The Seeley and Clay Springs Fires - Impacts on Water Supply

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  • 7/28/2019 The Seeley and Clay Springs Fires - Impacts on Water Supply

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    April1Update

    TheSeeleyFireandPotentialImpactsonHuntingtonCreekWaterSupplyClaySpringsFireandPotential

    ImpactsonOakCreekWaterSupply

    TheSeeleyFire

    TheSeeleyfireburnedabout48,000acresincentralUtahsouthofScofieldinJulyof2012,including18,500

    acresof

    the

    Huntington

    Creek

    Watershed

    just

    below

    Electric

    Lake

    in

    the

    bottom

    half

    of

    the

    basin.

    This

    constitutesnearlyhalf(46%)ofthetotalwatershedareaof40,100acres.

    Figure1.BurnedportionoftheHuntingtonCreekWatershed.

    TheimpactfireshaveonwatersupplyandstreamflowinhighreliefareasoftheintermountainWestcanbe

    complex.Generallyinthefirstfewyearsafterafire,snowmeltcanbeaccelerateddueto:(1)

    carbon/dust/organicmaterialdepositiononthesnowsurface;(2)thevolumeofstandingblackenedtimber

    changingthealbedo(reflectivity)ofthesnowpack;and(3)thereductionincanopycoverinareasthat

    formerlysustainedevergreenforest.Snowmeltcanconsequentlybeadvancedasmuchas6weeks,ormore.

    Theseconditionscanalsoleadtogreatersnowpacklossestowinderosionandsublimation. Conversely,the

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    lackofforestcovercanincreasetheamountofsnowonthegroundthatwouldnormallybeinterceptedbythe

    forestcanopy,and,particularlyinthedecadeortwoafterthefire,mayleadtohigheroverallAprilJulystream

    flow. However,inthefirstfewpostfireyearswithlowsnowpacksandwithlongperiodsbetweenstorms,the

    neteffectcanbeloweroverallsnowwaterequivalentonthegroundwithearlymelt.Someoftherunoffthat

    wouldnormallyhaveoccurredintheAprilJulytimeframecouldhappeninMarchorearlier.

    HuntingtonCanyon,southfacingaspectwithallsnowpackmelted.

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    Patchysnowonnorthandeastfacingaspects.

    WatersupplyforecastmodelsaregearedtopredicttheAprilJulyrunoffseasonbasedonobservedsnowpack

    andothervariables. TherearenodatasitesinsidetheHuntingtonCreekburnareaanddatausedinthe

    hydrologicmodelsarefromnonimpactednearbysites.Assuch,weanticipatethatrunoffonHuntington

    Creekwillbeshiftedtoanearliertimeframeduetotheburnconditionsinthewatershedandthatthe

    AprilJulyforecastislikelytooverestimatetheAprilJulystreamflow.Theseconditionscouldpersistfor

    severalyears.ItisalsoimportanttonotethattheinflowtoElectricLakeabovetheburnareawillnotbe

    impacted.

    Withsolittlesnowlefttomeltontheburnareathereislittleprobabilityofseriouserosionormasswasting

    phenomenafromthefirearea. Theremainingsnowislikelytomeltinsmalldailyincrementsandinfiltratethe

    soilsoverthenextmonthorso.Intenseprecipitationeventscouldtriggermudanddebrisflowsfromthe

    burn.

    WaterusersthatrelyonHuntingtonCreekareadvisedthattheAprilJulyflowwilllikelybelessthanthe50%

    exceedancenumberandforplanningpurposesareadvisedtousealowerfiguresuchasthe70%exceedance

    number.

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    PRI CE SAN RAFAELStr eamf l ow Forecasts - Apri l 1, 2013

    ==================================================================================================================================| || |

    For ecas t Poi nt For ecas t | ==================== Chance Of Exceedi ng * ====================== |Peri od | 90% 70% | 50% | 30% 10% | 30- Yr Avg.

    | ( 1000AF) ( 1000AF) | ( 1000AF) ( % AVG. ) | ( 1000AF) ( 1000AF) | ( 1000AF)====================================================================| =======================| =====================================Fi sh Ck ab Reser voi r nr Scof i el d APR- J UL 9. 3 13. 1 | 16. 0 53 | 19. 2 25 30

    | |Pri ce R nr Scof i el d Reser voi r ( 2) APR- J UL 10. 1 15. 6 | 20 49 | 25 33 41

    | |Whi t e R bl Tabbyune Cr eek APR- J UL 2. 4 3. 9 | 5. 0 32 | 6. 3 8. 5 15. 5

    | |

    Gr een R at Gr een Ri ver, UT ( 2) APR- J UL 700 1050 | 1320 45 | 1630 2130 2960| |El ectr i c Lake I nfl ow ( 2) APR- J UL 2. 8 4. 5 | 6. 0 45 | 7. 7 10. 5 13. 3

    | |Hunt i ngt on Ck nr Hunt i ngt on ( 2) APR- J UL 10. 5 14. 7 | 18. 0 45 | 22 28 40

