The Meteor Crater Experiment METCRAX 2006
Transcript of The Meteor Crater Experiment METCRAX 2006
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The Meteor Crater ExperimentThe Meteor Crater ExperimentMETCRAX 2006METCRAX 2006
©© John S. SheltonJohn S. Shelton
An Upcoming Study of Boundary Layer EvolutionAn Upcoming Study of Boundary Layer Evolutionand and SeichesSeiches in Arizonain Arizona’’s Meteor Craters Meteor Crater
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CoCo--authorsauthors
Dave Whiteman
University of Utah
Dave Fritts
Northwest Research Associates, Inc.
Andreas Muschinski
U. Massachusetts
Sharon Zhong
Michigan State University
Sebastian Hoch
University of Utah
Maura Hahnenberger
University of Utah
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Past Field Experiments
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METCRAX overviewMETCRAX overview
3 year meteorological research program 3 year meteorological research program supported by NSF grants to the 4 PIs and supported by NSF grants to the 4 PIs and through field support from NCARthrough field support from NCARField phase: October 2006 Field phase: October 2006 ---- Continuous Continuous measurements during month + ~8 intensive measurements during month + ~8 intensive observational periods (IOPs) in which observational periods (IOPs) in which tethersondes and rawinsondes will be flowntethersondes and rawinsondes will be flownNumerical modeling and analysis (mesoscale Numerical modeling and analysis (mesoscale numerical model, LES, DNS)numerical model, LES, DNS)
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METCRAX ObjectivesMETCRAX ObjectivesInvestigate the diurnal buildup and Investigate the diurnal buildup and breakdown of basin temperature breakdown of basin temperature inversions or cold air pools and the inversions or cold air pools and the associated physical and dynamical associated physical and dynamical processes.processes.Determine the role that basinDetermine the role that basin--scale scale seiches and internal waves play in seiches and internal waves play in transport and mixing in basin stable transport and mixing in basin stable layerslayers
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MotivationMotivationPhysical processes leading to boundary Physical processes leading to boundary layer evolution are poorly understood in layer evolution are poorly understood in complex terraincomplex terrainThis has led to forecasting problemsThis has led to forecasting problemsImproved understanding of the basic Improved understanding of the basic physics may lead to better forecastsphysics may lead to better forecastsUnderstanding of physics may be easier in Understanding of physics may be easier in simple laboratorysimple laboratory--like conditionslike conditions
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Basins and air pollutionBasins and air pollution
AustriaAustria’’s Klagenfurt basins Klagenfurt basin
Salt Lake Basin, UtahSalt Lake Basin, Utah
Vail, ColoradoVail, Colorado
Helmut Helmut DitschDitsch drawingdrawing
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StratusStratus
Craig Clements photoCraig Clements photo
Salt Lake Valley from Alta, Jan 2004Salt Lake Valley from Alta, Jan 2004
Axel Axel HennigHennig photophoto
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WellWell--formed basinsformed basinsnear Mauna Loa, Hawaiinear Mauna Loa, Hawaii
Kennecott copper Kennecott copper mine nr SLC, UTmine nr SLC, UT
Meteor Crater,AZ
Nature Conservancy photoNature Conservancy photo
GruenlochBasin
©© Bernhard Bernhard PospichalPospichal
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©© John S. SheltonJohn S. Shelton
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©© John S. SheltonJohn S. Shelton
Uniform rim heightUniform rim heightOn a flat plainOn a flat plain
No largeNo large--scale advectionscale advectionThe The ““rightright”” sizesize
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The craterThe crater
165 m depth165 m depth
1.2 km diameter1.2 km diameter
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Cold Pool Buildup/BreakupCold Pool Buildup/Breakup
Determine physical processes that govern Determine physical processes that govern boundary layer evolutionboundary layer evolution
Slope flowsSlope flowsRadiativeRadiative transfer (longtransfer (long-- and shortand short--wave)wave)Turbulent transferTurbulent transferAsymmetries in Asymmetries in blbl structure and evolutionstructure and evolutionAmbient flows above basinAmbient flows above basin
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Preliminary measurements Preliminary measurements --Temperature InversionsTemperature Inversions
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SeichesSeiches/Gravity Waves/Gravity Waves
SeichesSeiches: : ““standing waves in enclosed or standing waves in enclosed or partially enclosed bodies of waterpartially enclosed bodies of water”” have been have been observed in lake basins, reservoirs, bays, etc.observed in lake basins, reservoirs, bays, etc.Basin cold pools may exhibit oscillations Basin cold pools may exhibit oscillations similar to a basin of water. These resonant similar to a basin of water. These resonant modes might occur in a basin disturbed by modes might occur in a basin disturbed by wind or atmospheric pressure oscillations.wind or atmospheric pressure oscillations.
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Dr. Tom Horst, ISFFDr. Tom Horst, ISFFDr. Bill Brown, ISSDr. Bill Brown, ISS
NCAR field support:NCAR field support:
Equipment transport:Equipment transport:
AirwestAirwest Helicopters,Helicopters,Glendale, AZGlendale, AZ
Site permissions:Site permissions:BarringerBarringer Crater Co.Crater Co.Meteor Crater EnterprisesMeteor Crater Enterprises
ISSISS
ISFFISFFHOBOHOBOTethered balloon Tethered balloon sounding systemsounding system
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Inside the craterInside the craterContinuous observations:Continuous observations:
Two lines of Two lines of HOBOsHOBOs7 ISFF towers7 ISFF towers
IOP operations:IOP operations:3 tethersondes make occasional up3 tethersondes make occasional up--down soundings down soundings to 500 ft above crater rim from ~3 pm to ~10 amto 500 ft above crater rim from ~3 pm to ~10 am
Outside the craterOutside the craterContinuous observations:Continuous observations:
Radar profiler/RASSRadar profiler/RASS and and Doppler Doppler sodarsodar/RASS/RASS
IOP operations:IOP operations:RawinsondesRawinsondes at 3at 3--h intervalsh intervals
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Installing InstrumentationInstalling Instrumentation
Installing HOBOs
Helicopter Operation Inside the Crater
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ConclusionsConclusions
METCRAX, October 2006METCRAX, October 2006Boundary layer structure evolutionBoundary layer structure evolutionSeichesSeichesResults to be presented at next Mountain Results to be presented at next Mountain Meteorology ConferenceMeteorology Conference