upzones,definedhereasUrbanGreenareas(UG)
extend-ingover29.1km2,andPeriUrbangreenareas(PU),definedhere
asurbanareasoflow-densityhousingextendingover46.6km2.
Inadditiontothesetwomaincategories,therearealsoatotalof
11,541isolatedUrbanTrees(UT),manyofthemalongavenuesand
streets.Theyinclude8326trees,manageddirectlybythe
Munici-pality(UTMF),and3215treesownedbyotherpublicinstitutionsor
byprivate(UTO).
TheUGareascanbeclassifiedintwomaincategories:those
managed by the Municipality of Florence (UGMF=7.7km2), for
whichadetaileddatabaseofmorphometricparametersisavailable,
andthoserepresentedbyparksandurbangreenspacesmanaged
byotherpublicinstitutionsandbyprivate,definedhereasother
urbangreenspace(UGO=21.4km2).
ThePUareas surroundingthecityare: agriculturalfieldson
thevalleyfloor,typicallyhorticulturalwithapredominant
com-ponentofherbaceousplants(PUH)andextendingoveratotalarea
of9.5km2;agriculturalfieldsonthehillsaroundFlorence,typically
orchards,vineyardsandsparseolivetreeswithapredominant
com-ponentofwoodyplants(PUW),extendingoveranareaof33.4km2;
naturalforests(PUF)extendingover3.7km2.
AccordingtotheFlorenceMasterPlanthetotal urbangreen
spaces willbeenhanced by2.3km2 (UG
SP),and28,450isolated
urbantrees(UTSP)willbeplantedorreplaced.
Thetypesofurbangreenspacesandtreenumbershavebeen
obtainedbyoverlappingdifferentGISlayersoftheMunicipalityof
Florence(Opendatahttp://datigis.comune.fi.it)(Fig.2).In
particu-lartheweb-GISsuppliedlayersfortheUGMFandUTMFcategories,
thattheywerecreatedin1990withthepurposeofmanagingthe
urbangreenspaces.Theselayersarecontinuouslyupdatedandthey
providedsomefundamentalinformationforourresearch,suchas
plantspeciescompositionineachtypeofarea,theageofthetrees,
andmorphometricinformationsuchasdiameteratbreastheight
(DBH).Theotherurbangreenspacecategoriesweredetermined
byoverlappingtheGISlayersprovidedbytheFlorenceMasterPlan
thattakealltheothercategoriesintoaccount;unfortunatelythese
GISlayersdidnotprovidedetailedinformationaboutplantspecies.
Allthemapscreatedwiththisoverlappingweresubsequently
val-idatedthroughdigitalorthophotos.
2.2. TheIRSEdata
TheIRSEemissiondatabaseisbasedontheCorinair
methodol-ogy(EEA,2007)andwasdevelopedbytheRegionalAdministration
ofTuscany(IRSE,2010).Itcontainsyearlyamountsofpollutants
emittedsince1995,spatiallydisaggregatedat1km2resolution,on
thebasisofspatialproxiesofemissionintensity.Emissionsources
areclassifiedaccordingtotheEuropeanstandardnomenclature‘97
calledSNAP(SelectedNomenclatureforAirPollution),andinclude
threecategories:(i)diffuse:thatarenotlocalized,butdistributed
ontheterritory;(ii)punctual:that aregeographicallylocalized;
(iii)linear:relatedtolinearinfrastructuresuchasroadsand
rail-waylines.Inourstudy,byoverlappingtheadministrativeborders
oftheMunicipalityofFlorencewiththeIRSEspatializeddata,we
determinedtheannualdirect CO2 emissions(Fig.3).In practice
weconsideredonlytheCO2emissionswithinthecityboundaries
(Scope1,definedbyKennedyetal.,2010)andrecentlyadoptedin
theGlobalProtocolforCommunity-ScaleGreenhouseGas
Emis-sions (C40 & ICLEI, 2012C40, ICLEI, World Resources Institute,
2012).
