教育资源为主的文档平台

当前位置: 查字典文档网> 所有文档分类> 高等教育> 工学> ClimateDataChallengesInThe21stCentury

ClimateDataChallengesInThe21stCentury

上传者:敬大德
|
上传时间:2015-04-15
|
次下载

ClimateDataChallengesInThe21stCentury

PERSPECTIVE

ciatedwithourunderstandingofhowtheclimatesystembehaves.

ClimateDataChallengesInadditiontothealreadylargebodyofdigitalinstrumentaldataavailableindiverseholdingsinthe21stCentury

aroundtheglobe,asubstantialnumberofcriticalobservations,suchasmanyearlytemperatureob-servations,arenotyetwidelyavailableasdigitalJonathanT.Overpeck,1*GeraldA.Meehl,2SandrineBony,3DavidR.Easterling4

records.ItisimportanttocreateandmaintaincentralrepositoriesofthesedatainamannerthatClimatedataaredramaticallyincreasinginvolumeandcomplexity,justastheusersofthesefirmlydefinestheoriginandnatureofthedataanddatainthescientificcommunityandthepublicarerapidlyincreasinginnumber.Anewparadigmalsoensuresthattheyarefreelyavailable(1,2).Inofmoreopen,user-friendlydataaccessisneededtoensurethatsocietycanreducevulnerabilityaddition,anincreasingarrayofpaleoclimaticproxytoclimatevariabilityandchange,whileatthesametimeexploitingopportunitiesthatwilloccur.recordsfromhumanandnaturalarchives,suchasC

historicaldocuments,trees,sediments,caves,corals,limatevariabilityandchange,bothnaturalevolutionofclimate.Inevitably,thereareuncer-andicecores,arebeinggenerated.Theserecordsandanthropogenic,exertconsiderablein-taintiesintheobservationalrecordsthatneedtoareparticularlyhelpfulinunderstandingclimatefluencesonhumanandnaturalsystems.betranslatedintothedegreeofconfidenceasso-

variabilitybeforetheperiodofinstrumentaldata,

Theseinfluencesdrivethescientificquestforanunderstandingofhowclimatebehavedinthepastandwillbehaveinthefuture.Thisunderstandingiscriticalforsupportingtheneedsofanever-broadeningspectrumofsociety’sdecision-makersastheystrivetodealwiththeinfluencesofEarth’sclimateatglobaltolocalscales.Ourunderstand-ingofhowtheclimatesystemfunctionsisbuiltonafoundationofclimatedata,bothobservedandsimulated(Fig.1).Althoughresearchscientistshavebeenthemainusersofthesedata,anincreasingnumberofresourcemanagers(workinginfieldssuchaswater,publiclands,health,andmarineresources)needandareseekingaccesstoclimatedatatoinformtheirdecisions,justasagrowingrangeofpolicy-makersrelyonclimatedatatodevelopclimatechangestrategies.Quiteliterally,climatedataprovidethebackboneforbillion-dollardecisions.Withthisgravitycomesthere-sponsibilitytocurateclimatedataandshareitmorefreely,usefully,andreadilythaneverbefore.TheExplodingVolumeofClimateData

Documentingthepastbehavioroftheclimatesystem,aswellasdetectingchangesandtheircauses,requirestheuseofdatafrominstrumental,paleoclimatic,satellite,andmodel-basedsources.Theearliestinstrumental(thermometerandba-rometer)recordsstretchbacktothemid-tolate1600s,althoughwidespreadland-andship-basedobservationswerenotinitiateduntiltheearlytoFig.1.Climatedatafromobservationsandclimatemodelsimulationsarecriticalforunderstandingthepastmid-1800s,mostlyinsupportofweatherfore-andpredictingthefuture.Increasingly,theclimatedataenterprisemustservebothscientistandnonscientistcastingandanalysis.Changesinobservationsequallywellintermofobserved(left)andfuture(right)climatevariabilityandchange.Observations,models,throughtime,duetoshiftsinobservingprac-research,andunderstandingareallunderpinnedbyclimatedata,andallinturninformusesinsocietysuchtices,instrumentation,andlanduse,havemadeitasthoseshownsurroundingthearrow.Theglobeatleftshowsobservedannualmeansurfacetemperaturenecessarytodevelopandapplyadvanceddata-anomalies(2006–2010)fromthe1951–1980baseperiodaverage[NASAdataaredescribedin(20)].Arcticprocessingalgorithmsinordertodescribethetime

