Demand Cap Analysis

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    THEUPPERBASINVOLUNTARYDEMANDCAPASAMEANSOFMITIGATINGLEGALUNCERTAINTYINTHECOLORADORIVERBASIN:MODELINGRESULTS

    AReportoftheColoradoRiverGovernanceInitiative1

    April,2013

    Introduction

    InpreviouspublicationsoftheColoradoRiverGovernanceInitiative(CRGI),weconcludedone

    ofthemostimportantsourcesofuncertaintyinthebasinarethelegaluncertaintiesregarding

    theobligationsoftheUpperBasintoreleasewatertotheLowerBasin.Specifically,wehave

    highlightedthreerelatedandhighlysalientquestions:(1)doestheUpperBasinhavean

    obligationtodeliver7.5MAF/yeardownstream(onaverage)forLowerBasinconsumption;(2)

    doestheUpperBasinhaveanobligationtodeliverhalftheMexicanTreatyobligation(0.75

    MAF/year)downstream;and(3)canthefailuretoachieveoneorbothoftheseobjectives

    triggeracompactcall?2Thesearefundamentalquestions,astheylargelydeterminelongterm

    wateravailabilityinthebasin.Buttheyarealsolargelyignoredquestions,asuptothispoint,

    norulingonthesequestionshasbeenrequiredtooperatethesystemafortunatebyproduct

    ofUpperBasindemandsstillbeinglowenoughtoallowbothofthepresumeddelivery

    obligationstobefulfilled.Wherethesequestionscurrentlyariseareinlongtermsystem

    modeling,thelatestexamplebeingworkconductedfortheColoradoRiverBasinWaterSupply

    andDemandStudy(theBasinStudy).3

    Unfortunately,duetopoliticalsensitivities,theBasinStudydidnotprovide,orattemptto

    provide,adirectanalysisofthesequestions,asthemodelingassumptionswereconstructedin

    awaytominimizetheneedforcontroversiallegalassumptions.Thisisbestillustratedbythe

    conceptofmiraclewater.InmodelingscenariosinwhichtheUpperBasincouldphysically

    notdeliver7.5MAFdownstreamwithoutcurtailingUpperBasindepletions,theapproachwas

    toallowUpperBasinusestoproceedwithoutcurtailmentwhilemagicallyconjuringupthe7.5

    MAFdesiredbytheLowerBasinandinjectingitintothesystemdownstreamofLeesFerry

    evenifitwouldnotphysicallyexistinreality.Thissatisfiesthelegalinterpretationsand

    politicalobjectives

    of

    both

    basins:

    the

    Lower

    Basin

    receives

    the

    7.5

    MAF

    which

    they

    believe

    is

    1Formoreinformation,[email protected] orCRGIDirectorDougKenney([email protected]).2Themostcompletesummaryoftheseargumentshavebeenpublishedas:Robison,Jason,andDouglasS.

    Kenney.2013.EquityandtheColoradoRiver.EnvironmentalLaw,42(4):11571209[availableat:http://law.lclark.edu/live/files/13155robisonkenneyfinalforwebsitepdf].Avarietyofsupportingdocuments

    canbefoundattheColoradoRiverInformationPortalathttp://waterpolicy.info/projects/CRIP/index.html.3http://www.usbr.gov/lc/region/programs/crbstudy/finalreport/index.html

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    owedto

    orclarifi

    curtailm

    magnitu

    subtract

    doneto

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    Fig

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    (such

    withoutbei

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    couldbee

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    as

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    ThesharpdeclineinUpperBasinwateravailability5istheunavoidableconsequenceofhaving

    toreleasewaterdownstreambeforesatisfyingUpperBasindemandswhich,again,isapointof

    legaldispute,inpartbasedontheCompactwordinginSectionIII(d)thatdoesnotdescribe

    thesereleasesasandeliveryobligation,andinpartonthepremiseofequitythatruns

    through

    the

    Compact.

    As

    shown

    in

    the

    Figure

    1,

    a

    decline

    in

    average

    streamflows

    of

    20%well

    withinthescopeofmanyclimatechangestudiescouldresultinasituationinwhichLower

    BasinwateravailabilityfromthemainstemisroughlytwicethatoftheUpperBasin,despitethe

    intentoftheCompact(asshowninArticleIII(a))toallocateequalsharesamongbasins.