2.3. UrbanandforestCO2fluxmeasurements
Twoeddycovariancesiteshavebeenusedinthisstudyto
mea-sureCO2fluxes.ThefirstwasinstalledinSeptember2005atthe
Ximeniano Observatory(Lat43◦ 47 N;Long11◦ 15 E)(Fig.1),
inthecitycenterwherefluxesareentirelygovernedby
anthro-pogenicemissions,consideringthelackofgreenspaceintheflux
footprint(Mateseetal.,2009).ObservedCO2fluxesaretherefore
Fig.1. MapofItalyshowingthelocationoftheMunicipalityofFlorenceandthemediterraneanLeccetoforest(Si).IntheaerialphotographofFlorenceareshownthered startoindicatetheXimenianoObservatorysite,andtheurbantransect,dividedinsixsectionsfromT1toT6torepresentacontinuumfromurbantorural.
(Giolietal.,2012).ThesecondwasinstalledinJune2005inthe
Lec-cetoMediterraneanforest(Lat43◦18N;Long11◦16E)(Fig.1),a
holmoakcoppiceof20yearsage,located70kmsouthofFlorence
andextendingoveranareaofabout9km2.Meancanopyheight
is8.6mwithameantreeDBHof9.0cmanddensityof2948trees
ha−1,whilemeanannualNetEcosystemExchange(NEE)is−13.2
(±3.7)tCO2ha−1y−1(Magno,Gioli,Vaccari,&Canfora,2010),
rep-resentingaCO2sinkfromtheatmosphere.Bothtowers,whichare
stilloperating,usetheacquisitionprocedureindicatedbyMatese
etal.(2008)andadoptthesamefluxdataprocessingmethodology (Baldocchi,2003).
2.4. UrbangreenspacesandurbantreesCO2uptake
Usingthedetailedinformationaboutsurfaceareas,typeofgreen
space,species compositionandmorphometricmeasurementsof
thesingle trees, provided by the Municipality,we assigned an
annualCO2uptakefactorforUGMFandUTMF categories,through
ananalysisoftheliteratureandusingtheGuidelinesoftheIPCC
(IPCC,2003,2006),whichprovideatieredstructureofmethods
withvaryingdegreesofcomplexity.TheseCO2uptakefactorswere
thenappliedtootherurbangreenspacecategories:UGO,UTO,UGSP
andUTSP.
TheUGMFisformedbyfourcategories:Lawn,Forest,Mixed
Veg-etationandLawnwithShrubs,andforeachcategoryweassigned
aCO2 uptakefactor(Table1).ForLawncategoryweadoptedthe
valueof4.3tCO2ha−1y−1,correspondingtothevaluefortheannual
NetPrimaryProductionofGrasslandoftheWarmTemperate–Dry
ClimateZone(Chapter3.4–IPCC,2003).ForForestcategorywe
adoptedthevalue of 5.8tCO2ha−1y−1 determinedin a specific
case study using the Cascine Park in Florence (Paoletti et al.,
2011).For MixedVegetation,definedas anareawithtrees and
shrubs,and Lawn withShrubs categories, we addeda value of
0.07tCO2ha−1y−1asthecontributionoftheshrubs,accordingto
Zirkle,Lal,Augustin,andFollett(2012,chapter14,part3),tothe
previousuptakefactoridentifiedforLawnandForest.
Since2002,intheMunicipalityofFlorencedatabase,eachtree
hasbeenidentifiedand classifiedin termsof botanicalspecies,
geographicalpositionandmorphometricmeasurements.
TodeterminetheCO2 uptakefactorforthetreecategorywe
appliedthefollowingequation,(IPCC,2003):
CO2=
(CO2(t2)−CO2(t1))
(t2−t1)
(1)
whereCO2=carbondioxidecontentdifference.CO2(t2)=carbon
dioxidecontentreferredtotime2.CO2(t1)=carbondioxidecontent
referredtotime1.t2=time(2011)t1=time(2006).
TodeterminetheCO2contentoftheurbantrees,asrequiredfor
inEq.(1),weusedtheStockChangeMethod(IPCC,2003)applying
thefollowingequationforeachplantgenus:
Ctot=(V×D×BEF)×(1+R)×CF (2)
where Ctot=total carbon (above+below biomass). V=tree
vol-ume,m3.D=wooddensity,tm−3.BEF=BiomassExpansionFactor.
R=Root-to-ShootRatio.CF=carbonfractionofthedrybiomass.
Thetreevolume(V)wasdeterminedconsideringtheDBHvalues
foreachplantgenus,usingdendrometrictablesatsingleentry(CRA,
1980).Thewooddensities(D),foreachplantgenus,wereobtained
usingthevalues indicatedforItalybyFAO(2005); weusedthe
valuesof1.3forconiferspeciesand1.4forbroadleafspeciesasBEF
(IPCC,2003),whilefortheCFweusedthestandardvalueof0.5 (IPCC,2003).
