《大气科学进展AdvancesinAtmosphericSciences》论文投稿模板.docx

2345678910111213141516171819ASampleAASWordFile1.ihuaWANGCorresponding author : Lihua WANG Email: aas1Insertfootnote,andJohnSMITH2xInstituteofAtmosphericPhysics,ChineseAcademyofSciences,Beijing100029,China2InternationalPacificResearchCenter,UniversityofHawaiiatManoaHonolulu,Hawaii96822,USAABSTRACTAbrief,conciseabstractisrequiredatthebeginningofeachmanuscript.Theabstractshouldsummarizetheprincipalconclusionsarrivedatinthepaperandthemethodsusedtoreachthem.Theabstractshouldbe250wordsorlessinlength.Unlessabsolutelyessential,theabstractshouldcontainnomathematicalexpressionsandshouldrefrainfromincludingcitationsorfootnotes,andshouldnotusethefirstperson.Thetextintheabstractandthroughoutthewholemanuscriptshouldbedouble-spaced.Keywords:4-6keywordsshouldbeprovided.ArticleHighlights: 140characterlimitincludingspaces 140characterlimitincludingspaces 140characterlimitincludingspaces(Highlightsaretwotofourresult-orientedpointsthatprovidereaderswithanat-a-glanceoverviewofthemainfindingsofyourarticle.EachHighlightmustbelessthan140characters,includingspaces,andtheHighlightstogethermustclearlyconveyonlytheresultsofthestudy.Ideas,conceptsandmethodsarebestsavedfortheabstract.)20212223242526272829303132333435363738391. IntroductionThisdocumentprovidesauthorswiththebasicAdvancesinAtmosphericSciences(AAS)formattingguidelines.Thefollowingsectionsoutlinetheguidelinesandformattingfortext,figures,andtablesusingMicrosoftWord.AmorethoroughreviewofallmanuscriptrequirementscanbefoundintheAASAuthorGuide.Thelengthofthemanuscriptshouldbewithin6000wordsandthereshouldbenomorethan10figures.2. Text2.1.1.1 Thetext(12-point,TimesNewRoman)shouldbesetinonecolumnanddividedintosections,eachwithaseparateheadingandnumberedconsecutivelyusingthefollowingformat.2.1.1.2 1.evel2heading2.1.1.3 1.evel3heading2.1.1.4 1.evel4heading2.2 MathematicalformulasandtermsMathematicalformulascanappearasdisplayequationsorin-lineequations.Displayequationsarecenteredontheirownlineandareusuallynumbered,althoughthisisnotcompulsory.In-lineequationsappearrun-oninthetext.Pleaseensureallsymbolsaredefinedinthetextthatfollowsand,whencitingdisplayequations,useEq.(X),whereXistheequationnumber.4041424344454647484950515253545556575859606162WhenusingMicrosoftWordtoprepareamanuscript,useMathTypefordisplayequationsandothercomplicatedmathematicalexpressions.EquationnumbersshouldbegivenoutsideofMathTypeandsurroundedbyparentheses,suchas(1).Throughoutthepaper,pleaseensurethatallvariablesaresetinitalicfont.Ifthereareanyvectorormatrix/tensorquantities,theseshouldbesetinitalic+boldfont.Mathematicaltermsnotsetinitalics(i.e.inromanfont)includeuppercaseGreekletters,mostmathematicalfunctions(suchassinandIn),andmostmultiple-characterquantities,e.g.relativehumidity(RH).Thesequantitiesaresetromansothattheywillnotappeartobeproductsofvariables(e.g.sothatRHisnotconfusedwithR×H).Similarly,subscriptsthatarewordsorabbreviationsarenormallysetasroman,evenwhenthevariablewiththesubscriptissetitalic.Superscriptsshouldbeusedtorepresentexponentsorthetransposeofamatrix.Inallothercases,subscriptsshouldbeused.Twosubscriptsshouldbeseparatedbyacomma.3Figuresandtables3.1 FiguresFiguresoftenposetoughproblemsforbotheditorsandpublishers.Inthissection,detailedinstructionsforpreparingsuccessfulfiguresareprovided.Pleasefollowthestepsbelowtoproduceacceptablefiguresthathelpfacilitateasmoothpublicationprocess.AuFiguresFAQs''isalsoprovided(below),whichgivesanswerstothemostcommonproblemsrelatingtofiguresthatoccurduringthepublishingprocess.Mostimportantly,vector-basedgraphics(e.g.PS,PDF,AdobeIllustrator)arepreferred.Eachfigureshouldbeembeddedinthebodyofthemanuscriptascloseaspossibletoitscitationfollowingaparagraphorsection.63646566676869707172737475763.1.1 