    ImposingafirmobligationupontheUpperBasintodeliverpartoftheMexicanobligationonly

    intensifiestheeffect.Obviously,thissqueezecouldhavecatastrophicconsequencesforUpper

    Basinusers,leadingustospeculatethatthesituationwouldeitherneveroccuri.e.,a

    negotiatedsolutionorsuccessfulUpperBasinlitigationwouldstopthecurtailmentsorwould

    occuronlyaftersuccessfulLowerBasinlitigation.Anyofthesesolutions,however,couldtake

    avarietyofformsandanumberofyearsperhapsdecadestocomplete,andtheoutcome

    wouldhavesignificantandimmediateimpactsonwateravailabilityinbothbasins.Thislegal

    uncertaintyhangsoverthebasinandhasforatleast65years6.Arguably,thissourceof

    uncertaintyoutweighstheclimateanddemanduncertaintiesexposedandfeaturedintheBasin

    Studyanalysis.

    Thereisnowaytoallocatewaterdifferentlybetweenthetwobasinsthatresultsinanet

    basinwidegaininwateravailability;itisazerosumeffort.Buttherearewaystoallocatewater

    thatbalancestheriskofclimaterelatedshortagesmoreequitablybetweenbasins,andwhich

    hasthebenefitofreplacinguncertaintywithcertainty.Inwatermanagement,thevalueof

    certaintycannot

    be

    underestimated,

    and

    as

    argued

    above,

    the

    greatest

    threat

    to

    certainty

    is

    themannerinwhichthelegalambiguitiesandomissionswillultimatelybeaddressed.Remove

    http://waterpolicy.info/projects/CRIP/index.html.Thefigureisbasedonahostofhighly(andintentionally)

    debatableassumptionsandsimplifications;thus,itshouldbeviewedasastartingpointfordiscussion,ratherthan

    aformalprojectionorlegalinterpretation.Specifically,inscenarioswherethelongtermaverageLeeFerryflowis

    14.5MAF/yearorhigher,itassumesthattheUpperBasinwillberequiredtomaintainaminimumdelivery

    scheduleof8.23MAF/yearinordertosatisfytheCompactandTreaty,andthattheLowerBasinwillberequiredto

    pass1.5MAF/yearofthiswatertoMexico,withtheremainderavailableforusebytheLowerBasin.Inscenarios

    wherethelongtermaverageLeeFerryflowis14.0MAF/yearorless,itassumestheUpperBasinwillberequired

    tomaintainaminimumdeliveryscheduleof8.18MAF/yearinordertosatisfytheCompactandTreaty,andthat

    theLowerBasinwillberequiredtopass1.4MAF/yearofthiswatertoMexico.(Notethatthisfigurewas

    developedprior

    to

    Minute

    319;

    those

    rules,

    if

    modeled

    here,

    would

    have

    anegligible

    impact

    on

    the

    trend

    lines

    shownhere.)Allvaluesaremaximumwateravailableforusebeforesubtractingevaporationorotherlosses.5Notethattheavailabilityofwaterandtheentitlementorallocationofwaterareseparate(butobviously

    related)issues.TheCompactisclearthattheUpperBasinisallocated7.5MAF/yearofconsumptiveuses(Article

    III(a)),butvirtuallynoclimatescenario(paleo,historic,orfutureprojections)suggeststhisisarealisticpossibilityif

    anobligationtopasswaterdownstreamexists.6ThisconcernispartofthesubtextoftheUpperBasinCompactnegotiations(circa1948)[transcriptsavailableat

    http://lawpac.colorado.edu/record=b119651],andisreflectedinthedecisiontoallocateUpperBasinsharesin

    percentagesratherthanfixedvalues.

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    theselegaluncertaintiesandthedoorisopentoavarietyofdealsandcopingmechanisms,and

    theneedtoprepareforlegalshockstothesystemareavoided.This,inanutshell,wasthe

    motivationfortheUpperBasinVoluntaryDemandCapoptionsubmittedbytheCRGItothe

    BasinStudyforanalysis.Thefactthatthisoptionandtheothersocalledgovernance

    options

    7

    were

    not

    analyzed

    is

    the

    motivation

    for

    this

    memo.