TheaverageCO2uptakefactorpertree,determinedfollowing
theaboveprocedure(Table2),wasthenusedtoevaluatethetotal
Fig.2.Urbangreenspaces(uppermap)andurbantrees(lowermap)oftheMunicipalityofFlorence.
Table1
CategoriesoftheUGMF,withindicationsaboutthetotalsurface(ha),theCO2uptakefactor(tCO2ha−1y−1)andthetotalCO2uptakeperyear(tCO2y−1).
Categories Surface(ha) (%) CO2uptakefactor(tCO2ha−1y−1) TotalCO2uptake(tCO2y−1)
Lawn 562.3 73.0 4.3 2417.9
Forest 84.79 11.0 5.8 491.8
Mixedvegetation 79.75 10.4 5.9 470.5
Lawnwithshrub 43.16 5.6 4.4 189.9
770 100 3570.1
Table2
Plantgenus,numberoftreespergenus,numberofobservationsofdiameteratbreastheight,CO2increment(tCO2y−1)andCO2incrementpertree(tCO2y−1tree−1)ofthe
10generaofthetreesmanagedbytheMunicipalityofFlorenceandusedtodeterminetheCO2uptakefactorpertree.
PlantGenus Commonname No.trees No.obs. CO2Incr.(tCO2y−1) CO2Incr.pertree(tCO2y−1tree−1)
1 Tiliaspp.L. Lindentree 8621 10,559 357.8 0.0415
2 Quercusspp.L. Oaktree 8097 9048 105.8 0.0131
3 Cupressusspp.L. Cypresstree 8034 8683 244.6 0.0304
4 Celtisspp.L. Europeannettletree 6765 8178 166.4 0.0246
5 Pinusspp.L. Pinetree 5219 6748 344.7 0.0660
6 Platanusspp.L. Planetree 4415 6580 124.2 0.0281
7 Acerspp.L. Mapletree 3626 2119 28.8 0.0079
8 Oleaspp.L. Olivetree 3539 2907 12.1 0.0034
9 Ulmusspp.L. Elmtree 2148 3303 76.6 0.0357
10 Fraxinusspp.L. Ashtree 2087 1213 16.6 0.0079
Fig.3.DirectcarbondioxideemissionsoftheMunicipalityofFlorenceexpressedas ktCO2y−1.
The CO2 uptake factor of 5.0tCO2 ha−1y−1 was chosen for
PUHaccordingtotheresultsofCeschiaetal.(2010),who
evalu-ated,throughtheeddycovariancetechnique,thegreenhousegas
budgetsof15cropsitesacrossEurope,coveringalargeclimatic
gradientandawiderangeofagriculturalmanagementpractices.
ForthePUWweappliedaCO2uptakefactorof14.7tCO2ha−1y−1
according to Sofo et al. (2005), who evaluated the dry matter
accumulation and partitioning in the different plant organs of
Mediterranean orchards, and for the PUF, we applied the CO2
uptakefactorof13.2tCO2ha−1y−1measuredbytheeddy
covari-ancetowerinstalledontheLeccetoMediterraneanforest.
2.5. Urbantransect
Anurbantransectof6kminlengthwasdefinedfromFlorence
citycentertotheeasternperi-urbanarea,formedby6sectionsof
1kminlengthand0.5kmwidth,toassessthespatialvariability
ofsomelandscapemetricsindicesandcomparewithCO2
emis-sions(Fig.1).Thedirectionofthetransectwaschosenbecauseitis
representativeoftheaveragedistributionofthelandcoverclasses
foundintheMunicipality(datanotshown).Thefirstsection(T1)
wassetinthecitycenterclosetotheXimenianoObservatoryand
thelastsection(T6)intheperi-urbanarea.Foreachsection,3
land-scapemetricindiceshavebeendetermined,classifyingthelanduse
in8classes:urbanized(built-up,residential);urbaninfrastructure
(streets,communication/utilities,railwaystations,cemeteries)and
thepreviouslydefinedtypesofurbangreenspaces(UGMF,UGO,
UGSP,UTMF,UTO,UTSP).Theindices,determinedineachsection
ofthetransect,are:thePlandindex(Pland),indicatingthearea
percentageofeachlandusetypewithrespecttototal area;the
Shannon’sevennessindex(SHEI),indicatingthedegreeofevenness
amongpatchtypes;thepatchrelativedensity(PRD),indicatingthe
numberofpatchesineachsection.
