简介：Duetothecloserelationshipbetweenregionalclimateanomaliesandsocial-economyandsocietydevelopment,climatologistsworldwidepaidgreatattentiontotheregionalclimateanomaliesoveralongperiodoftimeandthecorrespondinginvestigationofregionalclimatemodelinghasmadegreatprogresses.Since1990theregionalclimatesimulationshavemadeamoresubstantialachievement.Thispaperwillfocusonthereliabilityanduncertaintiesofregionalclimatemodelingbyglobalclimatemodels,theadvancesonregionalclimatemodelingintheworldandtheoutlookofregionalclimatemodeling.

简介：自从Holocene，在Xiliao河山谷的农业开垦从草地导致了一个巨大的风景变化到农田。在这份报纸，我们由自从Qing王朝，在史前，Liao-Jin王朝和时期分析三主要农业开垦在Xiliao河山谷重新考虑人陆地关系。我们主张当人口统计的压力出现在这个区域时，特别在最后开垦期间，intraregional迁居(第二迁居)是主要反应减轻如此的压力，它也区分二个不同解决地点：起始的区域和第二等的区域。由于这二个区域之间的环境差别，一个人引起了更多的严肃的骚乱到本地环境的后者上的耕作。因此，第二等的区域成为了严重需要环境管理的关键区域。

简介：Abetterunderstandingofthelong-termglobalcarboncyclerequiredestimateofthechangesinterrestrialcarbonstorageafterthelastglacialperiod.Theresultsofsimulationatmid-Holocene(MH)fromPMIP(PaleoclimateModelingIntercomparisonProject)andthemoderndatafromCRU(ClimateResearchUnit,EastAngliaUniversity,UK)allowustousetheAtmosphere-VegetationInteractionModel(AVIM)tosimulatetheChineseterrestrialnetprimaryproductivity(NPP)at6kaBPandpresenttime.ThechangeofNPPandtotalNPPinChinafromnowtomid-Holoceneareabout54gm-2yr-1and0.63Pgyr-1,respectively,mainlyduetothebuild-upoftemperateforestandtropicalrainforest.ChineseterrestrialNPPvariationfromMHtonowiscloselyrelatedtothevariationinintensityofAsianmonsoon,whichcontrolledtheclimate-vegetationpatternchange.

简介：BasedontheseismicdatagatheredinpastyearsandthecorrelationbetweentheseaandlandareasoftheLowerYangtzePlatform,thestructuralcharacteristicsoftheSouthYellowSeaBasinsincetheIndosiniantectonicmovementisstudiedinthispaper.ThreestagesofstructuraldeformationcanbedistinguishedintheSouthYellowSeaBasinsincetheIndosinian.Thefirststage,LateIndosiniantoEarlyYanshanian,wasdominatedbyforelanddeformationincludingboththeupliftingandsubsidencestagesunderanintensivelycompressionalenvironment.Thesecondstage,whichiscalledtheHuangqiaoEventinthemiddleYanshanian,wasachangeforstressfieldsfromcompressiontoextension.Whileinthethirdstage(theSanduoEvent)intheLateHimalayan,thebasindevelopedadepressionintheNeogene-QuatemaryafterriftingintheLateCretaceous-Paleogene.Thelong-timeevolutioncontrolled3basinformationstagesfromaforelandbasin,thenafaultbasintoafinaldepressionbasin.Inconclusion,sincetheIndosinian,theSouthYellowSeaBasinhasexperiencedcompressionalfoldandthrust,collisionalorogen,compressionalandtensionalpulsation,strike-slip,extensionalfaultblockandinversionstructures,compressionandconvergence.TheNE,NEE,nearlyEWandNWtrendingstructuresdevelopedinthebasin.Fromwesttoeast,thestructuraltrendchangedfromNEEtonearEWtoNW.Whilefromnorthtosouth,theychangedfromNEEtonearEWwithastrong-weak-strongzoningsequence.Vertically,themarineandterrestrialfaciesbasinsshowa"seesaw"patternwithfoldandthrustintheearlystages,whichisstronginthenorthandweakinthesouthandanextensionalfaultinlaterstages,whichisstronginthenorthandweakinthesouth.Inthemarinefacies'basin,thrustdeformationismoreprevailingintheupperstructurallayerthanthatinthelowerlayer.ThetectonicmechanismintheSouthYellowSeaBasinismainlyaffectedbythecollisionbetweentheYangtzeandNorthChinaBlock,whilethestressenvironmentoflarge-scal