    TheDemandCapConcept

    ThecentralideaoftheUpperBasinVoluntaryDemandCap(hereaftertheDemandCap)is

    thattheUpperBasinagreestolimittotalUpperBasindepletionsatanegotiatedlevel(well

    belowthetheoretical7.5MAF/year)and,inreturn,isassuredthatneitherthefederal

    governmentnorthestatesoftheLowerBasinwillrequestorsupportadministrationofan

    interbasincompactcallinanyperiodwhenstorageinLakePowellisinsufficienttomaintain

    thepredetermined

    downstream

    release

    objective.8

    Establishing

    the

    value

    of

    the

    cap

    and

    the

    releaseobjectivearepointstobenegotiated;buttheprincipleistoestablishthesenumbersin

    advanceofacrisisandwithoutaneedtolitigatetheomissionsandambiguitiesthatexistinthe

    CompactandrelatedelementsoftheLawoftheRiver.Inthatregard,theDemandCapisnot

    intendedtoreplaceoramendtheCompact9,butrather,isanoperationalregimeplacedontop

    ofthisfoundationfollowingtheprecedentofthe2007InterimGuidelinesforLowerBasin

    ShortagesandCoordinatedOperationsforLakePowellandLakeMead(InterimGuidelines).

    AlsoanalogoustotheInterimGuidelines,enactmentofthevoluntaryagreementwouldrequire

    theunanimousagreementofthesevenbasinstates,andindoingso,wouldestablisha

    temporaryarrangement.

    In

    this

    case,

    the

    proposed

    operating

    regime

    would

    remain

    in

    effect

    foratermof40years,subjecttorenewal(nolaterthan10yearspriortoexpiration)by

    affirmativeactionbyaminimumof5of7states.Theagreementcouldbemodifiedor

    741of160submittedoptionswerecharacterizedasinvolvinggovernance;see

    http://www.usbr.gov/lc/region/programs/crbstudy/finalreport/techrptF.html.8TheDemandCapproposalcanbefoundintwoslightlymodifiedforms:theoriginalversionintheBasinStudy

    materials(option117at

    http://www.usbr.gov/lc/region/programs/crbstudy/finalreport/Technical%20Report%20F%20

    %20Development%20of%20Options%20and%20Stategies/Appendix%202%20

    %20Options%20Submitted%20to%20the%20Study/Appendix%20F2%20

    %20Options%20Submitted%20to%20the%20Study.pdf),andaslightlyupdatedversionontheColoradoRiver

    InformationPortal

    (http://waterpolicy.info/archives/docs/Upper%20Basin%20Voluntary%20Demand%20Cap,%20amended%20Feb%

    202012.pdf?p=1683).Neitherversionisreprintedhereinitsentirelyasthefollowingsectionprovidesthemost

    comprehensivearticulationandanalysistodate.9Infact,theDemandCapproposalisseenasawaytohonorandreinforcetheheartoftheCompact,whichisthe

    commitmenttoanequalsharingofwateramongthetwobasins.

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    terminatedatanytimebyunanimousagreementofthestates.Onceterminated,theLawof

    theRiver,asitcurrentlyexists,providesthedefaultlegalandoperationalregime.

    TheDemandCapisnotacompletelynewidea,asasimilarideawasoncefloatedataBasin

    StudymeetinginAlbuquerque.10

    Then,asnow,theidearaisesseveralconcerns.Firstand

    foremost,while

    the

    value

    of

    eliminating

    legal

    uncertainty

    is

    undeniably

    attractive

    and

    valuable,

    thereisabenefitassociatedwithuncertaintyinthatitallowsallpartiestoretainhopeforthe

    legalinterpretationthatbestsuitstheirinterests.ToagreetoacapforcestheUpperBasinto

    concedeapracticalapportionmentsignificantlylessthan7.5MAF11;similarly,agreeingtothe

