简介:Inthestrapdowninertialnavigationsystem,theFiberOpticalGyro(FOG)musthavehighprecisiontogiveaccuratenavigationinformation.Inthispaper,adigitalclosedloopdetectionmethodbasedontherampwavemodulatingtechnigueisintroduced.DSPandFPGAhavemanyadvantagesindigitalsignalprocessing.Inthedesign,byusingDSP,acomplexarithmeticoperationiscompletedtomeettheneedsofclosedloopcontrolofFOGwithinashorttime.AllkindsofcontrolsignalsareproducedeasilybyFPGA,underwhichDSPcouldworkproperly.CombiningtheDSPandFPGA,thedetectingmethodisimplementedsuccessfully.Intheend,theresultoftestandperformanceisgiven.FromtheresultwecanconcludethattheprecisionofFOGisimprovedandthenoisesarelimitedtoalowlevel.
简介:XishuangbannaofYunnanProvinceisafamoustropicalfoggyregion.AfieldexperimentwascarriedoutfromNovember23to30of1997duringwhichfogsoccurredregularlyeveryday.Inthepaperthecharacteristicsofmacrostructureoffogareanalyzedandthephysicalprocessesofformationanddissipationoffogarestudied.TheresultsshowthattheXishuangbannavalleyfogformsfirstlyintheloweratmospherewithtwo-layerstructuresandthendevelopssuddenlyintheverticaldirectionafterreachingtheground.Furthermore,thevegetationeffectontheformationanddissipationoffogisdiscussedspecially.
简介:Basedonthehigh-resolutiondatasetscollectedinaseafogfieldexperimentatthenortherncoastofSouthChinaSea,thevariationsofliquidwatercontent(LWC)andnetlongwaveradiationflux(NLRF)duringtwoseafogeventson16th-17thand18th-19thMarch,2008areexaimeedbywaveletanalysis,andthecoolingmechanismsforfogformationandpersistencearealsoinvestigated.Themainresultsareshownasfollows.(1)Seafogmaydevelopandpersistwhetheritiscloudyornotaloft.However,whenthereiscloudalofttheLWCislessandwindspeedinseafogishigherthanthatintheclearsky.(2)Thequasi-periodicoscillations(QPOs)ofNLRFareobservedintheformationstageofthetwofogs.QPOsofLWCareonlyfoundinthedevelopingstagenomatterwithcloudlessorcloudycondition.(3)Itislikelythatseafogformsbythecoolingeffectsoflongwaveradiationanddevelopsthroughtheverticalmixinginducedbytheradiativecoolingattheupperlevel.(4)Duringseafogdevelopmentandpersistence,othermechanismscouldalsoplayimportantrolesinfog-layercooling,suchasturbulentheattransportandradiationtransportbetweenair-seainterfaces.
简介:ThesynopticanalysisofseafoginwesternAntarcticsearegionismadebasedontheobservationdataintheChineseAntarcticstation,GreatWallStation,fromDecember1994toNovember1995,andthefacsimileweatherchartsissuedbyChile.Itisfoundthatmorethan90%foginthisregionistheadvectioncoolingfog.Also,thesynopticmechanismofthefogcreationanddistinctionisdiscussedbyanalyzingthepressurefield,thetemperaturefieldandtheupperlevelstratification.Finally,thefocusofattentioninforecastingfogispointedout.
简介:TwofieldexperimentswereperformedinordertodissipatethefogatWuqingDistrictofTianjininNovemberandDecemberof2009.Hygroscopicparticleswereseededtodissipatefogdropletson6-7November,2009.Liquidnitrogen(LN)wasseededintothenaturalsupercooledfogintheexperimentsof30November–1December,2009.Significantresponsewasfoundafterseeding.Significantchangeswereobservedinthemicrostructureoffoginthefieldexperiments.Theoffogdropletchangeddramatically;itincreasedfirstandthendecreasedafterseeding.RemarkablevariationalsowasfoundintheLiquidWaterContent(LWC)andinthesizeoffogdroplet.TheDropletSizeDistribution(DSD)offogbroadenedduringtheseedingexperiments.TheDSDbecamenarrowaftertheseedingended.Afterseeding,thedropletswerefoundtobeatdifferentstagesofgrowth,resultinginatransformofDSDbetweenunimodaldistributionandbimodaldistribution.TheDSDwasunimodalbeforeseedingandthenbimodalduringtheseedingexperiment.Finally,theDSDbecameunimodallydistributedonceagain.
简介:Inthispaper,aheavyseafogeventoccurringovertheYellowSeaon11April2004wasinvestigatedbaseduponobservationalandmodelinganalyses.Fromtheobservationalanalyses,thisseafogeventisatypicaladvectioncoolingcase.Seasurfacetemperature(SST)andspecifichumidity(SH)showstronggradientsfromsouthtonorth,inwhichwarmwaterislocatedinthesouthandconsequently,moistureislargerinthesouththaninthenorthduetoevaporationprocesses.Afterfogformation,evaporationprocessprovidesmoremoistureintotheairandfurthercontributestofogevolution.TheseafogeventwasreproducedbytheRegionalAtmosphericModelingSystem(RAMS)reasonably.Therolesofimportantphysicalprocessessuchasradiation,turbulenceaswellasatmosphericstratificationinseafog’sstructureanditsformationmechanismswereanalyzedusingthemodelresults.Therolesoflongwaveradiationcooling,turbulenceaswellasatmosphericstratificationwereanalyzedbasedonthemodelingresults.Itisfoundthatthelongwaveradiativecoolingatthefogtopplaysanimportantroleincoolingdownthefoglayerthroughturbulencemixing.Thefogtopcoolingcanoverpowerwarmingfromthesurface.Seafogdevelopsupwardwiththeaidofturbulence.Thebuoyancyterm,i.e.,theunstablelayer,contributestothegenerationofTKEinthefogregion.However,thetemperatureinversionlayerpreventsfogfromgrowingupward.
