075_PVPowerOutputVariabilityCorrelationCoefficients
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Transcript of 075_PVPowerOutputVariabilityCorrelationCoefficients
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Copyright2010CleanPowerResearch 1
PVPowerOutputVariability:CorrelationCoefficients
ThomasE.HoffandRichardPerez
CleanPowerResearch
www.cleanpower.com
Draft,November11,2010
AbstractUtilityplannersandoperatorsareresponsibleforguidingwherePVsystemsarelocatedandare
accountableforsystemreliability.TheyareconcernedabouthowshorttermPVsystemoutputchanges
mayaffectutilitysystemstability.Thatis,theyareconcernedaboutPVpoweroutputvariability.
Thispaperintroducesanovelapproachtoestimatethemaximumshorttermoutputvariabilitythata
fleetofPVsystemsplacesonanyconsideredpowergrid.Akeyinputtothisapproachisthecorrelation,
orabsencethereof,existingbetweenindividualinstallationsinthefleetattheconsideredvariability
timescale.
ShorttermPVpoweroutputvariabilityisdrivenbychangesintheclearnessindex.Thus,thepaper
focusesonanalyzingthecorrelationcoefficientofthechangeintheclearnessindexbetweentwo
locationsasafunctionofdistance,timeinterval,andotherparameters. Thepaperpresentsamethod
toestimatecorrelationcoefficientsthatuseslocationspecificinputparameters.Themethodappearsto
becapableofdescribingsitepaircorrelationacrosstimeintervalsfromsecondstohours.
Themethodisderivedempiricallyandvalidatedusing12yearsofhourlysatellitederiveddatafrom
SolarAnywhereinthreegeographicregionsintheUnitedStates(Southwest,SouthernGreatPlains,and
Hawaii).Resultsattimeintervalslessthanonehourarecorroboratedusingfindingsfromrecent
investigationsthatwerebasedon10secondtooneminutedatasets.
Thestrengthandstructureofthemethodissummarizedbythreefundamentalfindingsthatboth
confirmandextendconclusionsfrompreviousstudies:
1. Correlationcoefficientsdecreasepredictablywithincreasingdistance.2. Correlationcoefficientsdecreaseatasimilarratewhenevaluatedversusdistancedividedbytheconsideredvariabilitytimeinterval.3. Theaccuracyofresultsisimprovedbyincludinganimpliedcloudspeedterm.
ThepresentapproachhaspotentialfinancialbenefitstosystemsthatareconcernedaboutPVpower
outputvariability,rangingfromdistributionfeederstobalancingregions.
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IntroductionPVcapacityisincreasingonutilitysystems.Asaresult,utilityplannersandoperatorsaregrowingmore
concernedaboutpotentialimpactsofpowersupplyvariabilitycausedbytransientclouds.Utilitiesand
controlsystemoperatorsneedtoadapttheirplanning,scheduling,andoperatingstrategiesto
accommodatethisvariabilitywhileatthesametimemaintainingexistingstandardsofreliability.
Itisimpossibletoeffectivelymanagethesesystems,however,withoutaclearunderstandingofPV
outputvariabilityorthemethodstoquantifyit.Whetherforecastingloadsandschedulingcapacity
severalhoursaheadorplanningforreserveresourcesyearsintothefuture,theindustryneedstobe
abletoquantifyexpectedoutputvariabilityforfleetsofuptohundredsofthousandsofPVsystems
spreadacrosslargegeographicalterritories.Underestimatingreserverequirementsmayresultina
failuretomeetreliabilitystandardsandanunstablepowersystem.Overestimatingreserve
requirementsmayresultinanunnecessaryexpenditureofcapitalandhigheroperatingcosts.
ThepresentobjectiveistodevelopanalyticalmethodsandtoolstoquantifyPVfleetoutputvariability.
Variabilityintimeintervalsrangingfromafewsecondstoafewminutesisofprimaryinterestsincecontrolareareservesaredispatchedoverthesetimeintervals.Forexample,regulationreservesmight
bedispatchedatanISOeveryfivesecondsthroughabroadcastsignal.KnowledgeaboutPVfleet
variabilityinfivesecondintervalscouldbeusedtodeterminetheresourcesnecessarytoprovide
frequencyregulationserviceinresponsetopowerfluctuations.