    proposalforcestheLowerBasintoconcedethattheirapportionmentisnotseniortoallUpper

    Basinuses(exceptUpperBasinPresentPerfectedRights).Forbothparties,theideamakes

    senseonlytotheextentthattheconcessionsinvolvedaremorethanoffsetbythevalueof

    thereducedlegaluncertaintyandtheotherancillarybenefitsoftheproposal.Insummary,

    potentialbenefitsoftheDemandCap(ascomparedtothestatusquo)include:x ThethreatofaninterbasinCompactcalliscompletelyeliminatedtherebyprotecting

    existingUpperBasinwaterusersfromacall,andeliminatingtherelianceofLowerBasin

    usersonsuccessfullylitigatingacallasistheneedforanyinterim

    litigation/negotiationconcerningtheexistenceofanUpperBasindeliveryobligation

    andseveralrelatedlegalissues(includingtheUpperBasinsshareoftheMexican

    deliveryobligationandtheuseofLowerBasintributaries);

    x TheDemandCaparrangementprovidesmechanisms(namely,theUpperBasincaponconsumption)thatencouragethemaintenanceofstorageinLakePowell(andallthe

    associatedbenefits

    thereof,

    including

    drought

    protection,

    and

    protection

    of

    recreation

    andhydropowerindustries);

    x Withtheexceptionofsomenewadministrativeexpenses(associatedprimarilywithtrackingUpperBasinconsumption),theDemandCapoptionrequiresnonew

    expenditures,andinfactislikelytosavesignificantpublicfundsbyeliminatingor

    reducingtheneedformanyexpensiveriskcopingstrategies,andbyreducingthe

    financialcosts(andpotentialimpacts)oflitigation;and,

    x Thearrangementprovidesafoundationuponwhichmanyemergingandnewreformscouldbeestablished,whilemaintainingtheexistingLawoftheRiverasthedefault

    10See:Kuhn,Eric.2011.RiskManagementStrategiesfortheUpperColoradoRiverBasin.DraftofJune7.

    11Arguably,thishasalreadyoccurredinUpperBasinreports,includingtheseminalstudybyTiptonandKalbach

    (1965)estimatinglongtermUpperBasinwateravailabilityasrangingfrom4.7to6.3MAF/year.(Tiptonand

    Kalbach,Inc.1965.WaterSuppliesoftheColoradoRiver.ReportpreparedfortheUpperColoradoRiverCommission.Denver,July.)ThisisalsodoneintheHydrologicDeterminations.

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    condition.Bylargelyremovingortemperingthegamechanginguncertainties

    (associatedwiththeeffectofclimatechangeonaverageandextremeflows,andthe

    interpretationofkeyLawoftheRiverissues),theDemandCapestablishesan

    environmentencouragingfurtherinnovations(includingriveraugmentation).

    TheModelingEffort

    Thefollowingmodelingwasconductedinsummerandfall2012usingCRSS12

    byKevinWheeler,

    ownerofWaterBalanceConsulting(andaproductoftheUniversityofColoradoCenterfor

    AdvancedDecisionSupportforWaterandEnvironmentalSystems(CADSWES)).Thisworkwas

    donecommensuratewiththeBasinStudyand,assuch,utilizedassumptionsfromthat

    investigationwhereverpossiblewithafewnotableexceptions.Modelingresultsareshown

    below,precededbyadiscussionofsomeprominentmodelingassumptionsandadjustments

    thatshaped

    the

    study

    design.

    MethodologyandAssumptions

    Themodelingapproachwastocomparetheperformanceofthedemandcapscenarioagainsta

    statusquo(hereaftertheBaseline)scenario,primarilyfromthestandpointofconsumptionlevelsinbothbasinsandreservoirstorage.Thesearethemacrolevelvariablesofinterestin

    anyoperationalregimethatmodifiestherelationshipbetweentheUpperandLowerBasin.For

    bothscenarios,

    inputs

    (supplies)

    derive

    from

    use

    of

    the

    downscaled

    GCM

    projected

    hydrology.

    Thatclimaticscenario,whichassumeswarming,hasthefurtherinfluenceofaugmenting

    demandsspecifiedintheBasinStudysScenarioAdemandschedule.13

    Thesesupplyand

    demandelementshaveavarietyofembeddedassumptionsandshortcomings,notdetailed

    here,butwereselectedtodovetailtheanalysiswiththeBasinStudytotheextentpossible.

