MEASUREMENT,COMPARISON,ANDUSEOFREMOTELY DERIVEDLEAFAREAINDEXPREDICTORS By RYANR.JENSEN ADISSERTATIONPRESENTEDTOTHEGRADUATESCHOOL OFTHEUNIVERSITYOFFLORIDAINPARTIALFULFULLMENT OFTHEREQUIREMENTSFORTHEDEGREEOF DOCTOROFPHILOSOPHY UNIVERSITYOFFLORIDA 2000 ACKNOWLEDGMENTS Adissertationisnevertheresultofoneperson’sefforts. Rather,itisthe culminationofmanypeopleworkingtogetherforacommongoal. Iwishtothankmy committeemembers,PeterWaylen,NigelSmith,andFrancisPutzforteachingmehow toconductresearchandwriteadissertation. Iwouldespeciallyliketothankmy committeechair,MichaelBinford,forprovidingmewiththeguidance,freedom,and knowledgetocompletethisdissertation. Myfamilyhasbeeninstrumentalinallowingmetocompletethiswork. Mywife, Tricia,andmytwodaughters.SavannahandSierra,havesufferedpatientlythroughmany dayswhendadwaseitherawaydoingfieldwork,orworse,typingonthecomputerinour livingroom. Thankyougirls! Iwouldalsoliketothankmyfather,JohnJensen,for reviewingthisworkmanytimes. Finally,Iwouldliketothanktheofficestaffandmy fellowgraduatestudentsfortheirsupport. 11 TABLEOFCONTENTS page ACKNOWLEDGEMENTS ii ABSTRACT v CHAPTERS 1 INTRODUCTION 1 2 STUDYAREA 9 LongleafPine/TurkeyOakSandhills ,9 SandPineScrub ,13 Hammocks ,14 OtherNorthFloridaCommunities 15 3 BACKGROUNDANDLITERATUREREVIEW 16 BiophysicalRationale ,16 RemoteSensingofVegetation 16 LeafAreaIndex 24 VegetationIndices 26 LAIandRemoteSensingVegetationIndices 29 ArtificialNeuralNetworks 30 NetworkArchitecture 33 NetworkTraining 35 NeuralNetworksandRemoteSensing 37 SatelliteImagery 38 4 METHODS 40 Goals 40 Hypotheses 40 Methods 42 FieldLAIMeasurements .42 BrightnessValueExtraction .43 MultipleRegressionofSixTMSpectralBands .43 VegetationIndicesandLAI. .44 ArtificialNeuralNetworkandLAI 44 OverallAccuracy 44 5 RESULTS 46 RegressionAnalyses .46 Hi ArtificialNeuralNetwork .59 OverallAccuracy 70 Discussion 75 6 ECOLGOGICALSTUDIES 77 LeafAreaIndex,Fire,andSuccessionin LongleafPine/TurkeyOakSandhills. 79 ComparisonsoftheUrbanForestsinGainesvilleandOcala,FL 92 6 DISCUSSIONANDCONCLUSION 106 Discussion 106 OtherSensors 108 Conclusions 110 FutureResearch 114 APPENDICES A COMPUTATIONOFLOCALTASSELEDCAPCOEFFICIENTS 112 B GISPROGRAMUSEDTOINTERPOLATEBRIGHTNESSVALUES 115 C CREATIONOFLAISURFACEIMAGESUSINGANNS 121 REFERENCES 122 BIOGRAPHICALSKETCH 133 IV AbstractofDissertationPresentedtotheGraduateSchool oftheUniversityofFloridainPartialFulfillmentofthe RequirementsfortheDegreeofDoctorofPhilosophy MEASUREMENTANDCOMPARISONOFREMOTELY DERIVEDLEAFAREAINDEXPREDICTORS INNORTHCENTRALFLORIDA By RyanR.Jensen May2000 Chair:MichaelW.Binford MajorDepartment:Geography Environmentalchangeoccursinresponsetobothnaturalandanthropogenic causes. Astheworld’shumanpopulationcontinuestoincrease,anthropogenicchange willalsoincrease. Thesechangesaffectthehealthandvigorofforeststhroughoutthe world,includingthoseinnorthcentralFlorida. LeafAreaIndex(LAI),theamountof leafareaperunitgroundarea,isanimportantbiophysicalvariablethatisdirectlyrelated toratesofatmosphericgasexchange,biomasspartitioning,andproductivity. While