VariabilityofaPVfleetisthusameasureofthemagnitudeofchangesinitsaggregatepoweroutput
correspondingtothedefinedtimeintervalandtakenoverarepresentativestudyperiod.Notethatitis
thechangeinoutput,ratherthantheoutputitself,thatisdesired. Alsonotethat,foreachtimeinterval
thechangeinoutputmayvaryinbothmagnitudeandsign(positiveandnegative). Astatisticalmetricis
thereforeemployedinordertoquantifyvariability:thestandarddeviationofthechangeinfleetpower
output.
Itishelpfultographicallyillustratewhatismeantbyoutputvariability.TheleftsideofFigure1presents
10secondirradiancedata(PVpoweroutputisalmostdirectlyproportionaltoirradiance)andtheright
sideofthefigurepresentsthechangeinirradianceusinga10secondtimeintervalforanetworkof25
weathermonitoringstationsina400meterby400metergridlocatedatCordeliaJunction,CAon
November7,2010(HoffandNorris,2010).Thelightgraylinescorrespondtoirradianceandvariability
forasinglelocationandthedarkredlinescorrespondtoaverageirradiancedistributedacross25
locations.Resultssuggestthatspreadingcapacityacross25locationsratherthanconcentratingitata
singlelocationreducesvariabilitybymorethan70percentinthisparticularinstance.
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Figure1
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outputvariabilitytobethestandarddeviationofthechangeinoutputoversometimeinterval(suchas
oneminute),usingdatatakenfromsometimeperiod(suchasoneyear).
Thesimplifiedmodelcoveredthespecialcasewhenthechangeinoutputbetweenlocationsis
uncorrelated(i.e.,cloudimpactsatonesitearetoodistanttohavepredictableeffectsatanotherforthe
consideredtimescale),fleetcapacityisequallydistributed,andthevarianceateachlocationisthesame. Undertheseconditions,HoffandPerezshowedthatfleetoutputvariabilityequalstheoutput
variabilityatanyonelocationdividedbythesquarerootofthenumberoflocations:1
(1)
whereisthestandarddeviationofthechangeinoutputofthefleetusingatimeintervaloft, isthestandarddeviationofthechangeinoutputofthefleetconcentratedatasinglelocation,andNisthenumberofuncorrelatedlocations.
MillsandWiser(2010)havederivedasimilarresultthatrelatesvariabilitytothesquarerootofthe
numberofsystemswhenthelocationsareuncorrelated.
MaximumOutputVariabilityEquation(1)hasimportantimplicationsforutilityplanners.Itallowsthemtodeterminereserve
capacityrequirementstomitigateworstcasefleetvariability. Forexample,supposethatthevariability
ofasinglesystemwas10kWperminuteandtherewere100uncorrelatedidenticalsystemsinthefleet.
Totalfleetvariabilityequals0.1MW(
perminute. Theplannercouldthenapplythedesired
confidencelevel(e.g.,theymaychoose3standarddeviations)todeterminetherequiredreserve
capacity(e.g.,3x0.1MW=0.3MW).
Thiscalculationisapplicablewhentwofundamentalconditionsaresatisfied:(1)theoutputvariabilityat
asinglelocationcanbequantifiedand(2)thechangeinoutputvariabilitybetweenlocationsis
uncorrelated.
Considerthefirstcondition. Oneapproachtodeterminingsinglelocationvariability( )istoanalyze
historicalsolarresourcedataforthelocationofinterest.Thedatawouldneedtohavebeencollectedat
aratethataccommodatesthetimeintervalofinterest(perhapsdowntoafewseconds)overa
substantialandrepresentativeperiodoftime(perhapsoverseveralyears).Suchhighspeed,high
resolutiondataisnotgenerallyavailable.2
Analternativeapproachistoconstructadatasetthatsimulatesworstcasevariabilityconditions.The
theoreticallyworstcasevariabilityofasinglePVplantwouldbethatitcyclesalternatelybetween0and
100percentofitsratedoutputeverytimeinterval.Forexample,supposethatthePVplantisratedat1
1SeeEquation(8)inHoffandPerez(2010).2OneofthefewexamplesofthissortofdataisprovidedbyKuszamaul,et.al.(2010).