3. Results
3.1. CO2uptake
The total urban green spaces of the Municipality of
Flor-enceuptake 72.5(±18.2)ktCO2y−1;ofthese,13.5ktCO2y−1 are
taken up by the UG (UGMF+UGO), 58.7ktCO2y−1 by the PU
(PUH+PUW+PUF); and 0.3ktCO2y−1 by the UT (UTMF+UTO).
-50 0 50 100 150 200 250 kt CO 2 uptakes emissions -5 0 5 10 15 20 25 30 1 2 3 4 5 6 7 8 9 10 11 12 %
Month of the year
offset capacity
A
B
Fig.4. (A)MonthlyCO2anthropogenicemissions(blackline)andurbangreen spacesuptakes(grayline)errorsbarsrepresent95%confidenceintervalsofthe aver-ages;(B)Monthlyoffsettcapacity(absolutepercentagevalue)oftheurbangreen spaceswithrespecttoCO2emissions.
Almost80%ofthetotalCO2 uptakebytheurbangreenspacesis
duetothePUareas,witha predominantcontributionfromthe
orchards,olivetreesandgrapevinesonthehillsaroundthecity.
FortemporaldisaggregationoftheCO2uptakeweusedtheCO2
fluxmeasurementsmeasuredattheLeccetosite(Fig.4).Ona
sea-sonalbasis,theLeccetoforestisahighercarbonsinkduringspring
andearlysummer,while itbecomesa net,smallcarbon source
duringmid-summer.Thisseasonalpatternisknowntobetypical
ofmostMediterraneanecosystemsthatarewaterlimitedduring
thesummerandonaverageabout83%oftheannualcarbonuptake
oftheLeccetoforestoccursfromJanuarytoJune.
3.2. CO2emissions
Florence’sdirectCO2emissionshavebeencomputedbymeans
oftwoinformationsources:theIRSEinventorialyearlyemission
databasespatiallydisaggregatedat1km2resolutionandtheeddy
fluxsitelocatedinthecitycenter.Eddycovariancedatahavebeen
usedintwoways:(i)todirectlyvalidateIRSEinventorialdataat
thelocationofthetower;(ii)toprovideatemporalemission
pat-ternatmonthlyscale,whichcanbeappliedtoyearlyinventorial
datatoobtaina monthlyemission trend.Wefoundarelatively
goodagreementbetweentheCO2emissionsmeasuredattheurban
fluxtower(309±42tCO2ha−1y−1),andthecorrespondingpixel
extractedbytheIRSE(255tCO2ha−1y−1),thatjustifiesusingIRSE
dataontheentireMunicipalityofFlorence,revealingatotaldirect
anthropogenicCO2emissionof1161.5(±136)ktCO2y−1.The
sea-sonalpatternofdirectCO2emissionsmeasuredattheXimeniano
Observatorywasusedfortemporaldisaggregationofthe
invento-rialestimates,demonstratingthatthemonthlydirectemissionsof
thecityarehighestduringthewinter(DecemberandJanuary)and
lowestduringsummer(JulyandAugust),accordingtodomestic
Fig.5.Theurbantransectfromurbantorurallandscape.Foreachsectionsthepiechart.representthePlandIndex,wherethegreenisthepercentageofurbangreenspaces andthegrayisthepercentageoftheurbanizedareas.Plandindexwasreferredtothesectionsurfaceequalto0.5km2.
3.3. CO2balance
Withina carbonbalanceperspective, thetotal sinkofurban
greenspacesoftheMunicipalityofFlorenceoffset6.2%ofthetotal
directanthropogenicCO2 emissions.Ofthis,1.1%ismadebythe
UGand5.1%bythePU.WhenincludingtheFlorenceMasterPlan
scenariointhebalancecomputation,theoffsetcapacityofurban
greenspacesgrowsto6.4%.Thetimedisaggregationonamonthly
scale(Fig.4),revealsthattheurbangreenspacesaremoreefficient
inoffsettingthedirectanthropogenicCO2emissionsduringMarch
(11.2%),April(23.3%),May(16.3%)andJune(26.2%),asthesearethe
mostproductivemonthsassociatedtorelativelylowanthropogenic
emissions.
