intromountainwxclimate-fall2017 · 2017-08-10 · weather and topography form two sides of the fire...
TRANSCRIPT
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IntroductiontoMountainWeatherandClimate
Atmos 6250:MountainMeteorologyJimSteenburgh
DepartmentofAtmosphericSciencesUniversityofUtah
Reading
Meyers,M.,andW.J.Steenburgh,2013:Mountainweatherprediction:Phenomenologicalchallengesandforecast
methodology.MountainWeatherResearchandForecasting:RecentProgressandCurrentChallenges.T.Chow,S.deWekker,
andB.Snyder,Eds.,Springer,1–34.
Beniston,M.,2003:Climatechangeinmountainregions:Areviewofpossibleimpacts.ClimaticChange,59,5–31.
Questions
HowmuchoftheEarth’slandsurfaceiscoveredbymountains?
WhatfractionoftheEarth’spopulationlivesinmountainousareas?
GlobalReliefTopology*
*DoesnotincludeglaciatedareasofGreenlandandAntarctica
Source:Meybeck etal.(2001),MountainResearchandDevelopment
GlobalReliefTopology
Source:Meybeck etal.(2001),MountainResearchandDevelopment
Plains 14.2%
Mid-AltitudePlains8.4%
High-AltitudePlains 2.6%
Lowlands 11.4%
RuggedLowlands3.2%
Platforms 14.4%LowPlateaus 8.3%
Mid-AltitudePlateaus 3.4%
HighPlateaus 0.5%
VeryHighPlateaus0.5%
Hills 8.7%
LowMountains9.8%
Mid-AltitudeMountains 10.3%
HighMountains3.0%
VeryHighMountains1.4%
GlobalReliefTopology
Source:Meybeck etal.(2001),MountainResearchandDevelopment
MountainsOnly24.5%
Mountains&Hills33.2%
Mountains,Hills,&Plateaus45.9%
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Plains 17.8%
Mid-AltitudePlains2.8%
High-AltitudePlains 0.6%
Lowlands 12.3%
RuggedLowlands5.5%
Platforms 10.0%LowPlateaus 4.3%
Mid-AltitudePlateaus 1.4%
HighPlateaus 0.1%
VeryHighPlateaus0.2%
Hills 13.1%
LowMountains14.8%
Mid-AltitudeMountains 12.5%
HighMountains3.4%
VeryHighMountains 1.3%
GlobalRunoff(Internal&External)
Source:Meybeck etal.(2001),MountainResearchandDevelopment
Topologyvs Runoff
Source:Meybeck etal.(2001),MountainResearchandDevelopment
MountainsOnly24.5%
Mountains&Hills33.2%
Mountains,Hills,&Plateaus45.9%
MountainsOnly32.0%
Mountains&Hills45.1%
Mountains,Hills,&Plateaus51.1%
Topology
Runoff
Plains 16.59%
Mid-AltitudePlains3.32%
High-AltitudePlains 0.53%
Lowlands 15.23%
RuggedLowlands8.68%
Platforms 9.26%LowPlateaus4.33%
Mid-AltitudePlateaus 2.16%
HighPlateaus0.46%
VeryHighPlateaus0.16%
Hills 13.29%
LowMountains10.71%
Mid-AltitudeMountains 9.65%
HighMountains3.78%
VeryHighMountains 1.84%
GlobalPopulation
Source:Meybeck etal.(2001),MountainResearchandDevelopment
Runoffvs.Population
Source:Meybeck etal.(2001),MountainResearchandDevelopment
MountainsOnly32.0%
Mountains&Hills45.1%
Mountains,Hills,&Plateaus51.1%
Runoff
Population
MountainsOnly26.0%
Mountains&Hills39.3%
Mountains,Hills,&Plateaus46.5%
KeyPoints• Mountains,hills,plateauscovernearlyhalf(45.9%)thegloballandsurfaceandcontainnearlyhalf(46.5%)oftheworld’spopulation
• Mountainsandhillsgenerateagreaterfractionofrunoffrelativetotheirareathanotherlandforms,servingasglobal“watertowers”
• Youdon’tneedtoliveinmountainsorhillstobeaffectedbytheirweather,climate,andhydrologicimpacts
©SLTrib/Galbraith
MountainWeatherHazardsandEconomics
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ForecastChallengesinMountainousRegions
• Extremetopography,hydrologic,meteorological,climatological,andsocio-economiccontrasts
• Sparseorunrepresentativeobservations
• Weatherforecastsmustbespatiallydetailed
• Manymodelspoorlyresolveoraccountforlocaltopographic,atmospheric,land-surface,ecologic,andhydrologicprocesses
Questions
Whatweather-relatedhazardsarestronglyinfluencedbyorography?
