How the shape of sand dune indicate the wind direction延伸文章資訊,搜尋引擎最佳文章推薦
1. Sand dune
Lighter winds blow from several different directions, and the dunes, being of ... repetition of dune shapes and spacings when they are close together indicate that ...SandduneSectionsArticleIntroductionGeomorphiccharacteristicsSandsWindsFormationandgrowthofdunesDuneandsheetpatternsFixeddunesinsemiaridregionsShowmoreMediaVideosImagesAdditionalInfoAdditionalReadingMoreArticlesOnThisTopicContributorsArticleHistoryLoadPreviousPageWindsWindshavethreesourcesofvariationthatareimportant—namely,direction,velocity,andturbulence.Mostofthegreatdesertsarefoundinthesubtropicalareasofhighatmosphericpressure,wherethewindscirculateinaclockwisedirectionintheNorthernHemisphereandacounterclockwisedirectionintheSouthernHemisphere.Thehigh-pressuresystemstendtodipdowntotheeastsothatwindsarestrongerthere,apatternmirroredbythedunes.PolewardofthesecirculationsystemsarethezonesofeastwardmovingdepressionsinwhichtherearegenerallywesterlywindsthatmoldthedunesoftheNorthAmericanandCentralAsiandesertsandofthenorthernSahara.Theboundariesbetweenthesetwocirculationsystemsmigratebackandforthseasonally,sothatcomplicateddunepatternsarefoundinthezonesofoverlap.Onlyafewdeserts,notablytheTharDesertofIndiaandtheSonoranDesertoftheAmericanSouthwest,areaffectedbymonsoonalwindsystems.Somedunesarebuiltbyseabreezesandlocalwinds,asincoastalPeru.Thedirectionofthewindatanyoneplaceinthedesertisaffectedbyanumberoflocalfactors.Windsareparticularlychanneledaroundtopographicalfeatures,suchastheTibestiMassifintheSahara,sothatdunesareaffectedbydifferentwindsondifferentsidesoftheobstruction.Windsalsocanbechanneledaroundthedunesthemselves,therebydevelopingpatternsofsecondaryflowthatmodifytheshapesofthedunes.Thepatternofwindvelocityalsoisimportant.Likemanynaturalphenomena,windvelocitieshavealog-normaldistribution:therearealargenumberofmoderatebreezesandadiminishingnumberofincreasinglymoreviolentwinds.Thegreatestvolumesofsandareprobablymovedbyunusuallystrongwinds,becausetheamountofsandmovedbywindisapowerfunction(exponentialfact
2. Types of Dunes
These dunes form under winds that blow from one direction, and they also are ... The largest crescentic dunes on Earth, with mean crest-to-crest widths ... Straight or slightly sinuous sand ridges typically much longer than they ...RipplesonaduneinEurekaValley,California(photographbyTerrenceMoore).AworldwideinventoryofdesertshasbeendevelopedusingimagesfromtheLandsatsatellitesandfromspaceandaerialphotography.Itdefinesfivebasictypesofdunes:crescentic,linear,star,dome,andparabolic.ThemostcommonduneformonEarthandonMarsisthecrescentic.Crescent-shapedmoundsgenerallyarewiderthanlong.Theslipfaceisonthedune'sconcaveside.Thesedunesformunderwindsthatblowfromonedirection,andtheyalsoareknownasbarchans,ortransversedunes.Sometypesofcrescenticdunesmovefasteroverdesertsurfacesthananyothertypeofdune.Agroupofdunesmovedmorethan100metersperyearbetween1954and1959inChina'sNingxiaProvince;similarrateshavebeenrecordedintheWesternDesertofEgypt.ThelargestcrescenticdunesonEarth,withmeancrest-to-crestwidthsofmorethan3kilometers,areinChina'sTaklimakanDesert.ThesecrescenticdunesofcoastalPeruaremigratingtowardtheleft(photographbyJohnMcCauley).Straightorslightlysinuoussandridgestypicallymuchlongerthantheyarewideareknownaslineardunes.Theymaybemorethan160kilometerslong.Lineardunesmayoccurasisolatedridges,buttheygenerallyformsetsofparallelridgesseparatedbymilesofsand,gravel,orrockyinterdunecorridors.SomelineardunesmergetoformY-shapedcompounddunes.Manyforminbidirectionalwindregimes.Thelongaxesofthesedunesextendintheresultantdirectionofsandmovement.LineardunesadvanceonsmallplayaseastofLakeEyreintheSimpsonDesertofcentralAustralia(photographbyC.Twidale).LineardunesinthewesterndesertsofEgypt(photographbyCarolBreed).Radiallysymmetrical,stardunesarepyramidalsandmoundswithslipfacesonthreeormorearmsthatradiatefromthehighcenterofthemound.Theytendtoaccumulateinareaswithmultidirectionalwindregimes.Stardunesgrowupwardratherthanlaterally.TheydominatetheGrandErgOrientaloftheSahara.Inotherdeserts,theyoccuraroundthema
3. Dunes
Dunes. In physical geography, a dune is a hill of sand built by either wind or ... superposed or coalesced forms, usually of barchanoid or linear shapes. ... Simple dunes represent a wind regime that has not changed in intensity or direction ...SkiptomaincontentEarthScienceDesertsSearchfor:DunesInphysicalgeography,a dune isahillofsandbuiltbyeitherwindorwaterflow.Dunesoccurindifferentformsandsizes,formedbyinteractionwiththeflowofairorwater.Mostkindsofdunesarelongeronthewindwardsidewherethesandispusheduptheduneandhaveashorter“slipface”intheleeofthewind.Thevalleyortroughbetweendunesiscalleda slack. A“dunefield”isanareacoveredbyextensivesanddunes.Largedunefieldsareknownasergs.Somecoastalareashaveoneormoresetsofdunesrunningparalleltotheshorelinedirectlyinlandfromthebeach.Inmostcasesthedunesareimportantinprotectingthelandagainstpotentialravagesbystormwavesfromthesea.Althoughthemostwidelydistributeddunesarethoseassociatedwithcoastalregions,thelargestcomplexesofdunesarefoundinlandindryregionsandassociatedwithancientlakeorseabeds.Dunesalsoformundertheactionofwaterflow(fluvialprocesses),andonsandorgravelbedsofrivers,estuariesandthesea-bed.Themodernword“dune”cameintoEnglishfromFrenchcirca1790.Inancienttimes,wordscognateto“dune”probablyhadthemeaningofabuilt-uphillorcitadelfortification.[1]ErgChebbi,Morocco ConservationDunehabitatsprovidenichesforhighlyspecialisedplantsandanimals,includingnumerousrarespeciesandsomeendangeredspecies.Duetowidespreadhumanpopulationexpansion,dunesfacedestructionthroughlanddevelopmentandrecreationalusages,aswellasalterationtopreventtheencroachmentofsandontoinhabitedareas.Somecountries,notablytheUnitedStates,Australia,Canada,NewZealand,theUnitedKingdom,andNetherlands,havedevelopedsignificantprogramsofduneprotectionthroughtheuseofsanddunestabilization.IntheU.K.,aBiodiversityActionPlanhasbeendevelopedtoassessduneslossandtopreventfuturedunesdestruction.SandblowingoffacrestintheKelsoDunesoftheMojaveDesert,California.AeolianduneshapesCrescentic“Crescent-sh