sea-iceextentisthe5-year(2006–2010)June-July-Augustaverage,excludingsea-iceconcentrationslessthan10%[NOAAdataaredescribedin(21)].Theglobeatrightdepictsprojectedsurfacetemperature1

anomaliesforanexamplefive-memberannualmeanensembleaveragefromaclimatemodel(CCSM4),InstituteoftheEnvironment,845NorthParkAvenue,Suite532,UniversityofArizona,Tucson,AZ85721,USA.2National2081–2100minusthe1986–2005average,forthefuturegreenhousegasandaerosolemissionscenarioCenterforAtmosphericResearch,Boulder,CO,USA.3CNRS,RCP8.5(22).Thesea-iceextentfromthemodelisa5-year(2096–2100)June-July-Augustensembleaverage,LaboratoiredeMétéorologieDynamique,InstitutPierre-Simonexcludingsea-iceconcentrationslessthan10%.TheleftsideofthetimeseriesatbottomisannualmeanLaplace,observedgloballyaveragedsurfacetemperatures(20),andtherightsidedepictsfutureprojectionsforfive-4

UniversitéPierreetMarieCurie,Paris,France.NationalOceanicandAtmosphericAdministration(NOAA)/memberensembleaveragesfromCCSM4forthreeemissionscenarios(RCP2.6,RCP4.5,andRCP8.5).TheNationalClimaticDataCenter,Asheville,NC,USA.magnitudeoffutureclimatechangedependsonwhatsocietydecidestodonowintermsofemissions*Towhomcorrespondenceshouldbeaddressed.E-mail:

内容需要下载文档才能查看

reductions.TakinglittleactionproducesthegreatestwarmingasreflectedbytheRCP8.5trajectory,whereasjto@email.arizona.edu

aggressivereductionsasrepresentedbyRCP2.6resultinstabilizedwarmingatamuchlowerlevel.

70011FEBRUARY2011

VOL331

SCIENCE

http://wendang.chazidian.com

Downloaded from http://wendang.chazidian.com on March 17, 2015

SPECIALSECTION

overcenturytomillennialtimescales,throughperiodsofpastabruptclimatechange,andduringtimeswhenclimateforcingwassubstantiallydif-ferentfromthatoftoday(3)—allcriticalforunder-standingwhattheclimateofthefutureislikelytobe.Someoftheserecordshavebeencentrallyarchived(4),butmanyhavenotoraredescribedonlyinisolatedreferences.

Anotherkeysourceofclimatedataisspace-borneinstruments.Thedevelopmentoflong-term,high-qualityclimateobservationsfromsatellitesismoredifficultthanfromsurface-basedinstru-mentaldata,becauseindividualsatellitesandtheirinstrumentshaveshortlifespans(typicallyafewyears),overwhichtheirorbitsandsensitiv-itiescanchange.Theseproblemsrequiretheuseofadvanceddata-processingtechniques,andtheresultingdataarepronetobeingreprocessedaspreviouslyunknownproblemsarediscoveredovertime.Inaddition,gapsintherecordsandsystem-aticerrorsbetweensatellites(oralackofoverlap-pingcalibrationperiods)maketheincreasinglyimportantconstructionofcoherentclimatedatarecordsmoreofachallenge(5).

Athirdbroadtypeofdataismodel-based“reanalyses”:hybridmodel-observationaldatasetscreatedbyassimilatingobservationsintoaglobalorregionalforecastmodelforagiventimeperiod(suchas1958tothepresent).Theseprovidephysicallyconsistentandexpandeddepictionsoftheobservedtime-evolvingclimatesystemandhavebecomeindispensableinclimatesystemresearch.Thefutureofreanalysisrestsinthees-tablishmentofdedicatedeffortsthatincludefrozenmodelversionsandallowreprocessingofallobservationaldatafieldsasmodelsandinputdatasetsimprove.Futurereanalysismeth-odswillincludemorediverseobservationaldatatypes(suchasatmosphericchemistry,bio-spheric,oceanographic,andcryosphericdata)andlongertimescales(includingpaleoclimatictimescales).