3.4. Urbantransect
ThePlandindexrevealsaclearpatternofthelevelof
urbaniza-tionofthecity:T1andT2havethehigherpercentageofurbanized
area,onaveragemorethan50%;T3andT4haveapproximatelythe
samepercentageofurbanizedandurbangreenspaces;whileinT5
andT6,thepercentageofurbanizedareaislessthan10%(Fig.5).
SHEIindexhasalmostthesamevaluealongtheurbantransect,
andconsideringthatitrangesfrom0(completelyunevenlandscape
distribution)to1(completelyeven),everypatchclassabundance
isofthesamemagnitude(Fig.6A).Thesectionoftheurbantransect
thatshowsthelowestvalueoftheSHEIindexisT1,whiletheone
withthehighestvalueisT5.
Thepatchrelativedensity(PRD),whichisanindicatorof
land-scapefragmentation,exhibits.
A positive correlation (r=0.89) with total CO2 emissions
(Fig. 6B), and negative correlation (r=−0.85) with CO2 uptake
(Fig.6C).PRDvaluesarehigherincorrespondancetothesectors
closertothecitycenter(T1andT2),while theyarenot
signifi-cantlyaffectedbytheforecastinterventionsplannedintheFlorence
MasterPlan(Fig.6C).
4. Discussions
The total annual CO2 uptake by the urban green spaces of
theentireMunicipalityofFlorenceoffsets6.2%ofthetotaldirect
anthropogenicCO2 emissions.Thisisquitehigh,withrespectto
otherurbanareas.Escobedo,Varela,Zhao,Wagner,andZipperer
(2010),usedfieldmodeledandspatialdataonurbantreesto
ana-lyzetheCO2sequesteredbytreescomparedtothetotalemissions
oftwosubtropicalAmericancities,GainesvilleandMiami-Dade,
withtheresultthattheurbantreesoffsetonly3.4%and1.8%.The
highervalueofFlorenceisduetoacombinationoftwofactors:(i)
weconsideronlythedirectemissionstotheatmosphereinstead
oftotal;(ii)thedistributionoftheurbangreenspaces,the
major-ityofwhicharelocatedinthePUarea.Infact,ifwecomputethe
offsettingcapacitynotconsideringthePUcontributionweobtain
avalueof1.1%.Theseresultspointoutthatparticularattention
mustbetaken inurbanplanningtopreservePUCO2 offsetting
capacity,alsobecausenewlybuiltareaswilloccupyPUsurfaces,
asindicatedbytheFlorenceMasterPlan.Thisfollowsan
urbaniza-tionmodelfoundalsoinRome(Salvati,Munafo,GargiuloMorelli,
&Sabbi,2012),whichhasevolvedinthelastdecades,froma
“com-pactgrowthmodel”toa“dispersemodel”(Schneider&Woodcock,
2008).
TheapplicationoftheIPCCmethodologytoestimatethe
mag-nitudeof CO2 uptake enablestherole ofurbangreen spacesin
theurbancarbonbalancetobequantified.ThemeanannualCO2
uptakeforurbanlawnsusedinthisstudyiscomparablein
magni-tudetothatindicatedbyConant,Paustian,andElliott(2001)and
QianandFollett(2002),whoestimatedthatlawnshaveapotential
CO2 uptakerateof3.6tCO2ha−1y−1anditisalsocomparableto
theuptakefactorspublishedbyJoandMcPherson(1995).
The mean CO2 uptake factor per tree appliedin this study
(26kgCO2tree−1y−1)iscomparablewiththefindingsofNowakand
Crane(2002),whoreportedaCO2uptakefactorrangingfrom12.2
to21.2kgCO2tree−1y−1.Moreoverinarecentstudydoneonthe
CascinePark,thelargestgreenareainFlorencethatcovers118ha,
usingtheUFOREmodel, ameanannual uptakefactor hasbeen
determinedof33.8kgCO2tree−1y−1(Paolettietal.,2011).TheDBH
datausedinourstudy,providedbytheMunicipalityofFlorence,
allowedtoustoruleouttheeffectoftheinter-annualvariability
oftreegrowth.Infact,eveniftheexactdatesoftheDBHdata
sam-plingsarenotknown,ourcalculationsarebasedonalargenumber
ofsamplestakenduringeachyearfrom2006to2011,withmore
than9800DBHmeasurementsperyearonaverage.