Tipsforauthorswhenpreparingfigures(1) Aimtoproduceyourfiguresat100%thepublicationsize.Figuresareadjustedintotwosizesforthepublishedproduct:one-columnsizingatapproximately60-80mmwide(Fig.1);andtwo-columnsizingatapproximately120-160mmwide.Step1.Tbresizeapicture,onthePictureToolsFormattab,intheSizegroup,enterthenewmeasurementsintotheHeightandWidthboxes.Pleaseproducethefiguresas100%ofthepublicationsize.Forthepublicationsize,figuresareadjustedintothreesizes,one-columnsizeofabout70mmwideztwo*columnsizeofabout140mmwideandthree-columnsizeof160mmwide.Step 3. If the fonts in your figures are smaller than the inserted text, please increase the font sizes.Step2.Tocomparethefontsizes,pleaseinsertanexampletextbehindyourpublicationsizedfigure.ChooseArialfontstylefromthedrop-downlistgiven,andchangesthesizeofthefontto9.Fig.1.Figuresareadjustedintotwosizesforthepublishedproduct:one-columnsizingatapproximately60-80mmwide;andtwo-columnsizingatapproximately120-160mmwide.(2) Ensureallannotation/labellinginyourfiguresisreadableinthefbntsfntsizesyouhaveused.ThepreferredfontandsizeforfigureIabeIlingZannotationisArial9pt.Ifotherfontsarepreferred/necessary,pleasechoosethemcarefullyandensurethattheyareallembedded.Ifitisdifficultforyoutoembedallthefonts,pleaseconvertthemtopaths77787980818283848586878889909192(oroutlines).Forexample,pleasecreatefontoutlinesforfiguresdrawninAdobeAcrobatIllustratortoavoidthembeingtransformedorremoved(Fig.2).Fig. 2. Temporal evolution of the Nino3.4 index for three reference ENSO events (referred to as ENSO-1, ENSO-2, ENSO-3) modeled by the ICM. The colored curves denote the corresponding ENSO (refer to the legend in the top-right corner of the figure), which are chosen to be “true” states as comparisons with prediction experiments. The notation (-1) denotes the year before the ENSO event, (O) denotes the year of the ENSO onset phase, and (1) represents the following year. The spring season, when there is a sharp drop-off in the correlation between predictions and observations associated with ENSO, is represented by yellow bars. The times between the black points are the start months of predictions over the period from July(-1) to June(I), with a one-month interval.Xpu 一OCN(3) At100%thepublicationsize,theresolutionforgraphicsfilesmustbe300-600dots-per-inchresolution(dpi)forcolorandgray-scaleimages,andatleast600dpiforblackandwhitelineimages.Pleasenotethatenlargementoffigureswilldecreasethe93949596979899100101102103104resolution.Forexample,a400dpiimagescaledat200%becomes200dpi(Fig.3).(o)(b)Fig. 3. Composited 200 hPa GH anomalies (units: gpm) 5-10 days prior to (a) minor SSWs and (d) major SSWs, derived from the NCEP-NCAR reanalysis dataset. The anomalies over dotted regions are statistically significant above the 99% confidence level according to the Student,s r-test. (b, e) Wavenumber-I and (c, f) wavenumber-2 components of 200 hPa height anomalies preceding (b, c) minor SSWs and (e, f) major SSWs, shown by contours (contour intervals: ±10, ±20, ±30 gpm). The color-filled contours in (b, e) represent the climatology of wavenumber 1 and the color-filled contours in (c, f) represent the climatology of wavenumber 2.105106107108109110111112113114115116117118119120121122(4) Inalmostallcircumstances,thelinethicknessforlines,numbers,andwordsshouldbeatleast0.2pt.Otherwise,theymayappearbrokenordisappearcompletelyinthefinalpublication.Pleasenotethatareductioninfiguresizewillmakethelineweightthinner.Forexample,a1-ptlinescaledat50%becomes0.5-pt(Fig.4).Fig.4.