简介:在通过β飞机barotropic的reinvestigated与加热和驱散的考虑建模的热带空气的多重equilibria和他们的稳定性。Wehave首先导出相应于多重equilibria或稳定流的模型方程的答案,然后直接由theLiapunov的使用为稳定流的稳定性建立标准方法。这些标准什么时候被用于equilibria的答案,获得了;马厩在热带区域与伪静止的循环的不同模式有关仔细流动,它是,被发现。在他们中的二个之间的这些稳定的流动和移动的配置作为季节变化提供相当合理的解释给象发作的大祸机制和亚洲夏季风的break-activecycle那样的热带发行量特征的许多基本问题。因而,发作或Asiansummer季风的突然的转变能被归因于热带发行量的多重平衡性质源于移流的非线性,它在其它之中提供另一解释。
简介:Si3N4powderandhot-pressedSi3N4ceramicsaddedwithAl2O3areusedforinvestigatetheiroxidationbehviorinairandnitrogenatmosphere(withoxygenpartialpressurePO2=1-10Pa),TheoxidationproductsofSi3N4areexaminedbychemicalanalysi,X-raydiffraction(XRD)andXPSmethod,Also,thermodynamiccalculationismadetoanalyzeoxidationbehaviorofSi3N4.TheresultsshowthatonlypassiveoxidationwilloccurwhenSi3N4isoxidizedinairathightemperature,whereasinN2athightemperature,theactiveoxidationisdominantinspiteoftheexistenceofalittlepassiveoxidation.
简介:Anovelatmosphericplasmadevicedevelopedinthispaper,whichismoreeffectiveandconvenienttostudytheplasma-initiatedpolymerization(PIP)thanconventionalsetup.Thestructureandmechanismofthedeviceisintroduced.Someplasma-initiatedpolymerizationexperimentsarecarriedoutonthedevice,andtheconversionofAA(Acrylicacid)andAM(Acrylamide)atmospheric(N2)plasmapolymerizationarerespectively89%and94%after120hpostpolymerization,wherebyIRspectraoftheproduct(AA,AM).OurPIPresultareconfirmed.
简介:Byusingtheupper-winddatafromJuly1980toJune1983,thevariationsofthelow-frequencyoscillation(LFO)intheatmospherebeforeandduring1982ElNinohavebeeninvestigated.BeforetheElNino,theLFOpropagatesfromwesttoeastovertheequatoroftheEasternHemisphereandfromeasttowestover20°N.TheeastwardpropagatingLFOovertheequatorconsistsofzonalwavenumber1propagatingeastwardandzonalwavenumber2withacharacterofstationarywave.Theoscillationofzonalwavenumber2canmodulatetheoscillationstrength.AftertheonsetoftheElNino,thepropagatingdirectionsoftheLFOovertheequatorand20°NoftheEasternHemispherechangetobewestwardandeastward,respectively.TheLFOoverthewesternPacificweakensrapidlyandonecomingfrommiddleandhighlatitudespropagatestotheequator.Fromthephasecompositionsofstreamlinefieldsforthezonalwavenumber1ofequatorialwestwardpropa-gatirgLFO,itisfoundthattheatmosphericheatsourceintheequatoroftheeasternPacific(EEP)excitesaseriesoftheequatorialcyclonesandanticycloneswhichmovenorthwardandwestwardandformthewestwardpropagatingLFOovertheequator.Withthewavelengthof20000km,thiskindofequatorialwaveissimilartothemixingRossby-gravitywave.Initswestwardandnorthwardmovement,thecirculationinEastAsiaismodified.ThismaybethemechanismoftheinfluenceofElNinoontheclimateofChina.
简介:TheChineseAcademyofMeteorologicalSciences(CAMS)hasbeendevotedtodevelopingaclimatesystemmo-del(CSM)tomeetdemandforclimatesimulationandpredictionfortheEastAsianregion.Inthisstudy,weevaluatedtheperformanceofCAMS-CSMinregardtosensibleheatflux(H),latentheatflux(LE),surfacetemperature,soilmoisture,andsnowdepth,focusingontheAtmosphericModelIntercomparisonProjectexperiment,withtheaimofparticipatingintheCoupledModelIntercomparisonProjectphase6.WesystematicallyassessedthesimulationresultsachievedbyCAMS-CSMforthesevariablesagainstvariousreferenceproductsandgroundobservations,includingtheFLUXNETmodeltreeensemblesHandLEdata,ClimatePredictionCentersoilmoisturedata,snowdepthclimatologydata,andChinesegroundobservationsofsnowdepthandwintersurfacetemperature.WecomparedtheseresultswithdatafromtheECMWFInterimreanalysis(ERA-Interim)andGlobalLandDataAssimilationSystem(GLDAS).OurresultsindicatedthatCAMS-CSMsimulationswerebetterthanorcomparabletoERA-Interimreanalysisforsnowdepthandwintersurfacetemperatureatregionalscales,butslightlyworsewhensimulatingtotalcolumnsoilmoisture.Theroot-mean-squaredifferencesofHinCAMS-CSMwereallgreaterthanthosefromtheERA-Interimreanalysis,butlessthanorcomparabletothosefromGLDAS.ThespatialcorrelationsforHinCAMS-CSMwerethelowestinnearlyallregions,exceptforNorthAmerica.CAMS-CSMLEproducedthelowestbiasinSiberia,NorthAmerica,andSouthAmerica,butwiththelowestspatialcorrelationcoefficients.Therefore,therearestillscopesforimprovingHandLEsimulationsinCAMS-CSM,particularlyforLE.