简介：自从2003，这篇论文考察中央规模天气动力学的主要理论进步，包括：(1)平衡并且失衡的流动的动态机制被使用学习中央规模循环的开始和发展问题。对称的不稳定性和横向波浪的不稳定性在线和旋涡空气传送对流被分析，并且进一步的研究在非线性的对流对称的不稳定性上被做了。在强迫对流和不稳定的传送对流和中央规模运动的波浪特征之间的相互作用也被讨论。(2)动态边界层建模的中间的空气被开发。复杂非线性的相互作用在大气的边界层和自由大气层之间理论上被分析。低级前面的地形学边界层和另外的边界层的结构动态问题被讨论。(3)在东亚空气发行量的背景下面的meso-β-scale暴风雨的形成和发展与MPV(潮湿的潜在的涡度)的变化被诊断异例。，并且在潮湿的空气。

简介：ThisarticleaddressessedimentresearchcarriedoutfortheThreeGorgesProjectsince1993,whentheconstructionoftheprojectwasformallystarted.Emphasisoftheresearchhasbeenplacedonthesolutionofrelevantproblemsarisingfromdesignandconstructionofvariousstructures,includingsedimentationproblemsintheChongqingreach;layoutoftheupperlockapproachchannelandwaysandmeanstomitigateitsdeposition;increasingreservoircapacitybyoptimizingreservoiroperation;compensatingdepthofflowrequiredbynavigationbelowtheGezhoubaProjectcausedbyscouring;mitigationofadverseeffectsoferosiononthereachfromZhichengtoJiangkou;andevaluatingscouroftheJinjiangreachcausedbyreleasingflowsoflowconcentrationsfromtheTGP.Inaddition,reductionofthesedimentloadenteringintothereservoirareaoftheTGPintherecentyearsaswellasthatexpectedoftheprojectedconstructionoflargehydropowerstationsontheJinshaRiverupstreamoftheTGPreservoirisalsonotedanddiscussed.

简介：Theeffectiveprecipitationandtheframeofatmosphericcirculationinthepastthreekeyperiods,i.e.30kaBP,18kaBPand6kaBP,havebeenanalyzedonthebasisofthepalaeolakestatusrecordproducedbytheChineseLakeStatusDataBase.Theresultsshowthatthewest-centralpartofChinawascharacterizedbyhighlake-levelsat30kaBP,resultingfromstrengthenedsouthwestmonsoons;whereasthehighlakestand,occurringinthewest-centralpartofChinaat18kaBP,wascausedbythesouthwardshiftandthestrengtheningofwesterliesalthoughthehigh-standdistributionwasreduced.Meanwhile,theeast-centralpartofChinawasunderthecontrolofstrongwintermonsoonsat18kaBP.Thehighlake-levels,whichoccurredintheeast-centralpartofChinaat6kaBP,arerelatedtotheenhancedEast-Asiansummermonsoons;whiletheloweringofthelake-levelinthewest-centralpartofChinaat6kaBPwasduetothenorthwardshiftandcorrespondingshrinkofthewesterlies.Acomparisonb

简介：TheCaofeidiansandbar-lagoonsystemissituatedalongthenorthwestcoastoftheBohaiSea.Thesystemhasevolvedfromtheabandoneddelta,whichcameintobeingbySuheRiverandXiaoqingheRiverinthemiddleHolocene.Atthemoment,thesystemhasalmostlostthesupplyofriversediments.(Fig.1)

简介：TheearthquakeactivityanddamageinmainlandChinain2003arereviewed.Therewere27earthquakeswithamagnitudeofover5.0,resultingin319peoplekilledand7147peopleinjured.Thetotaleconomiclossofover560millionUSdollarsrepresentsthehighestfigureformainlandChinasince1977,anditiscomparabletothetotallossduringonedecadeinthe1980's.ForthefirsttimeChinaInternationalSearchandRescue(CISAR)teamsweredispatchedtodisasterareasinChina,Algeriaandlran.