Weather-RelatedHazardsStronglyInfluencedbyOrography
• Floodsandflashfloods• Debrisflows• Wildland andurban-interfacefires• Airquality• Snowstorms• Icestorms• Avalanches• Highwinds(e.g.,downslope,gap)• Severeconvectivestorms(hail,flashfloods,etc.)• Transportationandroadmaintenance
Floods
• Producedbyprolongedprecipitationevents• Oftenassociatedwithorographicprecipitationenhancement
• Modulationofintensityandspatialdistributionofprecipitationbytopographycandeterminethecatchmentbasinsaffected
• Additionalfactorscanincludesnowmelt,ecology,etc.
Example:FrontRangeSep2013
Source:NOAA(2014,http://www.nws.noaa.gov/om/assessments/pdfs/14colorado_floods.pdf)
8Fatalities19,000homes/buildingsdamaged1,500homes/buildingsdestroyed$3Billioninlosses
BigThompsonCanyonBefore
Source:http://www.denverpost.com/2013coloradofloods/ci_24115527/before-after-photos-colorado-flood-2013
©DenverPost
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BigThompsonCanyonAfter
Source:http://www.denverpost.com/2013coloradofloods/ci_24115527/before-after-photos-colorado-flood-2013
©DenverPost
ImpactsAwayfromMountains
Source:http://www.denverpost.com/2013coloradofloods/ci_24115527/before-after-photos-colorado-flood-2013,Map:Google
©DenverPost
Evans,CO
FlashFloods
• Rapidfloodingoftenproducedbyheavyrainassociatedwithconvectivestorms(althoughthereareothermechanisms)
• Mountainscanplayarolebyinfluencingtheformationandmovement(orlackthereof)ofdeepconvectionandmesoscale convectivesystems
Example:RapidCityFlood1972
238killed3,000injured1335homesdestroyedDamfailurescontributedtolosses
Source:http://www.weather.gov/unr/1972-06-09
FlashFloodExample:BlackHills1972
Source:http://pubs.usgs.gov/fs/fs-037-02,PhotosbyPerryRahn
Impactsalsofeltawayfrommountains(RapidCity)
Weather-RelatedDebrisFlows
• Heavymountainprecipitationorsnowmeltleadstoawater-ladenmassofsoilandrockflowing(sometimesviolently)downamountainside
• Initiatedtypicallyonslopes>25degrees– Canmoveintolowerangleareas
• Majorconcernonfire-denudedslopes
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Thistle,UTSlideofApril1983
Source:http://geochange.er.usgs.gov/sw/changes/natural/elnino/
4millionm3 ofdebris
ProducedlakethatfloodedThistle,UT-6,UT-89,andrailroad
Lakedrainedbytunneling
$400+Millionindamage
MostexpensivelandslideinUShistory
Easytoseetoday!
Wildland Fire
Weatherandtopographyformtwosidesofthefireenvironmenttriangleandplayanimportantroleingeneratingextremefirebehavior
Source:COMET
BiggerandMoreFrequentFires
Largewildfireactivityincreasedsuddenlyandmarkedlyinthemid-1980s,withhigherlarge-wildfirefrequency,longer
wildfiredurations,andlongerwildfireseasons.Thegreatestincreasesoccurredinmid-elevation,NorthernRockiesforests,whereland-usehistorieshaverelativelylittleeffectonfirerisksandarestronglyassociatedwithincreasedspringandsummertemperaturesandanearlierspringsnowmelt.