简介:Basedonacurrentfogdetectiontheory,amultibandthresholdmethodforMODISdatawasputforwardtodetectdaytimefogintheSouthChinaSea.ItusedBands1,2,18,20and31ofMODISdatatoseparatefogfromthecloudandtheseasurface.Thedigitaldetectionindexeswereasfollows.IfRB1<20%,RB2<20%andRB1>RB2,thepixelwasidentifiedtobetheseasurface.IfRB1>55%,RB2>55%andTB31<273K,thepixelwasidentifiedtobeamiddle-andhigh-levelcloud.IfIFC>20,thepixelwasclassifiedtobeseafog.ThemethodwasverifiedwithseafogdataobservedfromthecoastalregionofGuangdongduringJanuary-April2011.Outofthe13samplesofsatellitedetection,ninewereconsistentwiththesurfaceobservations,threewereidentifiedtobelow-levelthecloudaccordingtothesatellitedetectionbutfogaccordingtothesurfaceobservations,andonlyonesamplewasidentifiedtobetheoceansurfacebythesatellitedetectionbutfogbythesurfaceobservations.BecausetheMODISdatacannotpenetratethecloudorfog,themodelwasdesignedforasinglefieldofviewwhichhadonlyonelayerofcloudorfog.Itcanaccuratelydistinguishfogwhichisnotcoveredbythecloud,butitidentifiesfogascloudiftheformeriscoveredbyacloud.Generallyspeaking,themodeliseffectiveandfeasible.
简介:Foghasrecentlybecomeafrequenthigh-impactweatherphenomenonalongthecoastalregionsofNorthChina.Accuratefogforecastingremainschallengingduetolimitedunderstandingofthepredictabilityandmechanismoffogformationassociatedwithsynoptic-scalecirculation.Onefrequentsynopticpatternoffogformationinthisareaisassociatedwithcoldfrontpassage(cold-frontsynopticpattern,CFSP).ThispaperexploredthepredictabilityofatypicalCFSPfogeventfromtheperspectiveofanalyzingkeycharacteristicsofsynoptic-scalecirculationdeterminingfogforecastingperformanceandthepossiblemechanism.TheeventwasensembleforecastedwiththeWeatherResearchandForecastingmodel.Twogroupsofensemblememberswithgoodandbadforecastingperformancewereselectedandcomposited.Resultsshowedthatthepredictabilityofthiscasewaslargelydeterminedbythesimulatedstrengthsofthecold-frontcirculation(i.e.,troughandridgeandtheassociatedsurfacehigh).Thebad-performingmemberstendedtohaveaweakerridgebehindastrongertrough,andassociatedhigherpressureoverlandandaweakersurfacehighoverthesea,leadingtoanadverseimpactonstrengthanddirectionofsteeringflowsthatinhibitwarmmoistadvectionandenhancecolddryadvectiontransportedtothefocusregion.Associatedwiththiscolddryadvection,adversesynopticconditionsofstratificationandmoistureforfogformationwereproduced,consequentlycausingfailureoffogforecastinginthefocusregion.Thisstudyhighlightstheimportanceofaccuratesynoptic-scaleinformationforimprovedCFSPfogforecasting,andenhancesunderstandingoffogpredictabilityfromperspectiveofsynoptic-scalecirculation.
简介:BasedondataofradiationfogeventsinXuanen,Hubeiprovince,2010,thispaperanalyzesthemicrophysicalprocessandevolutioncharacteristicsofradiationfogswithcomplicatedsubstrateintheupperandmiddlereachesoftheYangtzeRiver,andcomparesthemwithfindingsinotherareas.Resultsareasfollows:radiationfoginXuanenisevidentlyweakerindropletnumberconcentrationandliquidwatercontentthanlandfogsinotherareas.Itsliquidwatercontentfluctuatesobviously,0.01g/m3withvisibilityof1,000meters,whichisquitedifferentfromthatinurbanareas,butsimilartotheNanlingMountains.Bi-modaldropletdistributionislikelytooccurinXuanenmountainradiationfog(MRF)events.StatisticalanalysisshowsthattheobserveddropletsizedistributioncanbepiecewisedescribedwellbytheGammadistribution.Thereisapositivecorrelationbetweenliquidwatercontent,fogdropletconcentrationandmeanradius,especiallyinthedevelopmentanddissipationstage.CondensationgrowthanddropletevaporationaremajorprocessesofXuanenMRF.Thedissipationtimecoincidedwiththetimewhenthegrasstemperaturereachedthepeakvalue,whichindicatedthatdewevaporationisakeyroleinmaintainingXuanenMRF.Intheearlystageofdensefog'sgrowth,dropletswithdiameterofover20micrometerscanbeobservedwithvisibilityof800-1,000m,whichmightbecausedbythetransportationoflowclouddropletstoearth'ssurfacebyturbulence.Bigdropletsintheinitialstagecorrespondtohigherwatercontent,leadingtothehigherobservedvalueofwatercontentofXuanenMRF.