Finally,therehasbeenanexplosionindatafromnumericalclimatemodelsimulations,whichhaveincreasedgreatlyincomplexityandsize.Datafromthesemodelsareexpectedtobecomethelargestandthefastest-growingsegmentoftheglobalarchive(Fig.2).Thearchivingandsharingofoutputfromclimatemodels,particularlythoserunwithacommonexperimentalframework,beganinthemid-1990s,startingwithoutputfromtheearlyglobalcoupledatmosphere-oceangeneralcirculationmodels(AOGCMs)usedformakingfutureclimatechangeprojections(6).ThisledtotheCoupledModelIntercomparisonProject(CMIP),organizedbytheWorldClimateResearchProgram(WCRP),invitingallthemodelinggroupstomakeincreasinglyrealisticsimulationsof20th-centuryandpossiblefuture21st-centuryclimates(7–9).Recently,CMIP3involved16internationalmodelinggroupsfrom11countries,using23modelsandsubmitting36terabytesofmodeldata,allarchivedbythe

atmosphericdynamicsandregionalprecipitation,aswellaspredictingnat-uralclimatevariabilityandhowmuchEarth,andlocalpartsofit,couldwarmforagivenamountofgreenhousegasforcing.Newhigh-resolutionactivere-motesensingobservationsfromsatel-liteinstruments(suchasCALIPSOlidarorCloudSatradar)arerevealingtheverticaldistributionofcloudsforthefirsttime.However,tofacilitatethecom-parisonofmodeloutputswiththesecomplexnewobservationseffectively,ithasbeennecessarytodevelopanddistributenewdiagnostictools(re-ferredtoas“observationsimulators”)visualizingwhatthesesatelliteswouldseeiftheywereflyingabovethesim-ulatedatmosphereofamodel(11,12).Thankstothesedevelopments,itwill

Fig.2.Thevolumeofworldwideclimatedataisexpandingsoonbepossibletorigorouslyassessrapidly,creatingchallengesforbothphysicalarchivingandsharing,therealismofcloudsimulationsintheaswellasforeaseofaccessandfindingwhat’sneeded,partic-latestgenerationofmodels;fortheularlyifyouarenotaclimatescientist.Thefigureshowsthepriceofanadditional6%[160tera-projectedincreaseinglobalclimatedataholdingsforclimatebytes(TB)]ofCMIP5-relatedclimatemodels,remotelysenseddata,andinsituinstrumental/proxy

datathatmustbeshared.

data.

Climatechangemodelinghasevolvedinjust5yearsfromrunning

ProgramforClimateModelDiagnosisandIn-afewAOGCMexperimentswithasinglecategorytercomparison(PCMDI),signalinga“newerainofmodel,torunningmanymoreexperimentswithclimatechangeresearch”(10).Thisactivityhasamuchlargerprofusionofmodelsofincreasingmadeitpossibleforanyonetoopenlyaccesstheseresolutionandcomplexity.First-generationEarthstate-of-the-artclimatemodeloutputsforanalysissystemmodels(ESMs)arenowbeingrunaspart

ofthecurrentCMIP5exercise(13,14).ESMsandresearch.