- Westerling etal.(2006),Science
Trends1984–2011byEcoregion
Source:Dennisonetal.(2014),GRL
BillionDollarWildfireDisasters• Oakland1991• CaliforniaFall1993• WesternUS1994• WesternUS2000• WesternUS2002• California2003• WesternUS2006• WesternUS2007• WesternUS2008• WesternUS2009• TX–NM-AZ2011• WesternUS2012• Valley-ButteFiresCA2015• WesternUS2015• Gatlinburg,TN2016
SanDiego,CA,Oct2003
Source:https://www.ncdc.noaa.gov/billions/,Photo:http://interwork.sdsu.edu/fire/purpose.htm
AirQuality
Pollutantsfrequentlytrappedinbasinsandvalleys,leadingtopoorairqualityepisodes
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Source:http://www.lung.org/our-initiatives/healthy-air/sota/city-rankings/most-polluted-cities.html
MostPollutedCities(PM2.5Episodes)
WesternUSBasinsandValleys
Snowstorms
• Mountainsaffectintensityanddistributionofsnowfall,aswellassnowlevelsthroughtheblockingandchannelingofairmasses
• Canbewidespreadorhighlylocalized
2003FrontRangeBlizzard
Source:http://www.pieglobal.com/statistics-and-observations-on-the-colorado-blizzard-of-2003/http://www.ucar.edu/communications/newsreleases/2004/blizzard.html(photobyCarlye Calvin)
March16–20,2003Upto5feetofsnow,lossesof>$300millionduelargelytoroofcollapses
IceStorms
• Mountainsaffecttheblocking,damming,andchannelingofshallow,coldairmasses,contributingtothedevelopmentofthermodynamicprofilesfavorableforsleetorfreezingrain
NorthAmericanIceStormof1998
Photos:JohnFergusonandEnvironmentCanada
January5–91998NortheastUSandeasternCanada
100+mmoffreezingraininsomeareas$4+Billionindamage
Channelingbyorographycritical(Roebber andGyakum 2003,MWR)
Avalanches
Weatherandtopographyformtwosidesoftheavalanchetriangle
Source:http://www.avalanche-center.org/
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Avalanches
Source:http://avalanche.state.co.us/accidents/statistics-and-reporting/
LittleCottonwoodCanyon
Image:Steenburgh(2014),CourtesyAdamNaisbitt
“Basedondatafromthe1991/92skiseason,theestimatedrevenuelossforskiresortsinupperLCCduringtheclosureofSR-210foravalanchehazardis$1.4millionday-1
[$2.3millionday-1 in2013dollars(Blattenberger andFowles 1995)]”– CampbellandSteenburgh(2014)
Little Cottonwood Canyon, 23 Dec 1988 (Courtesy National Weather Service)
HighWinds
• Mountainscanproducelocalflowaccelerationsanddamagingwinds
• Examplesincludegapwindsanddownslopewinds
• Inadditiontoconcernsforstructures,terrain-inducedturbulenceandrotorsareamajorhazardforaircraft
DownslopeWinds
Source:http://www.atmos.washington.edu/Atlas/phot_oro09.html,PhototakenbyRobertSymons&courtesyMortonG.Wurtele
DownslopewindandrotorcloudovertheOwensValleyeastoftheSierraNevada
SevereConvectiveStorms
• Yes,theseoccurinthemountainstoo
• Inaddition,theseverestormenvironmentofthehighplainsandportionsofEuropeandSouthAmericaarestronglyinfluencedbyregionaltopographiceffects
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TetonTornado
Source:Fujita(1989,MWR)
F4CrossedContinentalDivide@3070m
Damageswath39.2kmlongand2.5kmwide
TransportationandRoadMaintenance
• 70%ofUSroadsinsnowyregionsthatreceive13cmormoreofsnowayear
• 24%ofUSweather-relatedvehiclecrashesoccuronsnowy,slushy,oricypavement
• 15%occurduringsnowfallorsleet• 1,300fatalites/yr onsnowy,slushy,oricypavement• 116,800injuriesperyearonsnowy,slushy,oricypavement• Winterroadmaintenanceaccountsfor20%ofstateDOT
maintenancebudgets• Stateandlocalagenciesspendmorethan$2.3billiononsnowand
icecontrol• Notallmountainweatherrelated,butillustratesimportanceof
winterweather
Source:http://www.ops.fhwa.dot.gov/weather/weather_events/snow_ice.htm
MountainWeatherNotAllBad!
AvenuesFoothills,29November2010
MountainWeatherEconomics
• Outdoorrecreationgenerates– IntheUS• $646billioninconsumerspending• 6.1milliondirectjobs
– InthewesternUSincludingAlaskaandHawaii• 197.5billioninconsumerspending• 1.8milliondirectjobs• $61.1billioninsalariesandwages
Source:https://outdoorindustry.org/research-tools/outdoor-recreation-economy/,16Aug2015
SkiingandSnowboarding
• $7.5BillionindirectspendingatUSresorts• 57millionUSresortvisitsperyear• Backcountrygearnow~8%ofequipmentsales• Highlysensitivetoweatherandclimatevariability
Source:https://www.nsaa.org/,http://www.snowsports.org/research-surveys/snow-sports-fact-sheet/,16Aug2015
MountainsRegionsandGlobalWarming
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Questions
Whydowecareaboutclimatechangeinthemountains?
Whatdoyouthinksomeoftheimpactsofclimatechangewillbeinmountainous
regions?