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MWandthetimeintervalofinterestis1minute.AsillustratedinTable1,maximumvariabilityoccurs
whenthePVplantisatfullpowerat12:00,zeropowerat12:01,fullpowerat12:02,etc.Asillustrated
intherightsideofthetable,thecorrespondingchangeinpowerfluctuatesbetween 1and1MW.The
standarddeviation3ofthechangeinpoweroutputequals1MWperminute.Thatis,a1MWPVplant
thatisexhibitingmaximumvariabilityovera1minutetimeintervalhasa1MWperminutestandard
deviation.Thiswouldimplythat1MWofreservecapacityisrequiredtocompensatefortheoutput
variabilityforasingleplant.
Table1.Maximumchangeinpoweroutputatonelocation.
Time Power(MW) Change(MW/min)
12:00 1 1
12:01 0 +1
12:02 1 1
12:03 0 +1
12:04 1
SupposethatthePVfleetcapacitywassplitbetweentwolocationsandeachweretoexhibit
maximumoutputvariability.Twopossiblescenariosexist.Thefirstscenario,illustratedinTable2,
assumesthatbothplantsturnonandoffsimultaneously.Aswasthecasewhereallcapacityis
concentratedatasinglelocation,thechangeinoutputfluctuatesbetween 1and1MWandthe
standarddeviationforthisscenariois1MWperminute.
Thesecondscenario,illustratedinTable3,assumesthattheplantscycleonandoffalternatelywitha
timeshiftof1minute.Inthiscase,thechangeinoutputfromthefirstlocationcancelsthechangein
outputatthesecondlocation.Theresultofthisscenarioisastandarddeviationof0MWperminute.
Itisincorrecttoconclude,however,thattheupperboundofoutputvariabilityfor1MWofPVis1MW
perminutebecausethisisthelargervalueofthetwoscenarios(thefirstequals1MWperminuteand
thesecondequals0MWperminute).Thisisbecauseeachofthetwoscenariosviolatestheassumed
conditionthatthelocationsareuncorrelated.Specifically,thechangeinoutputbetweenthetwo
locationshasperfectpositivecorrelationinthefirstscenario(i.e.,correlationcoefficientequals1)and
perfectnegativecorrelationinthesecondscenario(i.e.,correlationcoefficientequals 1).
3ThestandarddeviationofarandomvariableXequalsthesquarerootoftheexpectedvalueofXsquaredminusthesquareoftheexpectedvalueofX. EX EX.
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Table2.Maximumchangeinpoweroutputattwolocations(scenario1).
Time Power(MW) Change(MW/min)
Plant1 Plant2
Fleet
(1+2)
12:00 0.5 0.5 1 112:01 0 0 0 +1
12:02 0.5 0.5 1 1
12:03 0 0 0 +1
12:04 0.5 0.5 1
Table3.Maximumchangeinpoweroutputattwolocations(scenario2).
Time Power(MW) Change(MW/min)
Plant1 Plant2 Fleet1+2
12:00 0.5 0 0.5 0
12:01 0 0.5 0.5 0
12:02 0.5 0 0.5 0
12:03 0 0.5 0.5 0
12:04 0.5 0 0.5
FeasibleMaximumOutputVariabilityThesescenariosdemonstratethatitisimpossiblefortwosystemstoexhibitthebehaviorofworstcase
varianceindividually(bycyclingonandoffateachinterval)withouthavingeitherperfectpositiveor
perfectnegativecorrelation.Indeed,foreachsystemtoexhibititsmaximumvariance,itsoutput
changesmustbeexactlyintempowiththetimeinterval,looselyanalogoustoeachmemberofan
orchestrafollowingintimetoitsconductor,inwhichcasethesystemswouldbydefinitionhaveperfect
correlation(whetherpositiveornegative).Bythisreasoning,themaximumoutputvariabilityscenario
describedabove(1MWofvariabilityforeach1MWoffleetcapacity)isimpossible.Whenthesystems
havelessthanperfectcorrelation,asmustbethecaseforanyrealworldfleet,thevariabilityofthe
combinedfleetmustbelessthanthetotalfleetcapacity.