Thetemporaldisaggregationoftheemissionsanduptakesof
thecity(Fig.4)representsanewlevelofinformationthatmaybe
usedtoestimatetheefficacyofinterventionsandpoliciesaimedat
reducingCO2emissionsandenhancingCO2uptakes.Themaximum
efficiencyofurbangreenspacestooffsetemissionsisduringspring
anditisverylowduringwinterandsummermonths.Theinefficacy
ofthegreenspacesduringthesetwoseasonsisrelated:forthe
wintermonths,tohighCO2emissionsduetothedomesticheating
andthelowerairtemperaturethatlimitsplantcarbonuptake,and
forthesummerperiod,tolackofwaterandhighairtemperatures
thatinhibitcarbonuptake,eventhoughtheCO2emissionsduring
summerarelowerthaninotherseasonsoftheyear.Withinthis
perspective,policiesaimedatdecreasingCO2emissionsinwinter
monthswillbemoreefficientthanthoseaimedatincreasingCO2
uptake,whichstillremaincontrolledbyenvironmentalfactorssuch
asairtemperatureandprecipitation.
Weextractedasub-setofourCO2balanceresultsonanurban
transect taking into account a recent application of the
tran-secttheorydeveloped byurbandesignersnamed “SmartCode”
(www.smartcodecentral.org).Thishasrecentlybeenadoptedasthe
cornerstoneofarenewedsustainabledesignvariouslyaddressed
Fig.6. (A)Shannon’sevennessindex(SHEI)calculatedforeachsectionsoftheurban transectconsideringtheactualpatchesdistribution(SHEI,grayssymbols)andthe patchesdistributionifalltheinterventionsforecastbyMasterPlanwillbedone (SHEI+PS,blacksymbols).(B)Actualpatchrichnessindex(PRD)graybars,andthe totalCO2emissions(tCO2y−1)blacksymbols,foreachsectionsoftheurbantransect. (C)ActualPRDindexgraybars,andfuturePRDindex(PRD+PS,whitebars)with thenewpatchesoftheMasterPlanandtheactualCO2uptake(tCO2y−1)(Uptakes, blacksymbols),andthefutureCO2uptake(tCO2y−1)(Uptakes+PS,graysymbols anddottedline).
GrowthManual(Duany,Speck,&Lydon,2009),Landscape
Urban-ism (Waldheim, 2006), New Urbanism (Katz, 1994); Ecological
Urbanism(Mostafavi&Doherty,2010)andSustainableUrbanism
(Farr,2007).TheanalysisofFlorence’surbantransectrepresents
an attempt to merge a landscape analysis with a quantitative
carbonbalanceanalysis.SHEIindexalong thedifferentsections
indicatesthatthecitycenterisunbalancedcomparedtotheT5,
whichexhibitsthebestperformanceswithhighestSHEIindex.The
FlorenceMasterPlanwillenhancetheSHEIindexinmostofthe
sec-tions,contributingtobalancethedistributionofclasspatchesinthe
urbantransect(Fig.6A).Thefragmentationofpatchesinthe
vari-oussectionsshowsagoodagreementwiththetotalCO2emissions
y = 0.098x + 34.461 R = 0.77 y = 0.0177x + 73.985 R = 0.03 0 100 200 300 400 500 600 700 0 20 40 60 80 100 120 0 100 200 300 400 500 600 700 800
Number of tree per section (n°)
Urban green area per section (%)
CO2 uptakes (tCO2 y-1) per section
Urban green area Tree y = 0.1055x + 31.551 R = 0.81 y = -0.2776x + 300.73 R = 0.16 0 100 200 300 400 500 600 700 0 20 40 60 80 100 120 0 100 200 300 400 500 600 700 800
Number of tree per section (n°)
Urban green area per section (%)
CO2 uptakes (tCO2 y-1) per section
Urban green area + UPS Tree + UPS y = 0.0068x - 8.4953 R = 0.91 0 10 20 30 40 50 60 70 80 0 2000 4000 6000 8000 10000 12000 14000
Urbanized area per section (%)
CO2 emissions (tCO2 y-1) per section
C
A
B
Fig.7.Directcarbondioxideemissionsanduptakepersectionoftheurbantransect. (A)Actualurbangreenspaces(blacksymbolsandline),vsactualCO2uptakes(tCO2 y−1)onleftaxisandactualtotalnumberofurbantrees(opensymbols,dottedline); (B)ForecasturbangreenspacesassumoftheactualandforecastareaoftheMaster Plan(blacksymbolsandline),vsforecastCO2uptake(tCO2y−1)onleftaxisand forecasttotalnumberofurbantreesassumofUTMF,UTOandUTPS(opensymbols, dottedline);C)Urbanizedareapersection(graysymbolsandblackline)vsthedirect carbondioxideemissions(tCO2y−1).