ImportanceofMountains
• 40%oftheglobalpopulationlivesinwatershedsoriginatingfrommountains
• Mountainsareoftenecologicalislandswithuniquespeciesandstrongecosystemgradients
• Mountainsarepopularareasforecotourism
Source:Beniston (2003)
PotentialImpactsofClimateChangeinMountainousRegions
• Hydrology:Shiftsindistribution,seasonality,amount,andtype(e.g.,rainorsnow)ofprecipitationandrunoff
• Ecology:Shiftsandlossesofvegetation,forests,andbiodiversity
• HumanHealth:Shiftsinvector-bornediseases
• Tourism:Beneficialandadverseeffects
Source:Beniston (2003)
HydrologicConsequences• Moreprecipitationfallingasraininsteadofsnowin
areasnearthemeltingpointduringwinter
• Moresnowfallinsomecolder,highaltitudeandhighlatitudeareaswithfirstfewdegreesofwarming– Eventuallynearlyallaltitudeslose
• Substantiallossesofmostmountainglaciers
• Runoffchangesthatrequiringmitigationandadaption(easierforadvancedthandevelopingcountries)
Source:Beniston (2003)
ProjectionsforTschierva Glacier,Switzerland
Source:Beniston (2003),Courtesy:MaxMaisch,UniversityofZurich
EcosystemConsequences• Multifaceted– Likelylossofcoldestclimate/ecosystemzonesatmountainpeaks
– Migrationofsomespecieshigher– Lossofsomespeciesduetoadverseclimaticchangeandinvasivespecies• E.g.,troutcanonlygosohigh
– Survivalofsomespeciesinexistinghabitatareasduetolowerclimate-changesensitivity
• Insomeinstances,ecosystemdisturbanceisorwillhaveastrongerinfluencethanclimatechange
Source:Beniston (2003)
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HumanHealth
• Vector-bornediseaseslikemalariamaybecomemoreprevalentinsomemountainousandhighlandregions
Source:Beniston (2003)
ChangesintheincidencerateofMalariafora1°CtemperatureincreaseGreydenotesinvasionareasthatare
currentlymalariafree
Tourism• Directimpacts:Changesintheclimaticconditions
necessaryforrecreationactivities
• Indirectimpacts:Changestomountainlandscapesandsocio-economicshiftsindemandforactivitiesanddestinations
• Thesevarygeographicallyandbysector
• Maybeadverse(lossofsnowforskiing)andbeneficial(e.g.,longerhikingseason)
Source:Beniston (2003)
WinterSportsinNortheastUS• UnderA1Fiscenario(fossil-fuel
intensive)by2070–2099– Reliablesnowmobileseasons(>50days)virtuallyeliminated
– Only4of14geographicallydistributedskiareascanmaintaina100-dayskiseason(withmuchgreatersnowmakingrequirements)
– Consideranalysistobeconservative
Source:Scott(2008,Mitig.Adapt.Strat.Glob.Change)
Summary
• Mountainweatherimpactsarediverseandextendawayfrommountainousregions
• Globalwarmingwillhaveimportantimpactsonmountainclimate,ecology,humanhealth,andtourismthataremainlyadverse,butinsomecasesbeneficial
• Moreinthelecturestocome!
ReferencesBeniston,M.,2003:Climatechangeinmountainregions:Areviewofpossibleimpacts.ClimaticChange,59,5–31.
Blattenberger,G.,andR.Fowles,1995:Roadclosuretomitigateavalanchedanger:AcasestudyforLittleCottonwoodCanyon.Int.J.Forecasting,11,159–174,doi:10.1016/0169-2070(94)02008-D.
Dennison,P.E.,S.C.Brewer,J.D.Arnold,andM.A.Moritz,2014:LargewildfiretrendsinthewesternUnitedStates,1984–2011.Geophys.Res.Lett.,DOI10.1002/2014GL059576.
Fujita,T.T.,1989:TheTeton–Yellowstonetornadoof21July1987.Mon.Wea.Rev.,117,1913–1940.
Meyers,M.,andW.J.Steenburgh,2013:Mountainweatherprediction:Phenomenologicalchallengesandforecastmethodology.MountainWeatherResearchandForecasting:RecentProgressandCurrentChallenges.T.Chow,S.deWekker,andB.Snyder,Eds.,Springer,1–34.
Meybeck,M.,P.Green,andC.Vorosmarty,2001:Anewtypologyformountainsandotherreliefclasses:Anapplicationtoglobalcontinentalwaterresourcesandpopulationdistribution.MountainResearchandDevelopment,21,34–45.
NOAA2014:TherecordfrontrangeandeasternColoradofloodsofSeptember11–17,2013.Availableathttp://www.nws.noaa.gov/om/assessments/pdfs/14colorado_floods.pdf.
Roebber,P.J.,andJ.R.Gyakum,2003:Orographicinfluencesonthemesoscale structureofthe1998IceStorm.Mon.Wea.Rev.,131,27–50.
Scott,D.,J.Dawson,andB.Jones,2008:ClimatechangevulnerabilityoftheUSNortheastwinterrecreation–tourismsector.Mitig.Adapt.Strat.Glob.Change,13,577–596.
Steenburgh,W.J.,2014:SecretsoftheGreatestSnowonEarth.UtahStateUniversityPress.186pp.