    Similarly,weutilizedtheBasinStudytimehorizon,whichextendsto2060.Someofthe

    benefitsoftheDemandCapproposalareprobablymoreevidentatlaterdates,butwecould

    notexplorethispointwithoutaccesstosupplyanddemandscenariosextendingpast2060.

    Toperformthiscomparison,afewelementsofCRSShadtobemodified.Asforeshadowed

    earlier,themiraclewateralgorithmhadtobemodifiedintwoways.First,inthoseinstancesin

    whichmiraclewaterwasutilizedintheBaselinescenarios,thosequantitiesweresubtracted

    fromUpperBasinusetogetanaccuratevalueofhowmuchwatertheUpperBasinactually

    12CRSSistheColoradoRiverSimulationSystem,aRiverWarebasedmodelthatistheofficialmodelusedbythe

    BureauofReclamationforsystemoperationsandscenarioplanning.13

    Theimpactofassumedwarmingondemandsissignificant,averageroughly0.5MAF/yearby2060.

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    consumed.FailuretodosowouldmakecomparisonsoftheBaselinetotheDemandCap

    scenariomeaningless.Second,themiraclewateralgorithmisunlimitedi.e.,theprogramcan

    addinmorewaterthanwouldphysicallybemadeavailablefromUpperBasincurtailments.As

    amatterofphysicsandpolicy,welimitedmiraclewatertotheamountthatcouldactuallybe

    achieved

    through

    Upper

    Basin

    curtailments,

    subject

    to

    the

    protection

    of

    Upper

    Basin

    Present

    PerfectedRights(whichweassumetobe2.2MAF).

    AlsoproblematicwasthefactthatCRSSoperatesbasedondemands,notdepletions.Despite

    thenameDemandCap,ourproposalis,inreality,adepletioncap.Additionally,insatisfying

    demands,CRSStracksofwateravailabilityanddemandsinvariousreaches/tributaries,and

    doesnotsatisfydemandsinagivenriversegmentwherewaterisphysicallyunavailable.For

    thepurposesofouranalysis,thislevelofdetailissomewhatcounterproductive,asweassume

    thatonceafirmcapisinplace,physicalandinstitutionaladjustmentswouldbemadetoensure

    fulluseofthecap.AdjustmentsweremadetohittheUpperBasindepletionmaximums

    describedin

    the

    Demand

    Cap

    scenarios.

    BoththeBaselineandDemandCapscenariosrequiredrefinements.Ofthetwo,specifyingthe

    Baselinescenariowasthelargerchallenge,asitrequiressomeassumptionsabouthowthe

    currentrulesmightactuallybeinterpretedinpractice.Twoissuesareparticularlysalient.First,

    themagnitudeoftheUpperBasindeliveryobligationhadtobespecifiedatsomelevel,with7.5

    MAF/yearand8.25MAF/yearbeingobviouscandidates.Ratherthanchooseoneoftheother,

    weutilizedbothvalues(thuscreatingtwoBaselinescenarios).Second,theInterimGuidelines

    arescheduledtoexpirein2026ifnotrenewedormodified.Wechoosetokeepthese

    guidelines

    throughout

    the

    full

    scenario.

    To

    the

    extent

    that

    other

    legal

    assumptions

    were

    required,unlessotherwisenoted,weretainedtherulesalreadycodifiedinCRSS.

    ThreeadjustmentstotheoriginalDemandCapscenarioarenotable.First,weoriginally

    proposedusingacapvaluethatincludedUpperBasinevaporationlosses.Ultimately,we

    decidedtospecifyanUpperBasincapnumberbeforeevaporation,whichimmunizedtheUpper

    Basinfromthepracticalchallengeoftryingtopredictevaporationpreciselyinanygivenyear.

    (Weassumethoselossestobeintheneighborhoodof0.5MAF/year.)Second,inorderto

    investigatethepotentialbenefitsoftheDemandCapproposalinprotectingreservoirstorage,

    wequicklyrealizedthatitmightbeadvisabletopreventtheLowerBasinfromusingsurpluses

    attributableto

    enforcement

    of

    the

    Upper

    Basin

    cap.