globalandlocalmodelsthatmapbiophysicalparametersareprevalentintheliterature, landscapetoregionalscalemodelsarelesscommon. Therefore,theabilitytomapand monitorLAIoverlandscapetoregionalscaleareasisessentialforunderstandingmedium scalebiophysicalpropertiesandhowthesepropertiesaffectbiogeochemicalcycling, biomassaccumulation,andprimaryproductivity. Thisstudydevelopsandverifies severalnewmodelstoestimateLAIusinginsitufieldmeasurementsthroughoutnorth centralFlorida,LandsatThematicMapperremotelysensedimagery,remotelyderived vegetationindices,simpleandmultipleregression,andartificialneuralnetworks (ANNs). Thisstudyconcludesthatwhilemultiplebandregressionandregressionwith V individualvegetationindices(NormalizedDifferenceVegetationIndex,SoilAdjusted VegetationIndex,SimpleRatio,andGreennessVegetationIndex)canestimateLAI,the mostaccuratewaytoestimateregionalscaleLAIistotrainanANNusinginsituLAI dataandremotesensingbrightnessvaluesmeasuredfromsixdifferentportionsofthe electromagneticspectrum. ThenewANNmethodofestimatingLAIisthenappliedtotwoforestecology studies. ThefirststudyanalyzesLAIinlongleafpine/turkeyoaksandhillsasafunction oftimesincelastbum. Itconcludesthatintheabsenceoffire,sandhillLAIincreases, andthismaybeusefulforidentifyingwhereprescribedbumsneedtobedone. The secondstudyestimatesandcomparesurbanforestLAIinOcalaandGainesville,Florida asafunctionofexistingtreeordinancesinthetwocities. ItconcludesthatGainesville’s urbanforesthashigherLAIvaluesprincipallybecauseofaverystricttreeordinance. VI CHAPTER 1 INTRODUCTION Environmentalchangeoccursinresponsetobothnaturalandanthropogenic events. Naturaleventsincludemigrationofcontinents,buildinganderosionof continents,sealevelchange,theElNino-southemoscillation,hurricanes,tornados,fire, landslides,variationsofsolarintensity,andevenmeteorstrikes. Anthropogenicevents includelandcover/landuseconversion,increasedcarbondioxideemissionthroughfossil fuelburningandlandconversion,andfiresuppression(CurranandFoody,1994). Asthe world’shumanpopulationcontinuestogrow,human-inducedenvironmentalchangewill increase. Theseeventsareoftenwellstudiedatthelocalscalewhereobservationand contemplationhaveoccurredformillenniaandattheglobalscalewheresignificant amountsofresearchhavebeendonesincetheearly1960s. However,thisunderstanding rarelyextendstothelandscapeandregionalscalesasitisbasedonlimitedresearchand lacksrobustmodelsandrelevantdata(CurranandFoody,1994). Knowledgeof biophysicalcharacteristicsofvegetationatthelandscapeandregionalscalesisnecessary todescribeenergyandmassfluxesattheEarth’ssurfaceusingglobalcirculationmodels, carboncyclemodels,andwatermodels(WeissandBaret,1999). Theneedforsuch knowledgeisnowaccepted(IGBP,1990)andmodelsmustbedevelopedthatincorporate regionalscalemodels(Curran,1994). Manyoftheecologicalquestionsconcerningtherelationshipbetweenboth naturalandanthropogeniceffectsontheenvironmentrequireaccurateestimatesof biophysicalvariables. Biophysicalvariablesincludeecosystemcharacteristicssuchas 1 2 primaryproduction,totalplantbiomass,componentsofthenitrogencycle,and evapotranspirationratesthatdescribeecosystempropertiesandfunctions(Aberand