Climatemodeldatahavebeenarchivedandincludeatleastaninteractivecarboncyclecoupledaccessed,exchanged,andsharedprimarilywithintothetraditionalAOGCMs,whichhaveatmo-thephysicalclimatescienceresearchcommunity,sphere,ocean,land,andsea-icecomponents.Also,althoughtherehasbeengrowinginterestinthehigh-resolutionclimatemodels(suchasthosewithuseoftheseclimatemodeldatabyothercom-20-kmgridspacing)arerunfortimeslices,pastmunitiesofresearchers.CMIPwasdesignedtoandfuture,forintegrationsofadecadeortwoinprovidethisbroaderaccesstoclimatemodeloutputordertoobtainabetterquantificationofregionalforresearchersfromawiderangeofcommunities.climatechangeandsmaller-scalephenomenasuchTheIntergovernmentalPanelonClimateChangeashurricanes[forexample,see(15)].Thenetresult(IPCC)wasalsoabletouseCMIPmultimodeldataisahugeincreaseindatavolume(Fig.2).Earlysetstoprovidestate-of-the-artassessmentsofwhatphasesoftheCMIPprojectinvolvedlessthanthemodelsasagroupindicateaboutpossible1TBofmodeldata,whereasCMIP3archivedfutureclimatechange(10).Nowclimatemodels36TB,andCMIP5isexpectedtomakeavail-arebeginningtobeusedformuchmorethanable2.5petabytes(PB).Newcapabilitiesoftheclimateresearch.Inparticular,theyareexpectedtoEarthSystemGridportalwillprovidedistributedinformdecisionsthatsocietymusttakeatglobaltoaccesstoalargepartofthisnewmodeloutputlocalscalestoadapttonaturalclimatevariationsas(16),makingitpossibleformodelinggroupstowellastoanthropogenicclimatechange,andtosharedatafromdistributedlocalserverswithguidetheimplementationofpossiblemitigationWeb-basedaccesstools.Modeldatathusdonotmeasures.Thisputsnewdemandsonthevariety,needtobecentrallyarchivedbutcanbeaccessedscale,andavailabilityofobservationaldataneededinadistributedfashion.Clearly,thisisanformodelevaluationanddevelopment,andex-exampletobefollowedmorebroadly,withthepands,yetagain,thevolumeofclimatedatathatcaveatthatthesafetyandreliabilityoflong-term

archivesofthesedatamustnotbejeopardized.mustbesharedopenlyandefficiently(Fig.2).

Anillustrationofthechallengesandpossi-bilitiesposedbythefutureinteractionoffine-MeetingtheNeedsofaWideRangeofUsersscaleobservationaldatawithmorecomplexmodelsTheburgeoningtypesandvolumeofclimatedataistheevaluationofcloudsandthehydrologicaloneconstituteamajorchallengetothecli-cycle.Theseprocessesarecriticalforsimulatingmateresearchcommunityanditsfundingbodies.

内容需要下载文档才能查看

http://wendang.chazidian.comSCIENCEVOL33111FEBRUARY2011701

Institutionalcapacitymustexisttoproduce,format,document,andshareallthesedata,while,atthesametime,amuchlargercommunityofdiverseusersclamorstoaccess,understand,andusecli-matedata.Theseincludeanever-increasingrangeofscientists(ecologists,hydrologists,socialsci-entists,etc.)anddecision-makersinsocietywhohaverealmoney,livelihoods,andevenlivesatstake(resourcemanagers,farmers,publichealthofficials,andothers).Keyusersalsoincludethosewithpublicresponsibilities,aswellastheirconstituentsinthegeneralpublicwhomustsup-portandunderstanddecisionsbeingmadeontheirbehalf.Asaresult,climatescientistsmustnotonlysharedataamongthemselves,buttheymustalsomeetagrowingobligationtofacilitateaccesstodataforthoseoutsidetheircommu-nityand,indoingso,respondtothisbroaderusercommunitytoensurethatthedataareasusefulaspossible.

InadditiontothelatestIPCCassessment,variousongoingnationalclimateassessmentandclimateservicesactivitiesarebeinginitiatedthatwillneedtoaccessanduseclimatedata,justasagrowingnumberofclimateadaptationandmiti-gationeffortsaroundtheglobewillneedtobebetterinformedbyclimatedata.Theseeffortswillsucceedonlyifclimatedataaremadereadilyac-cessibleinformsusefultoscientistsandnon-scientistsalike.

TheFutureofClimateData:AnEmergingParadigm

Thus,twomajorchallengesforclimatesciencerevolvearounddata:ensuringthattheever-expandingvolumesofdata(Fig.2)areeasilyandfreelyavailabletoenablenewscientificresearch,andmakingsurethatthesedataandtheresultsthatdependonthemareusefultoandunder-standablebyabroadinterdisciplinaryaudience.Anewparadigmthatjoinstraditionalclimatere-searchwithresearchonclimateadaptation,ser-vices,assessment,andapplicationswillrequirestrengthenedfundingforthedevelopmentandanalysisofclimatemodels,aswellasforthebroaderclimatedataenterprise.Increasedsupportfromthefundingagenciesisneededtoenhancedataaccess,manipulation,andmodelingtools;improveclimatesystemunderstanding;articu-latemodellimitations;andensurethattheob-servationsnecessarytounderpinitallaremade.Otherwise,climatesciencewillsuffer,andtheclimateinformationneededbysociety—climateassessment,services,andadaptationcapability—willnotonlyfallshortofitspotentialtoreducethevulnerabilityofhumanandnaturalsystemstoclimatevariabilityandchange,butwillalsocausesocietytomissoutonopportunitiesthatwillinevitablyariseinthefaceofchangingconditions.