Tocorrecttheworstcasescenario,retaintheassumptionthateachpowerchangeiseitheratransition
fromzerooutputtofulloutputorfromfulloutputtozerooutput. Thisassumptioninitselfishighly
conservativesincetheimpactsofcloudtransientsonPVsystemswillalmostneverproducechanges
withmagnitudesashighas100percentofratedoutputandwillgenerallyproducechangesmuchless
than100percent.Asfortiming,ratherthanbeingsynchronized,eachsystemisassumedtocycleonand
offinarandomfashion,representingfleetsofPVsystemswithoutputsthatareuncorrelated.
RandomtimingofpoweroutputchangesisillustratedforasinglelocationinTable4fora1MWPV
system.Supposethatitis12:00andthetimeintervalis1minute.Thereisa50percentchancethatthe
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CorrelationversusDistanceBackground:CriticalFactorsAffectingCorrelationThecriticalfactorsthataffectoutputvariabilityaretheclearnessofthesky,sunposition,andPVfleet
orientation(i.e.,dimensions,plantspacing,numberofplants,etc.).Toimproveaccuracy,HoffandPerez
(2010)introducedaparametercalledtheDispersionFactor.TheDispersionFactorisaparameterthat
incorporatesthelayoutofafleetofPVsystems,thetimescalesofconcern,andthemotionofcloud
interferencesoverthePVfleet.HoffandPerezdemonstratedthatrelativeoutputvariabilityresulting
fromthedeploymentofmultipleplantsdecreasedquasiexponentiallyasafunctionofthegenerating
resourcesDispersionFactor.Theirresultsdemonstratedthatrelativeoutputvariability(1)decreasesas
thedistancebetweensitesincreases;(2)decreasesmoreslowlyasthetimeintervalincreases;and(3)
decreasesmoreslowlyasthecloudtransitspeedincreases.
MillsandWiser(2010)analyzedmeasuredoneminuteinsolationdataoveranextendedperiodoftime
for23timesynchronizedsitesintheSouthernGreatPlainsnetworkoftheAtmosphericRadiation
Measurement(ARM)program.Theirresultsdemonstrated7
thatthecorrelationofthechangeintheglobalclearskyindex(1)decreasesasthedistancebetweensitesincreasesand(2)decreasesmore
slowlyasthetimeintervalincreases.
Perezet.al.(2010b)analyzedthecorrelationbetweenthevariabilityobservedattwoneighboringsites
asafunctionoftheirdistanceandoftheconsideredvariabilitytimescale.Theauthorsused20second
tooneminutedatatoconstructvirtualnetworksat24USlocationsfromtheARMprogram(Stokesand
Schwartz,1994)andtheSURFRADNetworkandcloudspeedderivedfromSolarAnywhere(2010)to
calculatethestationpaircorrelationsfordistancesrangingfrom100metersto100kmandfrom
variabilitytimescalesrangingfrom20secondsto15minutes.Theirresultsdemonstratedthatthe
correlationof
the
change
in
global
clear
sky
index
(1)
decreases
as
the
distance
between
sites
increases
and(2)decreasesmoreslowlyasthetimeintervalincreases.
Theconsistentconclusions8ofthesestudiesarethatcorrelation:(1)decreasesasthedistancebetween
sitesincreasesand(2)decreasesmoreslowlyasthetimeintervalincreases.HoffandPerez(2010)add
thatthecorrelationdecreasesmoreslowlyasthespeedofthecloudsincreases.