4. Phase diagrams of dune shape and orientation depending on ...
New evidence indicates that sand availability does not only control ... wind conditions, transverse linear dunes form where sand availability ...SkiptomaincontentThankyouforvisitingnature.com.YouareusingabrowserversionwithlimitedsupportforCSS.Toobtainthebestexperience,werecommendyouuseamoreuptodatebrowser(orturnoffcompatibilitymodeinInternetExplorer).Inthemeantime,toensurecontinuedsupport,wearedisplayingthesitewithoutstylesandJavaScript.AdvertisementnaturescientificreportsarticlesarticlePhasediagramsofduneshapeandorientationdependingonsandavailabilityDownloadPDFSubjectsGeodynamicsGeomorphologyAbstractNewevidenceindicatesthatsandavailabilitydoesnotonlycontroldunetypebutalsotheunderlyingdunegrowthmechanismandthesubsequentduneorientation.Herewenumericallyinvestigatethedevelopmentofbedformsinbidirectionalwindregimesfortwodifferentconditionsofsandavailability:anerodiblesandbedoralocalizedsandsourceonanon-erodibleground.Thesetwoconditionsofsandavailabilityareassociatedwithtwoindependentdunegrowthmechanismsand,forbothofthem,wepresentthecompletephasediagramsofduneshapeandorientation.Onanerodiblesandbed,lineardunesareobservedovertheentireparameterspace.Then,thedivergenceangleandthetransportratiobetweenthetwowindscontrolduneorientationanddynamics.Foralocalizedsandsource,differentdunemorphologiesareobserveddependingonthewindregime.Therearesystematictransitionsinduneshapefrombarchanstolineardunesextendingawayfromthelocalizedsandsourceandvice-versa.Thesetransitionsarecapturedfairlybyanewdimensionlessparameter,whichcomparestheabilityofwindstobuildthedunetopographyinthetwomodesofduneorientation.DownloadPDFIntroductionDuneshavebeenprimarilyclassifiedaccordingtotheirshapeconsideringbothsandavailabilityandwinddirectionalvariability1.ThewinddirectionalvariabilityisusuallymeasuredbytheRDP/DPdimensionlessparameter.Itistheratiobetweentheresultantdriftpotential(RDP,thenormofthemeansandfluxvector)andthedriftpotential(DP,themeanofthenormsoftheindividualsandfluxvectors).Inzonesoflowsandavail
5. (PDF) Analysis of sand dunes to determine wind direction and ...
The studies have shown that wind prevailing direction is eastern-north to western-south, the strong wind being in north-south direction. It can also ...ArticlePDFAvailableAnalysisofsanddunestodeterminewinddirectionanddetectsandsourcesites(casestudy:KhartooranErg,Iran)January2007Project:Thestudyofremoval(detachment)andtransitionalregionsofwinderosionupongroundindicator(Casestudy:KhartouranErg)Authors:NaserMashhadiUniversityofTehranHadiAhmadiUniversityofTehranMREkhtesasiMREkhtesasiThispersonisnotonResearchGate,orhasn'tclaimedthisresearchyet.SadatFeizniaUniversityofTehranShowall5authorsHideDownloadfull-textPDFReadfull-textDownloadfull-textPDFReadfull-textDownloadcitationCopylinkLinkcopiedReadfull-textDownloadcitationCopylinkLinkcopiedCitations(15)References(7)Figures(1)AbstractandFiguresWindregimeandsandgrainsizearetwoofthefactorsthatdeterminethemorphologyanddynamicsofsanddunesindesertareas.RegardingtheimportanceofwindeffectsonsanddunesespeciallyinIran,inthisstudy,KhartooranErgwasanalyzedtodeterminewinddirectionandtodetectsandsourcesites.KhartooranErgislocatedoneasternnorthofIranandliesinKhorasanRazaviandSemnanprovinces.TheareaofErgwasdeterminedbasedongeologicalandtopographicalmapsandsatelliteimages.Then,sanddunesofergwereclassified,basedonaerialphotographandsatelliteimageinterpretation.SandduneformsintheKhartooranErgareoftenbarchansandcombinationofbarchanicridges,buttherearealsocomplextypesoflinearsanddunes.Basedonfieldsurveyfindings,thestabilizedinthesouthernpartoftheErgwereseparated,becauseofthesesandduneshavingbeendeformed.Accordingtothepresentedmodelsrelationshipbetweenmorphologyandwinddirection,thesandduneswereanalyzed.Thestudieshaveshownthatwindprevailingdirectioniseastern-northtowestern-south,thestrongwindbeinginnorth-southdirection.ItcanalsobesaidthatsandduneswhicharelocatedintheadjacentofErgandaresimpleandseparatecanbeusedasthemostsuitablecriteriatodeterminepredominantwind.Also,regardingtheErglocationwithrespecttoupperplainsanddeterminedwinddirection,itcanben