Atpresent,abouthalfoftheinternationalmod-elinggroupsarerestrictedfromsharingdigitalclimatemodeldatabeyondtheresearchcom-munitybecauseofgovernmentalinterestinthesaleofintellectualpropertyforcommercialap-plications;thesameholdstrueforsomeobser-vationaldata.Openandfreeavailabilityofmodeldata,observations,andthesoftwareusedforpro-cessingiscrucialtoallaspectsofthenewpar-adigm.Governmentsthatcurrentlyrestricteithermodeloutputorobserveddatadistributionmustbeconvincedthatitisinthebestinterestsofeveryonethatallclimatedatabemadeopenlyavailabletoallusers,includingthoseengagedinresearchandapplications.Internationalagree-mentsmusteliminatedatarestrictions,justasjour-nalsandfundingagenciesshouldrequireeasyaccesstoalldataassociatedwiththepaperstheypublishandtheworktheyfund.

Theoptimaluseofclimatedatarequiresamoreeffectiveinterdisciplinarycommunicationofdatalimitationswithregardto,forexample,spatialandtemporalsamplinguncertainties;in-strumentchanges;quality-controlprocedures;and,inparticular,whatmodel-basedclimatepre-dictionsorprojectionsdowellandnotsowell.Thefirststepistoincreasetheaccessibilityofobservationsandhigh-resolutionsimulationstoawiderangeofusers,eitherviaafewcentralizedportals(suchasPCMDI)withbroaderrespon-sibilities,orusingamoredecentralizedapproach.Asecondstepistodevelopaninternationalde-positorysiteformodeldiagnostictools(suchassatellitesimulators)andevaluationmetricsthatwouldhelpusersassessthereliabilityofspe-cificaspectsofmodelsimulations(suchasseaice,ElNiño–SouthernOscillation,ormonsoons,droughts,andotherclimateextremes).Thekeyisthatnewdata-sharingsystemshavetobeeval-uatedandimproveduntilalltypesofinterdis-ciplinaryusersareabletobeeffectivepartnersintheuseofclimatedata.

Anincreasinglydauntingaspectofhavingtensandeventuallyhundredsofpetabytesofclimatedataopenlyavailableforanalysis(Fig.2)ishowtoactuallylookatandusethedata,allthewhileunderstandinguncertainties.Moreresourcesneedtobededicatedtothedevelopmentofso-phisticatedsoftwaretoolsforsiftingthrough,accessing,andvisualizingthemanymodelversions,experiments,andmodelfields(temperature,pre-cipitation,etc.),aswellasalloftheobserveddatathatisonline.Inparallel,itisbecomingincreas-inglyimportanttounderstandcomplexmodelresultsthroughahierarchyofmodels,includingsimpleorconceptualmodels(17).Withoutthisstep,itwillbeextremelydifficulttomakesenseofsuchhugearchivedclimatedatasetsandtoassesstherobustnessofthemodelresultsandtheconfidencethatmaybeputinthem.Again,ful-fillingtheneedsofalltypesofinterdisciplinaryusersneedstobethemetricofsuccess.

Increasingly,climatescientistsandothertypesofscientistswhoworkeffectivelyattheinterfacebetweenresearchandapplicationsareworkingcloselytogether,andeven“coproducing”knowl-VOL331

SCIENCE

edge,withclimatestakeholdersinsociety(18,19).Thesestakeholders,alongwiththeinterdisciplinarysciencecommunitythatsupportsthem,aretheusersthatmustdrivetheclimatedataenterpriseofthefuture.

ReferencesandNotes

1.C.K.Follandetal.,inTemperatureTrendsintheLowerAtmosphere:StepsforUnderstandingandReconcilingDifferences,T.R.Karl,S.J.Hassol,C.D.Miller,

W.L.Murray,Eds.(U.S.ClimateChangeScienceProgramandtheSubcommitteeonGlobalChangeResearch,Washington,DC,2006),pp.119–127.