ObjectiveUtilityplannersclearlyrequireatoolthatcanreliablyquantifythemaximumoutputvariabilityofPV
fleetsusingamanageableamountofdataandanalysis.Equation(3)wouldpotentiallymeetthis
requirementifthechangeinoutputbetweenlocationswereuncorrelated(i.e.,correlationcoefficientis
zero).Inrealfleets,PVsystemswillgenerallyhavesomedegreeofcorrelation,soanyplanningtoolwill
havetoincorporatecorrelationeffectsincalculatingactualfleetvariability.
Thispapertakesasteptowardsageneralmethodbyanalyzingthecorrelationcoefficientofthechange
inclearnessindexbetweentwolocationsasafunctionofdistance,timeinterval,andotherparameters.
7SeeFigure5inMillsandWiser(2010).8TheresultsapplytoeitherchangesinPVoutputdirectlyorchangesintheclearskyindex
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ItuseshourlyglobalhorizontalinsolationdatafromSolarAnywhere(2010)tocalculatecorrelation
coefficientsfor70,000scenariosacrossthreeseparategeographicregionsintheUnitedStates
(Southwest,SouthernGreatPlains,andHawaii).Thecorrelationcoefficientstakenfromthesescenarios
arethencomparedtoamethodthatcouldproveusefulwhenintegratedintoutilityplanningand
operationstool.Recognizingthatthemethodmustalsobevalidatedforshortertimeintervals(several
secondstoseveralminutes),itsresultsarecomparedtostudiesbasedon10second,20second,and1
minuteinsolationdatasets.
ApproachHoffandPerez(2010)definedPVfleetvariabilityasthestandarddeviationofitspoweroutputchanges
usingaselectedsamplingtimeinterval(e.g.,suchasoneminuteoronehour)andanalysisperiod(such
asoneyear),asexpressedrelativetothefleetcapacity.Tosimplifythework,theyformulateditinterms
ofthechangeininsolationratherthanthechangeinPVpower.
Asstatedearlier,skyclearnessandsunpositiondrivethechangesinshorttermoutputforindividualPV
systems.MillsandWiser(2010)andPerez,et.al(2010)subsequentlyisolatedtherandomcomponentofoutputchangeandexaminedchangesattributableonlytochangesinglobalclearsky(orclearness)
index.Theglobalclearnessindexequalsthemeasuredglobalhorizontalinsolationdividedbytheclear
skyinsolation.
ThispapercontinuesinthedirectionofMillsandWiser(2010)andPerez,et.al.(2010)andfocuseson
changesintheglobalclearnessindex.
ChangeinGlobalClearnessIndexTheglobalclearnessindexataspecificpointintimeistypicallyreferredtoasKt*.Itequalsthe
measuredglobalhorizontalinsolation(GHI)dividedbytheclearskyinsolation.Thispaperreferstothe
changeintheindexbetweentwopointsintimeas Kt*.Sincethechangeoccursoversomespecified
timeinterval, t,atsomespecificlocationn,thevariableisfullyqualifiedas,
.Thisonly
representsonepairofpointsintime.Asetofvaluesisidentifiedbyconventionbyboldingthevariable.
Thus,
isthesetofchangesintheclearnessindicesataspecificlocationusingaspecifictime
intervaloveraspecifictimeperiod.
,,
,,, ,, ,,
(4)
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Copyright2010CleanPowerResearch 11
Table5illustrateshowtocalculatethechangeinclearnessindex(Kt*)duringconditionsofrapidly
changinginsolation.Forexample, Kt*between12:00and12:01equalsthedifferencebetweenKt*at
12:01andKt*at12:00(0.51.0= 0.5).
Table5.Exampleofhowtocalculatechangeinclearnessindex(Kt*)using t=1minute.