(Fig.6B),confirmingthatthisfragmentationisrelatedtotheCO2
emissions,probablythroughthepercentageofbuilt-upareas.The
relationsreportedinFig.7A–CbetweenCO2uptake/emissionand
green/urbanizedareasrepresentaninnovativeapproachtomerge
alandscapeanalysiswithaquantitativeenvironmentalanalysis,
capableofevaluatingtheefficacyoftheFlorenceMasterPlan,and
thatcouldbeappliedinotherurbanareasofthecity.
Therelationsbetweenthesumofthepercentageof
continu-ousgreenareas(sumofthecategoriesUGMF,UGO,PUH,PUWand
PUF)andthetotalCO2uptakebyeachsectionoftheurban
tran-sectforboththeexisting(Fig.7A;R2=0.77)andfuturegreenarea,
accordingtotheFlorenceMasterPlan(Fig.7B;R2=0.81),clearly
demonstratethatthemaindriverfortheCO2uptakeineachsector
isrepresentedbythecontinuousgreenareasinsteadofthetotal
numberoftrees(Fig.7A;R2=0.03andFig.7B;R2=0.16).Moreover,
thecorrelationbetweenthetotalurbanizedarea,definedhereas
thesumofthepatchesclassifiedasurbanized(built-up,
residen-tial),urbaninfrastructure(streets,railwaystationsandcemeteries)
andthetotalCO2 emissions(tCO2y−1)foreachsection(Fig.7C;
R2=0.91),demonstratesthatthepercentageofurbanizedareain
eachsectoristhemaindriverfortheCO2emissions.
5. Conclusions
Thereisageneralneedtoincreaseknowledgeabouttheroleof
urbangreenspacesinoffsettingGHGemissions,inparticularwith
thedirectmeasurementsofcarbonuptakeandemissioninurban
environments,asrecentlypointedoutbyPatakietal.(2011).The
approachappliedinthisstudyisa combinationofeddy
covari-anceobservationsinurbanandnaturalenvironments,inventorial
emissiondataandcarbonstockassessmentmethodsprovidedby
IPCC(2003,2006)thatmighteasilybeappliedinothercities.The
totalCO2emissionsoffsettingcapacityoftheurbangreenspaces
oftheMunicipalityofFlorence,excludingthecontributionofthe
PUareas,isverylow(1.1%).Withinacarbonbalanceperspective,
insteadofincrementingtheefficacyofurbangreenspacesto
bal-anceCO2emissions,theimplementationofmeasuresforreducing
theCO2emissionscouldprovidebetterresults.Moreoverour
cal-culationsonlyconcernthedirectCO2emissions,andifconsidering
alsoindirectemissionsinafullcarbonbalanceperspectivethe
off-settingcapacitywouldbeevenlower.TooffsetthetotaldirectCO2
emissionsofthecitymorethan880km2ofnaturalforestwould
benecessarywiththesameecophysiologicalcharacteristicsasthe
LeccetoMediterraneanforest,correspondingtoapproximately8
timestheentiresurfaceareaoftheMunicipality.Thisfactmight
encouragere-thinkingtheroleofurbangreen spaces,thathave
alotofbeneficialeffects,suchasreducingtheurbanheatisland,
reducingairpollution,particulatesandgases,filteringnoiseand
enhancingthewell-beingofthecitizenswholiveclosetothegreen
areas.QuantificationoftheCO2uptakebyurbangreenspacesmight
beusefultotheurbanplannerformanagingthe“freecityspace”
concept(Odum,1971),definedasspaceintheurbanterritory
cov-eredbygreen.Theargumentsofthisworkmightofferscientific
supporttothoseurbanpoliciesaimedatlimitingthedemandfor
land,ontheonehand,andcontainingthedensificationofsuburbs,
ontheother.Theurbangreenspaceshaveseveraldifferentroles,
includingtheoffsettingcapacityofanthropogenicCO2emissions
analyzedinthisstudy,thatshouldbecarefullyconsideredbyurban
plannersanddesignerstoeffectivelycontributetothedevelopment
ofasustainableurbandesign.