2.D.R.Easterlingetal.,inWeatherandClimateExtremesinaChangingClimate.RegionsofFocus:NorthAmerica,Hawii,Carribbean,andU.S.PacificIslands,T.R.Karletal.,Eds.(U.S.ClimateChangeScienceProgramandtheSubcommitteeonGlobalChangeResearch,Washington,DC,2008),pp.117–126.

3.E.Jansenetal.,inClimateChange2007:ThePhysicalScienceBasis.ContributionofWorkingGroupItotheFourthAssessmentReportoftheIntergovernmentalPanelonClimateChange,S.Solomonetal.,Eds.(CambridgeUniv.Press,Cambridge,2007),pp.433–497.

4.ArchivedattheWorldDataCenterforPaleoclimatology,www.ngdc.noaa.gov/wdc/usa/paleo.html.

5.NationalResearchCouncil,ClimateDataRecordsfromEnvironmentalSatellites(NationalAcademyPress,Washington,DC,2004).

6.G.A.Meehl,G.J.Boer,C.Covey,M.Latif,R.J.Stouffer,Eos78,445(1997).

7.G.A.Meehl,G.J.Boer,C.Covey,M.Latif,R.J.Stouffer,Bull.Am.Meteorol.Soc.81,313(2000).8.G.A.Meehl,C.Covey,B.McAvaney,M.Latif,

R.J.Stouffer,Bull.Am.Meteorol.Soc.86,89(2005).9.C.Coveyetal.,GlobalPlanet.Change37,103(2003).

10.G.A.Meehletal.,Bull.Am.Meteorol.Soc.88,1383

(2007).

11.J.M.Haynes,R.T.Marchand,Z.Luo,A.Bodas-Salcedo,

G.L.Stephens,Quickbeam.Bull.Am.Meteorol.Soc.88,1723(2007).

12.H.Chepferetal.,Geophys.Res.Lett.35,L15704

(2008).

13.K.A.Hibbard,G.A.Meehl,P.Cox,P.Friedlingstein,

Eos88,217(2007).

14.K.E.Taylor,R.J.Stouffer,G.A.Meehl,Asummaryofthe

CMIP5ExperimentalDesign(2009);www-pcmdi.llnl.gov/.15.K.Oouchietal.,J.Meteorol.Soc.Jpn.84,259

(2006).

16.D.N.Williamsetal.,Bull.Am.Meteorol.Soc.90,195

(2009).

17.I.M.Held,Bull.Am.Meteorol.Soc.86,1609(2005).18.M.C.Lemos,B.J.Morehouse,GlobalEnviron.Change

Hum.PolicyDimensions15,57(2005).

19.R.S.Pulwarty,C.Simpson,C.R.Nierenberg,in

IntegratedRegionalAssessmentofGlobalClimateChange,C.G.Knight,J.Jäger,Eds.(CambridgeUniv.Press,Cambridge,2009),pp.367–393.

20.J.Hansen,R.Ruedy,M.Sato,K.Lo,Rev.Geophys.48,

RG4004(2010).

21.R.W.Reynolds,N.A.Rayner,T.M.Smith,D.C.Stokes,

W.Wang,J.Clim.15,1609(2002).

22.R.H.Mossetal.,Nature463,747(2010).

23.TheauthorsthankG.Strand[NationalCenterfor

AtmosphericResearch(NCAR)]andS.Veasey(NationalClimaticDataCenter)fortheircontributions.NOAAsupportedthiswork(J.T.O.)throughitsRegional

IntegratedSciencesandAssessmentsProgram.Portionsofthisstudywerealsosupported(G.A.M.)bytheOfficeofScience(B.E.R.),U.S.DepartmentofEnergy,CooperativeAgreementno.DE-FC02-97ER62402;andNSF.NCAR(G.A.M.)issponsoredbyNSF.10.1126/science.1197869

http://wendang.chazidian.com

内容需要下载文档才能查看

Climate Data Challenges in the 21st CenturyJonathan T. Overpeck et al.Science 331, 700 (2011);

DOI: 10.1126/science.1197869

This copy is for your personal, non-commercial use only.

If you wish to distribute this article to others, you can order high-quality copies for yourcolleagues, clients, or customers by clicking here.

Permission to republish or repurpose articles or portions of articles can be obtained byfollowing the guidelines here.