简介：基于一0.5?牰'虨宫摤嫕?牰湩楣慰?潣灭湯湥?湡污獹獩儻汩慩?潍湵慴湩`

简介：Byanalyzinghigh-resolutionSPOTimagesandincombinationwithfieldworkandchronometry,threetypicalfault-offsetsitesonthesouth-middleAltynTaghstrike-slipfaultwerestudiedtoobtainthesinistralhorizontalsliprateofthefault.AtAnnanba,theleft-lateralstrike-sliprateonabranchofthesouthAltynTaghfaultis7.5±1.7mm/asince9.36±0.73kaBP.AtSevenSpring,thefaulthasfourbranchesandtheleft-lateralstrike-sliprateononeofthemis2.3±0.5mm/asince13.86±1.07kaBP,anditisdeducedthatthetotalsliprateofallthefourbranchesis6.9±1.5～9.2±2.0mm/asinceHolocene.AtYuemakeqi,theleft-lateralstrike-sliprateofthefaultis10.6±3.0mm/asince4.73±0.38kaBP.Aslip-rateof7～11mm/aonthemiddlesegmentoftheAltynTaghfault(between88°30'Eand93°05'E)sinceHolocenecanbededucedfromthethreesitesmentionedaboveandtheresultissimilartothelatestGPSobservation.

简介：有在位于亩的东南的Salawusu河山谷的Milanggouwanstratigraphic节的palaeosols的palaeo活动的沙丘沙和fluvio湖的外形我们自从150kaBP，和谷物尺寸参数鈥?Mz，荒芜的富有经验的丰富的显著选择在grainsize粗糙、好的节奏变化，蟽，Sk，Kg和SC/D也对在山峰和山谷价值之间的multi-fluctuational引申的状况作出回应。同时性grainsize特征值鈥??5，?16，?25，?50，?75，?84并且?95是respondingly被表明极大地有节奏的跳动。在此，Milanggouwan节能被划分成粗糙、好的27谷物尺寸沉积当自从150kaBP，荒芜的变化的气候地质的过程的一个真实、综合的记录源于古老的冬季的其他的发展和东亚的夏天季风，骑车，它能被考虑。

简介：ContinentalChinahasmoveddextralEastwardsinceCenozoictime,drivenbythecollisionoftheIndianwiththeEurasianplate.Evidenceforthiscomesfromlandscapeevolution,thedistributionofearthquakeepicenters,Cenozoicsedimentaryandvolcanicrocks,andthemeasurementofGPSvelocityvectors,thedistribntionofcrustalstress,paleomagneticdata,anddeepmantlestructure,amongothers.Thismovementcommencedaround40Ma,coupledwiththickenedlithosphereandwidespreadstressreleasealongstrikeslipfaultsthatboundthecontinentalChineseblock.BecauseofcontinuedNorthwardsubductionoftheIndianplate,manifestationofthedextralmovementhasintensifiedsince25Ma.Far-reachingeffectsincludeextensivestrike-slipmovementontheTan-LufaultinEasternChina,formationoftheDabieultrahighpressuremetamorphicterrane,extensivethrustfaultsinEastChina,delaminationandthickeningofthelithosphereofSouthChina,apossibletectonicdoublingoftheMiddle-LowerYangtzeValleymetallogenicbelt,andtheformationoftheJapan,Huanghai(EastChina),andSouthChinaSea.

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简介：在北半球从14个地点把重建和代理数据基于温度，这篇论文集中了于比较在北极和另外的区域之间的温度变化的周期包括大西洋，欧洲，中国，亚洲，和平，印度洋，并且美洲在到最后冰川的最大值的从最后Interstade的转变期间，从最后冰川的最大值到在Holocene和由单个光谱分析(SSA)的方法的小冰川期(LIA)的转变的megathermal时期结果证明在北极的环境变化在北美人并且更好很类似于那类似于亚洲，大西洋和太平洋，最不类似于印度洋和欧洲。温度的1500年的摆动在北极和欧洲两个都存在。