    InthisAprilreleasethe50%exceedancenumberforHuntingtonCreekis18,000acrefeetandthe70%

    exceedancefigureis14,700acrefeet.Theeasywaytoreadthistable:weare90%suretoget10.5KAFor

    higher,70%suretoget14.7KAF,50%toget18KAFandonly30%chanceofgetting22KAForhigher.Dueto

    theburnconditionsacrossthewatershednotcapturedbymodelinput;weadviseusingalowerforecast

    numbersuchasthe14.7KAFfigureinthisexample.

    TheClay

    Springs

    Fire

    (Oak

    Creek

    Watershed)

    TheClaySpringsfirenorthofDeltaburnedabout180,000acresinmidJulyof2012.Thisfirewas,inplaces,

    extremelyhotandburnedrootsbelowthegroundsurface.Theterraininthiseasttowestfacingwatershedis

    verysteepwithabout50%ofthewatershedonasouthfacingaspect. Nearlytheentirewatershed(99.6%)

    wasimpactedtosomedegreebythefire.

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    ClaySpringsfireperimetershowninred.

    TheOakCreekSNOTELsitewasdestroyedandlaterrebuilt,andiscurrentlygivinggoodinformationon

    snowpack,precipitation,

    temperature

    and

    soil

    moisture.

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    TheSNOTELsiteatOakCreekhascompletelymeltedoutsome3weeksearlierthanlastyearwithapproximatelythesameamountofsnowpack,illustratinghowburnedareasimpactmeltrates.(currentyearsnowpackblueline,2012,greenline)Thesiteisatanelevationof7800feetonasteepnorthfacingaspectandnormallyholdssnowwellintoMay.Atthispoint,thevastmajorityofthewatershedissnowfreeandsnowmeltrunoffisessentiallyoverfortheyear.

    ThesurfacesoilsattheOakCreekSNOTELsiteareshowingpossiblesignsofhydrophobicityorwaterrepellencyasthe2inchsoilmoisturesensor(greenline)refusestowetupsubstantiallyinspiteofthesite

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    meltingnearly7inchesofsnow. Thelowersensorsshowincreasedmoisturelikelyfromsourcesuphillfrom

    thesensors.SnowSurveypersonnelonsiteinlateMarchreportthatthesurfacesoilswereextremelydry

    eveninareasrecentlysnowcovered.Thisconditioncouldposeproblemsifhighintensityprecipitationevents

    occurlaterinspringandsummer.

    SouthfacingaspectoftheOakCreekWatershed.Dryanddustynorunofffromthisarea.

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    NorthfacingaspectoftheOakCreekWatershedwheretheSNOTELsiteislocated.

    ThisphotowastakenafewdayspriortowhentheSNOTELsitemeltedoutandiscurrentlybareofanysnow.

    WaterusersthatrelyonOakCreekareadvisedthattheAprilJulyflowwilllikelybelessthanthe50%

    exceedancenumberandforplanningpurposesareadvisedtousealowerfiguresuchasthe70%exceedance

    number.

    ==================================================================================================================================LOWER SEVI ER RI VER BASI N

    Str eamf l ow Forecasts - Apri l 1, 2013==================================================================================================================================

    | || |

    For ecas t Poi nt For ecas t | ==================== Chance Of Exceedi ng * ====================== |Peri od | 90% 70% | 50% | 30% 10% | 30- Yr Avg.

    | ( 1000AF) ( 1000AF) | ( 1000AF) ( % AVG. ) | ( 1000AF) ( 1000AF) | ( 1000AF)====================================================================| =======================| =====================================Sevi er R nr Gunni son APR- J UL 6. 4 34 | 52 53 | 70 98 99

    | |Chi cken Ck nr Levan APR- J UL 0. 05 1. 40 | 2. 40 53 | 3. 40 4. 50 4. 50

    | |Oak Cr eek nr Oak Ci t y APR- J UL 0. 09 0. 20 | 0. 30 18 | 0. 42 0. 63 1. 66

    InthisAprilreleasethe50%exceedancenumberforOakCreekis300acrefeetandthe70%exceedancefigure

    is200acrefeet.Theeasywaytoreadthistable:weare90%suretoget90KAForhigher,70%suretoget200

    KAF,50%toget300KAFandonly30%chanceofgetting420KAForhigher.Duetotheburnconditionsacross

    thewatershednotcapturedbymodelinput,weadviseusingalowerforecastnumbersuchasthe90orthe

    200KAFfigureinthisexample. Theseforecastfiguresaredramaticallylowerthanthoseissuedlastmonthdue

    tothehugedeclineinsnowpackacrossthewatershed.