简介：本文对高中英语教学中常用的"Warmingup"形式进行一些归纳,如合作型热身,拟人型热身,情景型热身,任务型热身,并联系新教材的内容举例说明各种形式的运用.

简介：Greenhousegasesandglobalwarminghavereceivedincreasingattentioninrecentyearsandgainedaprominentplaceonnationalandinternationalagendas.In1988theUnitedStatesCongressaskedtheU.S.NationalAcademyofSciencestoconductastudyonthepolicyimplicationsofgreenhousewarming.Oneofthetasksinthestudywastoexaminemitigationoptionsanddevelopanassessmentmethodologyforthem.Thistaskwasundertakenbyapanelof19scientists,economists,andengineers.TheauthorwastheChairmanofthatpanel.Inthispaper,themethodologydeveloped-the“technologicarcosting”method-isbrieflyreviewedandthereasonsforchoosingitovereconomicmodelingwerediscussed.Itconcludeswithadiscussiononhowthegreenhousewarmingproblemmayaffecttheenergyandpowersystemofthefuture.

简介：Jiansanzhen,Tianzong(SI11),Jugu(LI16),Jianzhen(SI9),Binao(LI14)andQuchi(LI11)weregivenwarming-needlemoxibustiontotreatshoulderperiarthritisin78cases,andtheresultshowedtotaleffectiveratewas97.4%.

简介：Thefocusofthisyear'sconferenceisGlobalExtremeEvents,characterizedaslarge-scaleclimaticeffectsthathavebeenincreasinginmagnitudeandfrequency.Prof.SinyanShen,ChairmanoftheGWInternationalProgramCommittee,hasbeenleadingtheworldonGlobalExtremeEventsandEmergencyResponse.InthelongtermclimatechangewillcausetheEarthtotransittoanotherequilibriumstatethroughmanyoscillationsinclimaticpattern.Globalwarmingcausesextremeeventsandbadweatherinthenearterm.Theimmediate

简介：在带的高潮植被上在东北中国和调查从210个气象学的车站基于数据，Kira的温暖索引(Wl)，寒冷索引(Cl)，并且徐文铎的湿度索引(Hl)被采用模仿并且在气候下面预言植被eco边界的动力学在东北中国温暖。带的高潮植被的未来植被eco边界改变类型能被划分成三种类型，例如扩大植被eco边界种类(为45鈥?的Wl价值范围5掳C路月)它将在温暖的气候下面向北移动，撤退植被eco边界种类(为25鈥?的Wl价值范围5掳C路月)它将从现在的地区，和绝灭的人口种类撤退(为5鈥?的Wl价值范围5掳C路月)它将被扑灭因为生态系统t在东北中国，为纬度的15掳和2600m有差别高度。基于我们的研究结果，edificators将向北移动大约400鈥?00km，大草原植被将移动eastwords900km，和人口将向上移动大约260鈥?在山的60m如果全球温度以后增加2掳C。然而，当纬度和高度增加了，动人的距离将变得越来越短。因此，在在Daxing'an山和Changbai山的高山的冻土带地区的人口可能消失。当他们放下了策略以后对气候变化作出回应时，结果被期望供应参考到本地管理。

简介：Basedonthedataupto1999fromhydroclimatologicaldepartments,thispaperanalyzestheclimaticdivideimplicationsoftheQinlingMountainsinregionalresponsetotheprocessofclimatewarming,duetowhichthegradesofdryness/wetness(GDW)in100yearsshowthatthenorthernregionhasenteredadroughtperiod,whilethesouthernisahumidperiod.Inacourseoftenyears,theD-valueofannualaverageairtemperatureoversouthernShaanxi(theHanjiangValley)andtheCentralShaanxiPlain(theGuanzhongPlain)hasnarrowed,i.e.,theformerwithaslightchangeandthelatterwithrapidincreaseintemperature.BothregionswerearidwiththedecreaseinprecipitationD-value,namelytheplainbecamewarmerwhilethesouthwasdrier.TheQinlingMountainsplayapronouncedroleintheclimaticdivide.Therunoffcoefficient(RC)oftheWeiheRiverdecreasessynchronouslywiththatoftheHanjiangduetoclimatewarming.TheRCofWeihedroppedfrom0.2inthe1950stolessthan0.1inthe1990s.TheWeiheValley(theGuanzhongPlain)ispracticallyanaridareaduetoshortageofwater.Thesuccessive0.5,1.0℃temperatureanomalyoverChinamarks,perhaps,theimportanttransitionperiodinwhichtheenvironmentbecomesmorevulnerablethanbefore.Thestudyshowstheobvioustrendofenvironmentalaridity,whichisofhelptotheunderstandingofregionalresponsetoglobalclimatechange.

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