Time GHI ClearskyGHI Kt* Kt*
12:00 1.0 1.0 1.0 0.5
12:01 0.5 1.0 0.5 0.5
12:02 0.0 1.0 0.0 +0.5
12:03 0.5 1.0 0.5 +0.5
12:04 1.0 1.0 1.0
Correlationanddependenceinstatisticsareanyofabroadclassofstatisticalrelationshipsbetweentwo
ormorerandomvariablesorobserveddatavalues(Wikipedia2010).Let
and
represent
twosetsofobserveddatavaluesforthechangeintheclearnessindexthathaveameanof0and
standarddeviations,and.9
Pearsonsproductmomentcorrelationcoefficient(typicallyreferredtosimplyasthecorrelation
coefficient)equalstheexpectedvalueof times dividedbythecorrespondingstandarddeviations.
,
(5)
Theanalysisisperformedasfollows:
1. Selectageographicregionforanalysis2. Selectalocationforthefirstpartofthepair3. Selectalocationforthesecondpartofthepair4. Selectatimeintervalfortheanalysis5. Selectaclearskyirradiancelevelbin6. Obtaindetailedinsolationdata7. Calculatethecorrelationcoefficient108. Repeatthecalculationforallsetsoflocationpairs,timeintervals,andclearskyirradiancebins.
9TheexpectedvalueofKt*equals0aslongasthestartingandendingGHIvaluesarethesame.Thisconditionis
satisfiedwhenthetimeperiodoftheanalysisisperformedoveronedaybecausethestartingandendingGHIboth
equal0.Itwillalsobeapproximatelytruewhentheanalysisencompassesmanydatapoints(aswouldbethecase,
forexample,ofananalysisofonehourofdatausingaoneminutetimeinterval).
10AppendixBillustrateshowtocalculateKt*correlationcoefficients.
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Copyright2010CleanPowerResearch 20
ThepaperusedhourlyglobalhorizontalinsolationdatafromSolarAnywheretovalidatethemethodby
calculatingcorrelationcoefficientsfor70,000scenariosacrossthreeseparategeographicregionsinthe
UnitedStates(Southwest,SouthernGreatPlains,andHawaii),whilevaryingdistance,timeinterval,
insolationbin,andotherparameters.Theseempiricalcorrelationcoefficientscomparedfavorablywith
thosederivedbythemethod. Themethodwasthenshowntobeindependentofselectedtimeinterval,
suchthathourlysatellitedatacouldbeusedtocalculatecorrelationcoefficientsforveryshorttime
intervals(severalsecondstoseveralminutes).Theseextrapolatedresultswerevalidatedusingresults
fromstudiesthatarebasedon20secondtooneminuteinsolationdata.
Thepaperhadseveralimportantfindings.First,correlationcoefficientsdecreasedwithincreasing
distance.Second,correlationcoefficientsdecreasedatasimilarratewhenplottedversusdistance
dividedbytimeinterval.Third,theaccuracyofresultswasfurtherimprovedwhenanimpliedspeed
termisintroducedintotheanalysis.Together,theseresultsprovidedthebasisforvalidatingthe
generalizedmethod.Themethod,basedoninputparametersfromhourlySolarAnywheredata,
producedcorrelationcoefficientsforshorttimeintervals(secondstominutes)thatcomparedquitewell
toresultsfromindependentstudiesthatused10second,20second,andoneminutedatasets.
Thepreliminaryconclusionofthisworkisthattheapproachvalidatedinthispapercanbeusedto
identifytheconditionsunderwhichthechangeinoutputbetweenlocationsareuncorrelated.Asa
result,itcanbeusedtosatisfyoneoftheinitialmotivationsofthisstudy:thedesiretoequiputility
plannerswithatoolcapableofplacinganupperboundonthemaximumoutputvariabilityofafleetof
PVsystemsusingamanageableamountofdataandanalysis.
Theresults,however,mayhavefurtherimplications.Inparticular,theresultsmaybethebasisfor
quantifyingoutputvariabilityevenwhencorrelationexists.
NextStepsThisstudydemonstratedtheabilitytopredictcorrelationcoefficientsusingtimeintervalsof1to4hours
usingmultiyeardatasets.Resultsalsosuggestedthatthemethodisvalidforshorttimeintervalswhen
comparedtohighspeedstudies,againbasedonlongtimeperioddatasets.
