简介:沿着在长江的更低的活动范围的Meiyu前面的重降雨事件在2009年6月23日与一个mesoscale骚乱旋涡被连接,这被发现,它从行星的边界层(PBL)发源并且以后向上发展了并且被使用过滤方法的Shuman-Shapiro发现。在在这个过程的PBL(PMDV)的mesoscale骚乱旋涡在Doppler雷达回响对应于很好短时间的暴风雨。从先进天气研究和预报模型(ARW)的高分辨率的模拟结果的分析证明沿着在PMDV的产生以前的Meiyu前面的南部的温暖的节有几表面骚乱。PMDV与mesoscale交往了对流系统(MCS)并且加强了本地对流降水。在PBL的北方和西南流动在PMDV形成的时候收敛了。同时,到旋涡的南方方面的PBL的顶上的一口西南的喷气增强了上升运动和集中。因此,shear线的强壮的冷空气流动北方什么时候shear线向南遇到了西南流动,被结束PMDV被产生。在PBL,西南风的增强,和北方风的向南方的侵略的集中线为PMDV的发展是批评的。当它在底层便于集中,潜伏的热的版本为PMDV的形成被发现关键。
简介:Globalseismicitycatalogsaresufficientforcharacterizingdoubleseismiczones(DSZs)insubductingslabandfacilitatetoestimatelayerseparationwithoutinconsistentuncertaintiesaslocalcatalogs.PreviousstudieshaveshownthecorrelationbetweenDSZslayerseparationandplateagewhilecorrelationforthoseyoungerthan~60Maissuspicious.ThelackingofDSZswithlayerseparationlessthan10kmfurthermakesitdifficulttopreciselyestimatesuchcorrelation.Thus,weincorporateeightDSZsdatadeterminedthroughlocalseismicityintoglobally-determineddatasetandreexaminesuchcorrelation.Thebestfittingresultsshowthatbothalinearmodelandasquarerootofplateagecanmathematicallyfitthelayerseparationwell.However,itisdifficulttodistinguishthesetwomodelswhenplateageisgreaterthan~20Masincetheirdifferenceislessthan2km.However,ifextrapolationispossible,bothmodelsshouldprovidephysicalinformationthatDSZswillnotformifthereisnosubductinglithosphere.Asaresult,theDSZscannotbeproduceduntiltheoceaniclithosphericagebecomesgreaterthan0.9Mainthesquarerootmodelwhilethelinearmodelgivesamisleadingresult.Assuchthesquarerootmodeldemonstratestherelationshipphysicallybetterthanthelinearone,itstillneedsfurthertestinthefuturewithmoreavailabledata,nevertheless,ourstudymightalsoprovideevidenceforthesuggestionthattheplateageisaprimarycontrolfactoroftheDSZsgeometryaswellasthesubductingprocesswhichdisregardsanylocaltectonicstresses.
简介:Thispaperextendsapredictionmodelformulti-directionalrandomwavetransformationbasedonanenergybalanceequationbyMasewiththeconsiderationofwaveshoaling,refraction,diffraction,reflectionandbreaking.Thisnumericalmodelisimprovedby1)introducingWen'sfrequencyspectrumandMitsuyasu'sdirectionalfunction,whicharemoresuitabletothecoastalareaofChina;2)consideringenergydissipationcausedbybottomfriction,whichensuresmoreaccurateresultsforlarge-scaleandshallowwaterareas;3)takingintoaccountanon-lineardispersionrelation.PredictionsusingtheextendedwavemodelarecarriedouttostudythefeasibilityofconstructingtheAiHuayachtportinQingdao,China,withacomparisonbetweentwoportlayoutsindesign.Wavefieldsinsidetheportfordifferentincidentwavedirections,waterlevelsandreturnperiodsaresimulated,andthentwokindsofparametersarecalculatedtoevaluatethewaveconditionsforthetwolayouts.AnalysesshowthatLayoutIisbetterthanLayoutII.Calculationresultsalsoshowthattheharborwillbecalmfordifferentwavedirectionsunderthedesignwaterlevel.Onthecontrary,thewaveconditionsdonotwhollymeettherequirementsofayachtportforshipberthingundertheextremewaterlevel.Forsafetyconsideration,theelevationofthebreakwatermightneedtobeproperlyincreasedtopreventwaveovertoppingundersuchwaterlevel.Theextendednumericalsimulationmodelmayprovideaneffectiveapproachtocomputingwaveheightsinaharbor.
简介:充分提取并且我的在时空尺寸的水库和地质的结构的多尺度的特征,新3D多尺度的容量的弯曲(MSVC)方法论在这份报纸被介绍。我们也为计算3D建议一个快算法容量的弯曲。与常规容量的弯曲属性相比,它的主要改进和关键算法在wavenumber域在时间频率领域和相应多尺度的适应微分操作符介绍多频率部件扩大,进容量的弯曲计算。这方法论能同时在两时空描绘地震多尺度的特征。另外,我们在各种各样的规模使用容量的弯曲的数据熔化充分利用弯曲大小在不同规模提取的地质的特征和异例。3DMSVC能加亮地质的异例并且同时减少噪音。因此,它改进弯曲属性分析的解释效率。3DMSVC被用于土地和海洋的3D地震数据。结果证明它能显示水库的空间分发,检测差错和破裂地区,并且识别他们的多尺度的性质。
简介:Detectingthetimingandamountofdeformationiscriticalforunderstandingthephysicalcausesandeventuallywarningofpossiblelandslidehazards.Monitoringofdeformationofstructuresandgroundsurfacedisplacementsduringlandslidescanbeaccomplishedbyusingdifferenttypesofsystemsandtechniques.Besidesgeotechnicalorphysicaltechniques,remotesensingtechniquescanbeclassifiedassatellitetechniques,photo-grammetrictechniques,geodetictechniques,groundbasedtechniques,andsoon.TostudyandgoverngrowinggeologicaldisastersinChina,especiallyintheThreeGorgesarea,ThreeGorgesResearchCenterforGeo-hazard(TGRG)isestablishinganinfrastructuretoef-fectivelyandcomprehensivelyanalyzethemechanismoflandslidedeformation,focusedontheHuangtupolandslide,usingofvariousad-vancedmonitoringsystemsandtechniques.Inthisarticle,theframeworkandlatestadvancesofintegrationofmultiremotesensingtechniquesintheinfrastructurearepresented.Differentremotesensingtechniques,dataprocessingandintegratingmethods,andthelatestresultsarediscussedindetail.Atlast,reviewsoncurrentworkandsuggestionsforfurtherworkareputforward.
简介:浮标系统的推广是为浮标系统的操作的最重要的过程之一。在现在的学习,包含表面浮标的一个单个点的绳索浮标系统,有部件的电报片断,锚被使用多身体动力学等等建模方法。运动方程在分离节点描述和充分笛卡儿的坐标被开发。然后数字的方法被用来解决平常的微分方程,当锚从董事会正在扔时,动力学模拟被完成。没有电流并且与在浮标系统的电流的不同节点的轨道和速度被获得。电缆线的每部分的短暂紧张力量在推广的进程被分析。当锚正在摸海床和力量将与不同漂浮配置改变的最大的紧张时,数字结果显示短暂收费载重增加到山峰价值。这个工作对浮标系统计划的设计和推广有用。