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简介：当前的学习的PurposeThe目的是开发并且验证一项运动特定的谨慎措施，运动员谨慎问询表(AMQ)，通过使用的5相关研究，4分开中国运动员的样品。AMQ是设计估计在运动context.MethodsIn研究1反映在场时刻的注意，了解，和接受的谨慎的一项3因素措施，项目的一个起始的水池基于以前的文学被产生，存在谨慎可伸缩，以及会见与并且从运动员，的反馈指导，并且谨慎专家。对AMQ的3因素结构的起始的支持经由探索因素被建立在学习2的分析，和通过在研究的确定的因素分析的跨validated3和4。在学习5，有直接措辞的接受项目的修改3因素AMQ在第四独立sample.ResultsConvergent被检验，接受subscale的并发的有效性没能在研究被证实3和4虽然解释颠倒措辞的项目，它可能由于运动员的疏忽和混乱。在5显示的令人满意的模型适合的学习和可接受的内部一致性的修改16条款AMQ。最重要地，16条款AMQ的会聚、并发的有效性被支持。3subscales与谨慎显示出重要积极协会，流动，健康，并且积极影响并且有经验的回避，染料烧尽，和否定affect.ConclusionTheAMQ的重要否定协会是在运动上下文的谨慎的一项psychometrically健全的措施。使用直接措辞的接受项目的重要性被讨论。

简介：TyphoonMegi,the13thtyphoonofthe2010typhoonseason,wasselectedforcasestudybyutilizingtheWeatherResearchandForecasting(WRF)model.Twelvesensitivityexperimentswithvariousinitialtropicalcyclone(TC)intensitiesandsizeswereconductedtoinvestigatetheirimpactsonthesimulationoftyphoontrack.InteractionbetweenTCandthewesternPacificsubtropicalhigh(WPSH)wasalsoanalyzedtoexplorethemechanismfortheimpactonTCtrackoftheinitialTCintensityandsize.NumericalresultsindicatethatthesimulatedTCsizeandTCtrackaresensitivetoinitialTCintensityandsize.StrongerinitialTCintensityandlargerinitialTCsizeoftenleadtolargersimulatedTCsizeandmakeTCturnnorthwardearlier.Furtheranalysissuggeststhat,withtheincreaseofinitialTCintensityandsize,moreairmassentersintotheTCregion,whichsubsequentlyreducestheextentofWPSH.Asaresult,thesteeringflowchangessignificantlyandeventuallycausestheTCtoturnnorthwardearlier.ThepresentstudyconfirmsthattheinitialTCintensityandsizehavecertaininfluencesontheTCtracksimulation,whichdemonstratestheimportanceofaccurateinitialconditionforsuccessfulsimulationoftheTCintensityandTCtrack.Moreover,italsodeepensourunderstandingoftheinteractionbetweenTCandWPSH,provideshelpfulcluesfortheTCtrackchangestudy,anddiscussesthefuturedirectionsforimprovementofTCtrackforecast.

简介：Basinmodelinghasbecomeanimportanttoolforanalyzingsedimentarybasins.TheNorthSubbasinoftheSouthYellowSeaBasinisfilledwiththickMeso-Cenozoicterrigenousdepositsduringtheriftevolutionstage.Theaccumulationofdataandachievementsofgeologicalinvestigationsinrecentyearshaveprovidedthepreconditionsforbasinmodeling.Thenecessaryparametersandgeologicalelementsforsimulationsarecollatedandsummarized.Modelingoftectono-thermalevolutionisperformedandtherelatedtrendinheatflowisreconstructedandcalibrated.Theheatflowvaluecommencesfromanaveragelevelof61mW/m~2duringMiddleLateJurassic,risestoabout80mW/m~2fromcirca145Matocirca74Ma,andthenundergoesagradualdeclineto65mW/m~2untiltheendofOligocene.Threeevolutionaryphases,namely,theinitialriftingphase,syn-riftingphase,andpost-riftingphase,havebeenidentified.ThemodelingresultsshowthattheNorthSubbasingenerallyentersintoastageofstrongriftingduringCretaceousandundergoesrapidsubsidenceuntiltheLateCretaceous,thenfollowsbyastageofmoderateriftingduringthePaleogene.Theinputandgeneralworkflowinvolvedin3-Dmodelingareintroduced.ReconstructionofthepetroleumsystemintheNorthSubbasinrevealsthatthethresholddepthofhydrocarbongenerationislocatednearthetopofthePaleogeneFuningformation,andtheunderlyingJurassicandCretaceoussourcerockshavereachedorexceededpeakoilgenerationandhavealmostcompletedthegenerationandexpulsionofhydrocarbons.ThemaingenerationandexpulsionintheJurassicsourcerockstakeplaceduringthesyn-riftingandpost-riftingphases,whereasthepeakgenerationandexpulsionintheCretaceousandPaleogenesourcerockstakeplaceduringthepost-riftingphase.Althoughthestudyareaisstillarelativelylessexploredsedimentarybasin,theresultsofmodelingcanprovidevaluableinformationforexploration.Apreliminarydiscussionofthemainuncertaintyfactor

简介：ObjectiveThenearlyparallelN–S-trendingriftsinsouthernTibetrepresenttheE–WextensionoftheTibetPlateau.MostdatawhichconstrainedtheageoftheextensionaldeformationcomefromisotopicdatingofthedikesprobablyrelatedtotheactivityofthenearlyN–Sfaultingandmicasfromhydrothermalactivityandthelowtemperaturethermochronologyofplateauuplift.Previous