intromountainwxclimate-fall2017 · 2017-08-10 · weather and topography form two sides of the fire...

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8/10/17 1 Introduction to Mountain Weather and Climate Atmos 6250: Mountain Meteorology Jim Steenburgh Department of Atmospheric Sciences University of Utah [email protected] Reading Meyers, M., and W. J. Steenburgh, 2013: Mountain weather prediction: Phenomenological challenges and forecast methodology. Mountain Weather Research and Forecasting: Recent Progress and Current Challenges. T. Chow, S. de Wekker, and B. Snyder, Eds., Springer, 1–34. Beniston, M., 2003: Climate change in mountain regions: A review of possible impacts. Climatic Change, 59, 5–31. Questions How much of the Earth’s land surface is covered by mountains? What fraction of the Earth’s population lives in mountainous areas? Global Relief Topology* *Does not include glaciated areas of Greenland and Antarctica Source: Meybeck et al. (2001), Mountain Research and Development Global Relief Topology Source: Meybeck et al. (2001), Mountain Research and Development Plains 14.2% Mid-Altitude Plains 8.4% High-Altitude Plains 2.6% Lowlands 11.4% Rugged Lowlands 3.2% Platforms 14.4% Low Plateaus 8.3% Mid-Altitude Plateaus 3.4% High Plateaus 0.5% Very High Plateaus 0.5% Hills 8.7% Low Mountains 9.8% Mid-Altitude Mountains 10.3% High Mountains 3.0% Very High Mountains 1.4% Global Relief Topology Source: Meybeck et al. (2001), Mountain Research and Development Mountains Only 24.5% Mountains & Hills 33.2% Mountains, Hills, & Plateaus 45.9%

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Page 1: IntroMountainWxClimate-Fall2017 · 2017-08-10 · Weather and topography form two sides of the fire environment triangle and play an important role in generating extreme fire behavior

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IntroductiontoMountainWeatherandClimate

Atmos 6250:MountainMeteorologyJimSteenburgh

DepartmentofAtmosphericSciencesUniversityofUtah

[email protected]

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.