    To

    do

    this,

    aLower

    Basin

    cap

    of

    7.5

    MAF/yearwasimposedthroughoutmostoftheDemandCapscenarios.Andthird,through

    initialmodelingrunswedeterminedthatanUpperBasincapof4.5MAF/year(notcounting

    evaporation)wasthebestvalueforillustratingthetradeoffsinherenttotheDemandCap.

    (Theoriginalproposalsuggested5.5MAFroughly5MAFindepletionsand0.5MAFin

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    evaporationasastartingpointofanalysis.)Ofcourse,weencouragesubsequentanalyses

    thatfeatureabroaderrangeofvalues.

    Results

    Theresultspresentedbelowarefromthesixth(andfinal)iteration,bywhichtimethekey

    modelingissuesdescribedabovehadbeenidentifiedandresolved.Eachfigureprovidesresults

    forthreescenarios:

    75Prot22 Thisbaselinescenarioassumesadeliveryobligationaveraging7.5MAF/year.

    FailuretodeliverthisvolumeresultsinUpperBasincurtailmentsasnecessary

    tomeetthisdelivery,withthecaveatthat2.2MAFofUpperBasinPresent

    PerfectedRightsarealwaysprotectedfromcurtailment(hencetheProt22

    nomenclature).

    82.5Prot22 Thisbaselinescenarioassumesadeliveryobligationaveraging8.25MAF/year.

    Aswith75Prot22,failuretodeliverthisvolumeresultsinUpperBasin

    curtailmentsasnecessarytomeetthisdelivery,withthecaveatthat2.2MAF

    ofUpperBasinPresentPerfectedRightsarealwaysprotectedfrom

    curtailment.

    4.5DoubleCap ThisDemandCapscenarioallowstheUpperBasintodeplete4.5MAF/year

    beforeevaporativelosses(roughly0.5MAF/year),andadditionallycaps

    LowerBasin

    consumption

    at

    7.5

    MAF/year.

    No

    Upper

    Basin

    delivery

    obligationisenforced(i.e.,noCompactcalls).

    Afewfiguresplottwoadditionalvariables:

    ASchedule(withClimateChange) ThesearetheprojectedUpperBasindemandsfromthe

    BasinStudyScheduleAdemandscheduleasadjusted(increased)toreflect

    theaddeddemandsassociatedwiththedownscaledGCMprojected

    hydrology.

    4.5SingleCap ThisDemandCapscenarioallowstheUpperBasintodeplete4.5MAF/year

    beforeevaporativelosses(roughly0.5MAF/year).NocaponLowerBasin

    consumptionisenforced.NoUpperBasindeliveryobligationisenforced(i.e.,

    noCompactcalls).

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    Collectively,thesevariablesallowustotrackdifferencesinhowtheDemandCapaffectswater

    availability(measuredintermsoftheamountofconsumptionallowed)andchangesin

    reservoirstorage.Asapracticalmatter,watermanagersarelikelytowanthighlevelsofboth

    variables,althoughinrealitythereisafixedquantityofwater,andmaximizingboth

    consumption

    and

    storage

    at

    all

    times

    is

    an

    impossibility.

    Similarly,

    it

    is

    an

    impossibility

    to

    simultaneouslyincreasewaterconsumptionandstorageforallusers;inputstothesystemare

    notmodifiedacrossallthescenariosi.e.,theyallusethesamedownscaledGCMprojected

    hydrologysothisisazerosumexercise.Thus,thewaytoevaluatetheresultsistocompare

    thequantitativetradeoffsintermsofsupplies(asmeasuredbyconsumption),storage(as

    measuredbyreservoirvolume/elevation),andreliability,andtodothiswithrespecttothe

    nonquantitativetradeoffsassociatedwiththeeaseofmaintainingthestatusquo(offeredbytheBaselinescenarios)versusthebenefitsofeliminatinglegaluncertainties(offeredbythe

    DemandCapscenarios).