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简介:Byutilizingthebarotropicvorticityequationincludingeffectsoforographyandhorizontaldiffusion,thelinearizedequationsdescribingsymmetricandantisymmetricmotionsandtheiranalyticsolutionsarepre-sented.Itcanbefoundfromthesolutionsthatnomatterwhatkindofmotionmaybe,eachsolutionconsistsofthreewaves,namely,Rossbywaverelatedtoinitialvalues,marchingwavepropagatingatRossbywavevelocityandstationarywave.Thelattertwoarecloselyrelatedtoorographyandhorizontaldiffusion.However,ifthemotionissymmetricattheinitialinstant,thentheantisymmetriccomponentsoforographyandofhorizontaldiffusionarelikelytoleadtothegenerationofantisymmetricmotion.Inthesteadystate,thesymmetricflowisconnectedwithsymmetricorographyandhorizontaldiffusionandtheantisymmetricflowwithantisymmetricorographyandhorizontaldiffusion.Further,inordertoverifytheaboveanalysis,threenumericalexperimentshavebeenmade.Theresultsshowthatantisymmetricorographycanproduceantisymmetricmotion.Finally,theatmosphericinteractionsbetweenNorthernandSouthernHemispheresarediscussed.
简介:BasedonMM5,POM,andWW3,aregionalatmosphere-ocean-wavecoupledsystemisdevelopedinthisworkundertheenvironmentofMessagePassingInterface.ThecoupledsystemisappliedinastudyoftwotyphoonprocessesintheSouthChinaSea(SCS).Theresultsshowthatthecoupledmodeloperatessteadilyandefficientlyandexhibitsgoodcapabilityinsimulatingtyphoonprocesses.Itimprovesthesimulationaccuracyofthetrackandintensityofthetyphoon.Theresponseofoceansurfacetothetyphoonisremarkable,especiallyontherightsideofthetyphoontrack.Theseasurfacetemperature(SST)declines,andtheoceancurrentandwaveheightareintensified.Inthecouplingexperiment,thedeclineofSSTintensifiesandtheinertialoscillationamplitudeoftheoceancurrentincreaseswhentheocean-waveeffectisconsidered.Therefore,theatmosphere-ocean-wavecoupledsystemcanhelpinthestudyofair-seainteractionandimprovethecapabilityofpredictingandpreventingweatherandoceanicdisastersinSCS.
简介:Aglobalcoupledair-seamodelofshallowwaterwaveisdevelopedbasedoncoupledocean-atmospheredynamics.Thecouplingisrealizedthroughtheair-seainteractionprocessthattheatmosphereactsontheoceanbywindstressandtheoceanactsontheatmospherewithheatingproportionaltoseasurfacetemperature(SST)anomaly.Theequationisharotropicprimitiveone.ResponseexperimentsofcouplingsystemarealsocarriedoutSSTAintwocategoriesofintensities.ComparedwiththeresultsofAGCMsimulationex-perimentinwhichonlythedynamicchangeofairsystemisconsidered,itdemonstratesthattheair-seainteractionbetweenthetropicaloceanandtheglobalatmosphereplaysaveryimportantroleintheevolutionofclimatesystem.Theresultsofnumericalsimulationshowthatitisencouraging.
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简介:Abaroclinicsemi-geostrophicmodelwithevaporation-windfeedbackmechanism(EWFM)andCISKisestablished,twonon-dimensionalparametersaandηareintroducedtorepresentEWFMandCISK,respectively.Analyticsolutionsofthemodelsystemareobtained,dynamicsanalysesandthemodelatmospherecalculationsfurtherconfirmthatEWFMandCISKareveryimportantphysicalprocessesinleadingtothelow-frequencyoscillationsinthetropics.
简介:不同尺寸的喷雾器被一个安德森空气刺绣花样收集观察黑碳(BC)的详细形态学与另外的伴随的喷雾器化学上被分开的喷雾器,用与一个精力DispersiveX光线分光计(SEM-EDX)装备的一台扫描电子显微镜。结果显示大多数BC喷雾器是在直径并且与同类的表面的大约50nm的球形的粒子。结果也证明这些粒子与另外的喷雾器或与自己一起聚集形成更大在测微计范围聚结。这些50-nmBC球形的粒子的形状被发现很类似于免除石油动力的车辆的内燃机的BCparticles的。这些球形的BCparticles被显示与发现帮助usingMatrix的激光解吸附作用/电离蒂米夫莱特·马斯·斯佩克特罗梅特里(MALDI-TOF-MS)的以前报导的fullerenes不同。
简介:ThesensitivityofDopplerwindlidarisanimportantparameterwhichaffectstheperformanceofDopplerwindlidar.Aerosolscatteringratio,atmospherictemperature,andwindspeedobviouslyaffectthemea-surementofDopplerwindlidarwithiodinefilter.Wediscussabouttherelationshipbetweenthemea-surementsensitivityandtheaboveatmosphericparameters.Thenumericalrelationshipbetweenthemisgiventhroughthetheoreticalsimulationandcalculation.
简介:根据强壮的ENSO处理的1982/1983的比较,象快速的开发,巨大的紧张和突然的撤退那样的关键特征在1997/1998关于温暖的事件被揭示,为这个过程在它海洋和空气的发作和进化期间为热带印度洋和西方的太平洋管理intraseasonal摆动的特征特征地详细被学习。