The following resources related to this article are available online at

http://wendang.chazidian.com (this information is current as of March 17, 2015 ):

Updated information and services, including high-resolution figures, can be found in the onlineversion of this article at:

http://wendang.chazidian.com/content/331/6018/700.full.html

Supporting Online Material can be found at:

http://wendang.chazidian.com/content/suppl/2011/02/10/331.6018.700.DC1.html

A list of selected additional articles on the Science Web sites related to this article can befound at:

http://wendang.chazidian.com/content/331/6018/700.full.html#related This article has been cited by 1 articles hosted by HighWire Press; see:http://wendang.chazidian.com/content/331/6018/700.full.html#related-urls This article appears in the following subject collections:Science and Policy

http://wendang.chazidian.com/cgi/collection/sci_policy

Science (print ISSN 0036-8075; online ISSN 1095-9203) is published weekly, except the last week in December, by theAmerican Association for the Advancement of Science, 1200 New York Avenue NW, Washington, DC 20005. Copyright2011 by the American Association for the Advancement of Science; all rights reserved. The title Science is aregistered trademark of AAAS.

Downloaded from http://wendang.chazidian.com on March 17, 2015

版权声明:此文档由查字典文档网用户提供,如用于商业用途请与作者联系,查字典文档网保持最终解释权!

下载文档

热门试卷

2016年四川省内江市中考化学试卷
广西钦州市高新区2017届高三11月月考政治试卷
浙江省湖州市2016-2017学年高一上学期期中考试政治试卷
浙江省湖州市2016-2017学年高二上学期期中考试政治试卷
辽宁省铁岭市协作体2017届高三上学期第三次联考政治试卷
广西钦州市钦州港区2016-2017学年高二11月月考政治试卷
广西钦州市钦州港区2017届高三11月月考政治试卷
广西钦州市钦州港区2016-2017学年高一11月月考政治试卷
广西钦州市高新区2016-2017学年高二11月月考政治试卷
广西钦州市高新区2016-2017学年高一11月月考政治试卷
山东省滨州市三校2017届第一学期阶段测试初三英语试题
四川省成都七中2017届高三一诊模拟考试文科综合试卷
2017届普通高等学校招生全国统一考试模拟试题(附答案)
重庆市永川中学高2017级上期12月月考语文试题
江西宜春三中2017届高三第一学期第二次月考文科综合试题
内蒙古赤峰二中2017届高三上学期第三次月考英语试题
2017年六年级(上)数学期末考试卷
2017人教版小学英语三年级上期末笔试题
江苏省常州西藏民族中学2016-2017学年九年级思想品德第一学期第二次阶段测试试卷
重庆市九龙坡区七校2016-2017学年上期八年级素质测查(二)语文学科试题卷
江苏省无锡市钱桥中学2016年12月八年级语文阶段性测试卷
江苏省无锡市钱桥中学2016-2017学年七年级英语12月阶段检测试卷
山东省邹城市第八中学2016-2017学年八年级12月物理第4章试题(无答案)
【人教版】河北省2015-2016学年度九年级上期末语文试题卷(附答案)
四川省简阳市阳安中学2016年12月高二月考英语试卷
四川省成都龙泉中学高三上学期2016年12月月考试题文科综合能力测试
安徽省滁州中学2016—2017学年度第一学期12月月考​高三英语试卷
山东省武城县第二中学2016.12高一年级上学期第二次月考历史试题(必修一第四、五单元)
福建省四地六校联考2016-2017学年上学期第三次月考高三化学试卷
甘肃省武威第二十三中学2016—2017学年度八年级第一学期12月月考生物试卷