简介：TakingtheHuaihetotheNvshanhusegmentoftheTanlu(Tancheng-Lujiang)faultzoneasthemainresearchtargettoexplorewhethertherehasbeennewactivitysincethelateQuaternary,andbasedontheinterpretationofremotesensingimagesandrepeatedsurfaceinvestigations,weexcavatedtrenchesatthesectionswherethetectoniclandformissignificant,identifiedandrecordedthedeformationpatternsofthefaultandanalyzedtheactivitybehavior.Samplesofnewactivityanddeformationwerecollectedandorientedslicesweregroundbasedonthesamples'originalstatetomakethemicrostructuralanalysisanddemonstration.Alloftheaboveresearchshowsveryclearlineartectonicgeomorphologyalongthefault,threetrenchesacrossthefaultzoneallrevealednewdeformationtracessincelateQuaternary.ThelateststratumdislocatedbythefaultisthelateQuaternaryandHolocene.Themainslipmodeisstickslip,asrepresentedtypicallybyfaultscarps,wedgeaccumulation,thefaultsandthefilledcracksandsoon.Ingeneral,itshowsthecharacteristicsofbrittlehigh-speeddeformationandbelongstotheprehistoricearthquakeruins.Theaboveunderstandingwasconfirmedpartiallybymicroscopicanalysis.Inaddition,thesimilaritiesanddifferencesandthepossiblereasonsforthecharacteristicsofthelatestactivitiesoftheTancheng-LujiangfaultzoneinthenorthandsouthoftheHuaiheRiverregionsarealsodiscussedinthispaper.

简介：BecauseofthesignificancetotheformationandevolutionoftheTibetanplateau,thedisplacementandsliprateoftheAltynTaghfaulthavebeentopicsfullofdisputation.ScientistswhoholddifferentopinionsontheevolutionofTibetinsistondifferentslipratesanddisplacementsofthefaultzone.Inthearticle,studyisfocusedonthelateQuaternarysliprateoftheAltynTaghfaultwestoftheCherchenRiver(between85°Eand85°45'E).OnthebasisofhighresolutionSPOTimagesoftheregion,threesites,namelyKoramlik,AqqanpastureandDalakuansay,werechosenforfieldinvestigation.Tocalculatethesliprateofthefault,displacementofterraceswasmeasuredonSPOTsatelliteimagesorinsituduringfieldworkandthermo-luminescence(TL)datingmethodwasused.Togettheagesofterraces,samplesofsandwerecollectedfromtheuppermostsandbedsthatliejustunderloess.Themethodforcalculatingsliprateoffaultistodividethedisplacementofterracerisersbytheageofitsneighboringlowerterrace.Thedisplacementofriversisnotconsideredinthisarticlebecauseofitsuncertainties.AtKoramlik,thesliprateoftheAltynTaghfaultis11.6±2.6mm/asince6.02±0.47kaB.Pand9.6±2.6mm/asince15.76±1.19kaB.P.AtAqqanpasture,about30kmwestofKoramlik,thesliprateis12.1±1.9mm/asince2.06±0.16kaB.P.AtDalakuansayi,thesliprateofthefaultis12.2±3.0mm/asince4.91±0.39kaB.P.Hence,wegettheaveragesliprateof11.4±2.5mm/aforthewesternpartoftheAltynTaghFaultsinceHolocene.ThisresultisclosetothelatestresultsfromGPSresearch.

简介：Huanghe河三角洲是世界的大河之一，自从最后，Huanghe河里的Huanghe河三角洲paleoenvironmental进化是一个热问题冰川。基于联合AMS14核心DYZK1沉积标明日期在的C在亚底部侧面上Huanghe河三角洲和声学的顺序沉没了，phytolith分析在96件沉积样品上被执行。谷物尺寸参数，磁性的危险性与biostratum的垂直变化被相结合重建在Huanghe河三角洲的paleo沉积、气候的条件。在索引参数有一条重要垂直变化法律的学习结果表演，和Huanghe河三角洲的那沉积环境经历了河的facies-sealand转变的进化进程外形潮汐的完全外形浅海的faciesdelta外形自从26.0kaB。P...phytolith分析结果如下。第一，phytoliths被划分成矛尖状，光滑伸长，多刺伸长，一种特殊格律，长矩形，bulliform和其它类型。在不同sedimental环境，phytolith内容定期变化，显示phytolith在沉积环境有的一样装配稳定性的某个度。第二，矛尖状，phytoliths的光滑伸长和多刺伸长范畴在潮汐的扁平的外形和三角洲免职有更大的内容，当时一在浅海的外形的更小的内容和河的外形环境。通过变化系数的比较分析，第三，在沉积的主要phytolith范畴的内容在sealand转变外形和河的外形免职有一个更大的变化振幅，当在tidalflat外形和三角洲外形免职是更稳定的时。