Melillo,1991). AbiophysicalvariableofprincipalimportanceisLeafAreaIndex(LAI) definedasm^ofleafperm^ofground(Curran,1994;PierceandRunning,1998; Lymbumer,L,P.J.BeggsandC.R.Jacobson.,2000). Leavesrepresentthefundamental photosyntheticorganoftreesandotherplants. Inputstoleavesincludeshort-andlong- wavelengthradiation,water,andnutrientsfromthesoil. Outputsincludelong- wavelengthradiation,conductionandconvection,transmissionoflight,transpiration, reflectance,andenergystoredincarboncompounds(sugars)forexporttotheremainder oftheplant(AberandMelillo,1991). Becauseleavesaretheprimaryorgansforcanopy- atmospheregasexchange,LAIisakeyvariableinatmosphericcirculationmodels (Ruimy,A.,B.Saugier,G.Dedieu,1994). Leavesfixcarbondioxide(CO2)during photosynthesis,andreleaseCO2duringrespiration. Thebalancebetweenthetwois knownasnetcarbonfixationandwhenextrapolatedatthelandscapescalethishelpsto explainlarge-scalecarbondynamics. Oneimportantwaythatbiophysicalvariables,such asLAI,aremeasuredatthelandscapescaleisthroughremotesensing. Satelliteremotesensing,definedasthemeasurementandanalysisofearth phenomenafromspace,hasbeenusedinmanyvegetationstudies(e.g.,Bonan,1993; Curran,1994;Gong,Ruiliang,andYu,1997). Remotelysenseddatafromsatellites possessavarietyofattributesusefulforlarge-scalevegetationmapping. Forexample, satelliteremotesensingdataprovideasynopticviewoflandscape-toregional-scaleareas andarecollecteduniformlyinspaceandtimeinanondestructivemanner(Green, Mumby,Edwards,Clark,andEllis,1997;FriedlandBrodley,1997). Satelliteremote 3 sensingcancontinuouslymonitortheearth’ssurfacethroughorbitingplatformsthat containsensors,whichmeasureemittedorreflectedenergy(AberandMelillo,1991). Despiteitsimportance,knowledgeofandabilitytomeasurelandscape-scale*LAI usingremotelysenseddataislimitedbecause: (i) CurrentmethodsofinsituLAImeasurementarelaborintensive,makingit difficulttomeasurethroughoutlargegeographicareas,renderinguseofthese methodsbeyondthestandlevelimpractical(Fassnacht,Gower,MacKenzie, Nordheim,andLillesand,1997). (ii) Adequatespatialandtemporalsamplingisdifficulttoachieveusingground measurementtechniquestomonitorlandscapescaleLAI(WeissandBaret,1999). (Hi) Present-dayfieldLAIdataaredifficulttorelatetohistoricalremotesensordata becauseforestschangeoverthetimeelapsedbetweensceneacquisitionandLAI measurement.(LillesandandKeifer,1996;Jensen,2000). (iv) StandardmethodsforestimatingLAIfromsatelliteremotesensingdataare inadequateacrosstherangeofLAIbecausesomestudieshavefoundathreshold LAIvalueof2-4wherecommonlyusedvegetationindicesfailtoincreasein relationtoincreasedLAIvalues(e.g.,theNormalizedDifferenceVegetation Index(Figure1-1;CarlsonandRipley,1997;Datt,1998;LawrenceandRipple, 1997). Interception,scattering,andemissionofelectromagneticradiationbyleavesare closelyrelatedtoforestcanopystructure(Mather,1987). IfthespatialaspectsofLAI TurnerandGardner(1991)definelandscapeasthelandformsorecosystemsofaregionintheaggregate, ortothelandsurfaceanditsassociatedhabitatsatscalesofhectarestomanysquarekilometers. 4 0.8 0.7 0.6 0.5 NDVI 0.4 0.3 0.2 0.1 0 Figure1-1.Leaf-Area-Index(LAI)saturationinrelationtotheNormalizedDifference VegetationIndex(adaptedfromCarlsonandRipley,1997).