网友关注

教资统考《保教知识与能力》重要考点:幼儿各年龄阶段的游戏特点
教师资格考试幼儿心理学精讲:儿童学习的发展
2014教师资格考试幼儿《教育心理学》复习资料七
2014年教师资格考试幼儿教育心理学考点:幼儿的言语
2014年教资考试幼儿心理学精讲五:乔姆斯基与心理语言学
2014教师资格考试幼儿《教育心理学》复习资料六
2014教师资格考试幼儿《教育心理学》复习资料二
教资统考《保教知识与能力》重要考点:儿童发展理论
教资统考《保教知识与能力》重要考点:婴幼儿发展
教师资格考试幼儿心理学精讲:意识发生和发展
2014教资考试幼儿《教育心理学》复习指导:亲子关系的发展
2014教师资格考试幼儿《教育心理学》复习资料一
2014年教资考试幼儿心理学精讲四:西方儿童心理学研究
2014教资考试幼儿《教育心理学》复习指导:独生子女社会性发展的问题
2014教资考试幼儿《教育心理学》复习指导:幼儿能力的发展
教师资格考试幼儿心理学精讲:婴儿记忆的发展
2014年教师资格考试幼儿教育心理学考点:幼儿的记忆
教师资格考试幼儿心理学精讲:儿童内部言语发展
2014教资考试幼儿《教育心理学》复习指导:幼儿美术活动心理一
2014年教师资格证考试幼儿园教育学案例分析二
教师资格考试幼儿心理学精讲:思维和想象
教师资格考试幼儿心理学精讲:道德行为与判断
2014教师资格考试幼儿《教育心理学》复习资料八
教师资格考试幼儿心理学精讲:依恋发展的阶段
2014年教师资格考试幼儿教育心理学考点:幼儿的注意
2014教资考试幼儿《教育心理学》复习指导:幼儿游戏活动心理
2014年教师资格考试幼儿教育心理学考点:幼儿的思维
2014教资考试幼儿《教育心理学》复习指导:游戏对幼儿心理发展的价值
教师资格考试幼儿心理学精讲:婴儿注意的发展
教师资格考试幼儿心理学精讲:依恋的类型

网友关注视频

沪教版牛津小学英语(深圳用) 四年级下册 Unit 8
第8课 对称剪纸_第一课时(二等奖)(沪书画版二年级上册)_T3784187
冀教版小学数学二年级下册第二单元《有余数除法的竖式计算》
飞翔英语—冀教版(三起)英语三年级下册Lesson 2 Cats and Dogs
【部编】人教版语文七年级下册《过松源晨炊漆公店(其五)》优质课教学视频+PPT课件+教案,江苏省
苏科版数学八年级下册9.2《中心对称和中心对称图形》
【部编】人教版语文七年级下册《老山界》优质课教学视频+PPT课件+教案,安徽省
【部编】人教版语文七年级下册《老山界》优质课教学视频+PPT课件+教案,安徽省
【部编】人教版语文七年级下册《泊秦淮》优质课教学视频+PPT课件+教案,广东省
【获奖】科粤版初三九年级化学下册第七章7.3浓稀的表示
8.对剪花样_第一课时(二等奖)(冀美版二年级上册)_T515402
沪教版牛津小学英语(深圳用) 四年级下册 Unit 7
沪教版八年级下册数学练习册20.4(2)一次函数的应用2P8
河南省名校课堂七年级下册英语第一课(2020年2月10日)
每天日常投篮练习第一天森哥打卡上脚 Nike PG 2 如何调整运球跳投手感?
外研版英语三起5年级下册(14版)Module3 Unit2
【部编】人教版语文七年级下册《泊秦淮》优质课教学视频+PPT课件+教案,辽宁省
北师大版小学数学四年级下册第15课小数乘小数一
冀教版小学数学二年级下册第二周第2课时《我们的测量》宝丰街小学庞志荣.mp4
第五单元 民族艺术的瑰宝_16. 形形色色的民族乐器_第一课时(岭南版六年级上册)_T1406126
【部编】人教版语文七年级下册《逢入京使》优质课教学视频+PPT课件+教案,安徽省
外研版英语七年级下册module3 unit1第二课时
六年级英语下册上海牛津版教材讲解 U1单词
8 随形想象_第一课时(二等奖)(沪教版二年级上册)_T3786594
【部编】人教版语文七年级下册《泊秦淮》优质课教学视频+PPT课件+教案,湖北省
第4章 幂函数、指数函数和对数函数(下)_六 指数方程和对数方程_4.7 简单的指数方程_第一课时(沪教版高一下册)_T1566237
化学九年级下册全册同步 人教版 第25集 生活中常见的盐(二)
二年级下册数学第二课
外研版英语七年级下册module3 unit2第一课时
第12章 圆锥曲线_12.7 抛物线的标准方程_第一课时(特等奖)(沪教版高二下册)_T274713