    Giventhe

    importance

    of

    these

    non

    quantitative

    variables,

    it

    is

    impossible

    for

    us

    to

    impartially

    establishanyscenarioasthewinnerorbest,andthus,toarguefororagainstenactmentof

    theDemandCappolicy.Butthatisnotthepointofthisexercise.Thepointistoillustrate

    tradeoffsandopportunitiesassociatedwiththepursuitofagovernancebasedsolution,inthis

    case,aDemandCapscenario.WhetherornottheDemandCapisagoodapproachiscertainly

    debatable;whetherornotgovernancebasedreformsshouldbepartofthesearchforsolutions

    isnot.Basinleaderswillsoonbeforcedtomakedecisionsregardingseveralgovernanceand

    LawoftheRiveritems,includingextensionoftheInterimGuidelines;thedefinitionofUpper

    Basindeliveryobligations,ifany,totheLowerBasinand/ortoMexico;thedesignand

    implementation,ifany,

    of

    an

    interbasin

    Compact

    call;

    the

    quantification

    of

    Upper

    Basin

    Present

    PerfectedRights;andsoon.Again,muchoftheappealoftheDemandCapisthatitcan

    subordinateorcompletelyeliminatemanyofthemostdivisiveissues,anddosoinawaythat

    leavestheCompactunalteredandasthedefaultinstitutionalframework.

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    Depletions:Upper asin

    10

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    Depletions:Lower asin

    11

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    ReservoirStorage

    12

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    13

    FindingsandConclusions

    Theprecedingfiguresillustratesomeofthemostimportanttradeoffsassociatedwithadopting

    theDemandCapproposal.Asnotedearlier,thedatadoesnotallowustomakeadefinitive

    rulingaboutwhichapproachisbest,butitdoesallowustospeculateonthetradeoffs

    (assuminga4.5

    MAF

    cap)

    that

    would

    be

    central

    to

    any

    decision

    making.

    What

    we

    believe

    to

    be

    thesalientlessonsofFigures2through7aresummarizedbelow.

    Depletions:UpperBasin

    Theplotofaveragedepletions(Figure2)isperhapsmostnotableforshowinghowboththe

    BaselineandDemandCapscenariosfallwellbelowthedemandsassociatedwithScheduleA

    anddownscaledGCMprojectedhydrology.TheDemandCapdoesnotsolvethisproblemof

    unmetdemands,

    but

    neither

    does

    either

    Baseline.

    14

    Thus,

    this

    plot

    is

    abetter

    illustration

    of

    the

    UpperBasinsupply/demandmismatchthanitisinstructiveinilluminatingasolution.

    ThePDF(probabilitydistributionfunction)showninFigure3illustratesakeyfeatureofthe

    DemandCap,asUpperBasindepletionsarerelativelyflatandstablewhencomparedtothe

    Baselinescenarios.Overall,theBaselinescenariosofferslightlymorewaterabout60%ofthe

    timeandslightlylessabout40%ofthetime,withbigdifferencesseenonlyattheextremes.Of

    course,muchofwatermanagementisfocusedonmanagementattheextremes.

    Overall,theUpperBasindepletionfiguresillustratethat,whiletheDemandCapconceptmight

    firstseem

    like

    aradical

    and

    significant

    concession

    for

    the

    Upper

    Basin,

    the

    effect

    during

    the

    studyperiodisrelativelymodestatleastatthe4.5caplevel.Extendingthetimehorizonpast

    2060wouldlikelyyieldmoredramaticresults,aswouldchangingtheclimatehydrology

    assumptions.Ultimately,fortheUpperBasin,thekeydecisionsarewhetherornotlosingthe

    extremehighsisworthbeinginsulatedagainsttheextremelows,andwhetherornottabling

    thelegalissues(forthetermoftheagreement)ispreferabletoleavingthoseopen.

    Depletions:LowerBasin

    Notsurprisingly,theplotofaverageLowerBasindepletions(Figure4)showstheneteffectof

    theDemandCapistolimitLowerBasindepletionsbelowwhatwouldbepossiblegiventhe

    Baselinescenariosassumingenforcementofeithera7.5MAF/yearor8.25MAF/yearUpper

    14ItisquitepossiblethatCRSSoverestimatestheUBshortagesforeachofthesescenarios,inthattheresolutionof

    themodeldoesnotincludesomeexistingstoragereservoirsand,thus,mayunderestimatetheabilityofthe

    systemtomeetsomedemands.