Thenextstepswillbetofurthervalidatetheresultsforshorttimeintervalsusingmeasuredhigher
speeddata.Plansincludetheuseof:1kmx1kmgrid,hourSolarAnywheredatainselectedlocations;
1kmx1kmgrid,oneminuteextrapolatedSolarAnywheredatainselectedlocations;andadditional10
seconddatafromthemobile,highdensitynetworkdescribedearlier(HoffandNorris,2010).A
particularlyimportantfocusofthisworkwillbetoassessthemethodsabilitytopredictcorrelation
betweenlocationsovershorttimeperiodsaswellaslongtimeperiods(severalhoursversusseveral
years).
AcknowledgementsPortionsofthisstudywerefundedunderaCaliforniaSolarInitiative(CSI)GrantAgreementtitled
AdvancedModelingandVerificationforHighPenetrationPV.TheCaliforniaPublicUtilities
CommissionistheFundingApprover,ItronistheProgramManager,andPG&EistheFunding
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Copyright2010CleanPowerResearch 21
Distributor.ThankstoBenNorris(CleanPowerResearch)whodesigned,implemented,andoperated
themobileirradiancenetworkandprovidedvaluablecommentsonthepaper.ThankstoJeffRessler
(CleanPowerResearch)forhiscomments.Opinionsexpressedhereinarethoseoftheauthorsonly.
ReferencesHoff,T.E.,Perez,R.2010.QuantifyingPVpowerOutputVariability.SolarEnergy84(2010)17821793.
Hoff,T.E.,Norris,B.2010.MobileHighDensityIrradianceSensorNetwork:CordeliaJunctionResults.
Kuszamaul,S.,Ellis,A.,Stein,J.,Johnson,L.2010.LanaiHighDensityIrradianceSensorNetworkfor
CharacterizingSolarResourceVariabilityofMWScalePVSystem.35thPhotovoltaicSpecialists
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SolarPower.LawrenceBerkeleyNationalLaboratoryTechnicalReportLBNL3884E.
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Forecasted7daysAheadandArchivalDatabacktoJanuary1,1998.www.SolarAnywhere.com.
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Copyright
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#11.0
0.0
0.0
1.0
1.0
ioncoefficie
GHI(kW/
#11.0
0.0
0.0
1.0
1.0
ioncoefficie
GHI(kW/
#11.0
0.0
0.0
1.0
1.0
Fi
n Power Res
resentthre
dtocalculat
Table8.
tequals1.0
m2) Clear
#2 #11.0 1.
0.0 1.
0.0 1.
1.0 1.
1.0 1.
tequals0.5
m2) Clear
#2 #11.0 1.
1.0 1.
0.0 1.
1.0 1.
1.0 1.
tequals0
m2) Clear
#2 #11.0 1.
1.0 1.
0.0 1.
0.0 1.
1.0 1.
ure13.Chan
earch
exampleso
correlation
Datatocalc
SkyI(kW/m2
#21.0
1.0
1.0
1.0
1.0
SkyI(kW/m2
#21.0
1.0
1.0
1.0
1.0
SkyI(kW/m2
#21.0
1.0
1.0
1.0
1.0
geinclearne
howtocalc
coefficients.
ulatecorrela
) Clearness
#11.0
0.0
0.0
1.0
1.0
) Clearness
#11.0
0.0
0.0
1.0
1.0
) Clearness
#11.0
0.0
0.0
1.0
1.0
ssindexforL
latethecha
tioncoefficie
Index C
#21.0
0.0
0.0
1.0
1.0
Index C
#21.0
1.0
0.0
1.0
1.0
Index C
#21.0
1.0
0.0
0.0
1.0
ocation2vs.
ngeinthecl
nts.
angeinClear
#11.0
0.0
+1.0
0.0
angeinClear
#11.0
0.0
+1.0
0.0
angeinClear
#11.0
0.0
+1.0
0.0
Location1.
arnessindex
essIndex
#21.0
0.0
+1.0
0.0
essIndex
#20.0
1.0
+1.0
0.0
essIndex
#20.0
1.0
0.0
+1.0
23
,