Acknowledgements
The authors would like to acknowledge the contributions
of:AlessandroMatese,FrancescoSabatiniandAlessandroZaldei
(IBIMET-CNR),fortheirvaluabletechnicalassistanceinthe
man-agement of the eddy covariance flux towers. Ramona Magno
(ConsorzioLaMMA)isacknowledgedforprovidingtheIRSE
Inven-tory data. A special thanks to: Emilio Borchi and Renzo Macii
of the Fondazione Osservatorio Ximeniano (Fi); Emanuela Lupi
and Marisa Sabbia of the Municipality of Florence; the
Lab-oratory on Climate, Sustainability and Security Infrastructure
(CEST)forproviding somefundamentalinstrumentsinstalledin
theurbanflux tower.Thispapercontributes toBRIDGEProject
(www.bridge-fp7.eu), fundedbytheEuropeanCommission.The
authorswouldliketothanktheanonymousreviewersfortheir
valuablecommentsandsuggestionstoimprovethequalityofthe
paper.
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Perrone(1970),Architect,PhDonUrban,LandscapeandEnvironmentalDesign (2002),iscurrentlyassistantprofessoronUrbanandRegionalPlanningat Depart-ment of Urban and Regional Planning–University of Florence. She has just concludedasemesterasvisitingprofessor(fullposition)onUrbanandRegional PlanningandParticipatoryPlanning,atInstituteofGeography(Geographisches Institut)–UniversityofTübingen.Shecollaborateswithsomeinternationalresearch networks,suchasAesop(AssociationofEuropeanSchoolsofPlanning)withinwhich sheisnational(Italy)representative(asalternatemember).Shehaspublished numerousacademicarticlesandhascontributedchapterstoseveralpublications onurbanpoliciesformanagingdiversity,urbanandregionalplanningwithregard tolandconsumptioncontainment,urban-ruralfringere-design,publicspace re-design,localdevelopmentpoliciesandplanningtools,participatoryplanning.
Vaccari(1967),AgriculturalSciencedegreein1994,PhDinEcologyand Envi-ronmentalSystems.ResearchscientistattheInstituteofBiometeorologyNational ResearchCouncil,since2002.Scientificinterestsandhighlights:EffectsofhighCO2 oncropsandnaturalecosystems;Biosphereatmosphereinteractions;Urbancarbon fluxes;Precisionagriculture;Biochar.Hehas36peerreviewedpapers,h-index=11.
Gioli(1971),EnvironmentalEngineeringdegreein1998.PhDinEcologyand Envi-ronmentalSystems.AdvancedresearchscientistattheInstituteofBiometeorology NationalResearchCouncil,since2004.Majorscientificresults:Developmentand extensivevalidationoftheaircraftfluxmeasurementsmethodology;Development ofupscalemethodstoderiveregionalscalecarbonbalance;Usingregionalfluxes asavalidationtollforatmosphericandecosystemmodeling:Studyofinteractions betweensurfaceandPBLfluxes.Hehas36peerreviewedpapers,h-index=11.
Toscano(1980),Sciencesandtechnology(OceanographyandMeteorology)degree in2005.MasterinAppliedMeteorologyin2006.PhDstudentinEcologyand EnvironmentalSystems.Excellentexperiencegainedduringmanynationaland internationalcampaign,planningandoperatingdataacquisitionofresearch air-craftthathadtobeoperatedinsynergywithseveralotheraircraftsandextensive groundactivities(atmosphericmeasurements,carbondioxidefluxes,boundary layercharacterization,environmentalpollutionsampling,remotesensing). Excel-lent experience gained during nationaland internationalshipboard missions (morpho-bathymetry,biostratigraphy,oceanographicsampling,carbondioxideand acetoneair-seafluxesmeasurements).Experienceinremotesensingtechniques, instrumentsandapplicationswithopticaldatagainedinthelastfiveyearsofwork experience.Experienceonsatellitedataproducts,processingandfinalapplications. Managementofmeteorologicalandmicro-meteorologicalinstrumentations,data acquisition,analysisanddataprocessing.Cropmodeling,experimentaland mod-elingdurumwheatgrowthstages,qualityandvulnerabledevelopmentalstages. Currentposition:ResearchscientistattheInstituteofBiometeorologyNational ResearchCouncil.Hehas9peerreviewedpapers,h-index=4.