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    14

    Basindeliveryobligationalthoughthedifferencesarenotextreme(notetheyaxisdivisions

    areonly200KAF).Again,whetherornottheLowerBasincanrealisticallyexpecttosurmount

    thelegalandpoliticalhurdlesassociatedwithenforcingeitherdeliveryobligationisastrategic

    considerationthatcannotbeshownquantitatively.IntheDemandCapscenario,theLower

    Basin

    is

    not

    required

    to

    pursue

    (or

    prevail

    in)

    such

    litigation.

    TheotherkeystrategicconsiderationfortheLowerBasinistheeffectoftheDemandCapon

    watersupplyreliability.ThePDF(Figure5)showsvirtuallynosignificantdifferencesin

    reliabilityovermostoftheruns,withthenotableexceptionofthelowesttailwhichshowshow

    theDemandCapshiftssomeoftheclimaterisktotheLowerBasin.Thisisaninherentand

    predictableconsequenceofeasingsomeoftheclimateriskontheUpperBasin(explained

    earlierandshowninFigure1).TheDemandCapisassumedtoamelioratethisconcernby

    betterprotectingreservoirstorage,thesubjectofthefollowingsetoffigures.

    ReservoirStorage

    TheimpactoftheDemandCaponreservoirstorageisconsistentlypositivei.e.,betterthan

    eitherBaselinescenario,andespeciallynotableinthelateryearsoftheruns.AverageLake

    Meadelevation,forexample,isroughly20feethigherintheDemandCapscenariothanthe7.5

    MAF/year(75Prot22)scenarioby2060(Figure6).ThestoryforLakePowellisalso

    consistentlypositive,inthattheDemandCapresultsingreaterstoragethaneitherBaseline

    (Figure7).

    NotethatFigure7alsoshowstheimpactofasinglecapi.e.,justanUpperBasincapas

    originallyproposedonreservoirstorage.Thedoublecapwasutilizedinthismodelingfor

    fearthat,withouttheLowerBasincap,anygainsinLakePowellreservoirstoragemightbelost

    tosurplususesdownstream.Figure8showsthesefearswereprobablyoverblown,asno

    discernibleimpactisseenforLakePowell.

    Conclusions

    Overall,the

    modeling

    of

    the

    Demand

    Cap

    shows

    that,

    compared

    to

    the

    statusquo,this

    institutionalreformcan(a)betterbalancetheriskofwatersupplyperturbationsassociated

    withclimatechangebetweentheUpperandLowerBasins,(b)eliminatemanysignificantlegal

    uncertainties,and(c)protectandenhancereservoirstorage,allwhilehavingmodestimpacts

    onwateravailableforconsumptiveuseinbothbasins.Whetherornotthisisviewedasan

    improvementoverthestatusquoisamatterofpersonaljudgment,andrestsonassumptions

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    15

    aboutwhatthestatusquomightactuallyentail.Itisworthnotingthat,formodelingpurposes,specifyingtheBaseline(statusquo)scenariosprovedmuchmoredifficultthantheDemandCap,whichisapowerfulreminderthatsignificantlegalomissionsandambiguitiesexistinthe

    LawoftheRiverduringperiodsofwaterscarcity.

    Thatagovernance

    reform

    can

    mitigate

    against

    both

    hydrologic

    (climate

    change)

    and

    legal

    uncertaintiesisevidencethatthisclassofreformsneedtobeconsideredprominentlyinthe

    searchforsolutions,despitetheiromissionintheBasinStudyanalysisandthehesitancyof

    manypartiestodiscussmattersoflawandpolitics.Thefactis,thethornylegalandpolicy

    issuesthatexistwillatsomepointdemandresolution,andthetimetodothatisbeforethe

    reservoirsareemptyandthespecterofaCompactcallhastakencenterstage.Conceptually,

    solutionsthatprotecttheCompactfromlegalchallengesshouldhavebroadappeal;the

    DemandCapisonepathwaytothatfuture.