(a)Observed(black)andsimulated(blue)TCtrackandobservedSSTat0000UTC16July2014.(b)Observed(solid)andsimulated(dashed)TCintensity,intermsofmaximumsustained10-mwindspeed(black;units:ms_1)andcentralminimumsealevelpressure(gray;units:hPa).(5) Informationthatisclearlyexplainedinthefigurecaptionshouldnotberepeatedinthefigureannotation.Pleaseaimtomakeyourfiguresbothreadableandconcise.(6) Foraxistitles,pleaseonlycapitalizethefirstletterofthefirstword(unlesssubsequentwordsarepropernouns).(7) Itisbettertodenotecombinedunitswithanegativeexponentthanasolidus(forward-slash).Pleasealsoensurethereisaone-letterspacebetweenunitswithdifferentsymbols.123124125126127128129130131132133134135136137138139140141142143144145(8) Forsubfigures,letteredlabels,i.e.(a),(b),(c)etc.,shouldbepositioned(preferablyinthecorners)inawaythatdoesnotobscureotherpartsofthefigure,andthepositioningshouldbeconsistentamongallsubfigures.(9) Forcolorfigures,CMYKisrequiredfortheprintversionofthejournal.Authorsshouldclearlyindicatewhichfiguresareintendedtobepublishedincolorwhensubmitting.Forfiguresincolorbutnotintendedtobepublishedincolor,itisstronglyrecommendedthatyoureproducetheminblackandwhitetoensuregoodqualityprinting.3.1.2 FiguresFAQs(1) Whyismyfigurelabellingfuzzyorsaw-toothed?Figuresareconvertedinto.epsformatbeforebeingadaptedintoourtypesettingsystem.As.epsformatisvector-based,forfiguresinpixel-basedformats(e.g.jpg,.bmp,.psd,.gif),afterconversion,thequalitywillbegreatlydiminishedandmightappearfuzzy.(2) Whyisthereashadowinmyfigure?InsertionoffiguresintowordorPPTmightcreateashadow.Tryprovidingusthefiguresinsourceformat.(3) Whyshouldlinethicknessesbeatleast0.2pt?Theprintresolutionislowerthanthefigureitself.ThelineswillappearbrokeninsteadOfcontinuousinthefinalprintedproductforlinethicknesseslowerthan0.2pt.(4) WhatisCMYK?CMYK(cyan,magenta,yellow,black)figuresarewidelyusedforprinting.(5) Whydoallthefontsneedtobeembeddedorconvertedtopathsoroutlines?Itisrecommendedthatallfontsareembeddedwhenfirstcreated.Ifitisdifficulttoembedthefontsinthefigure-drawingsoftware,thealternativeistocreateoutlinesforthefontsused.Insomecases,ifthefontsarenotembeddedorcreatedwithoutlines,theywillbeconvertedtoatotallydifferentfontorbecomelostwhenconvertedtoanotherformat.3.2 TablesTablesshouldbenumbered,haveacaption(abovethetable),andmentionedspecificallyinthetext(Table1),captionsshouldbedouble-spaced.Tablesshouldbeembeddedinthebodyofthemanuscriptascloseaspossibletoitscitationfollowingaparagraphorsectionbreak(WeunderstandthisplacementmaynotalwaysbepossibleforauthorsusingLaTeX).Table1.Thisisasampletablecaptionandtablelayout.Enterasmanytablesasnecessaryattheendofyourmanuscript.Trendintheatmosphericheatsource/sinkEanditscomponentsovertheCE-TPandW-TP,inunitsofWm_2(10yr)-1.TheanalysisperiodforSHandLHis1980-2003,andforRCitis1984-2004.RegionComponentMAMJJASONDJFAnnualSE-TPSH-5.4-3.1-2.6-2.3-3.4LH1.50.50.40.30.7RC-8.1一9.7-14.4-12.7-11.2E-12.0-12.3-16.6-14.7-13.9W-TPSH-3.0-6.10.21.1-2.0LH-1.41.3-1.60.40.3RC4.5-3.6-7.0-1.4-1.8E0.1-8.4-8.40.1-4.21461471481491501511521531541551561571581591601611621631641651661671681691701711721731741751761771781791801811821831841851861871884.CitationsandreferencesFollowingtheguidelinesforcitationsandreferencescanexpeditethetimetakentoprocessyourmanuscript.4.1 InstructionsforcitationsCitationstostandardreferencesinthetextshouldconsistofthenameoftheauthorandtheyearofpublication-forexample,Wang(1990)or(Wang,1990).Iftherearethreeormoreauthors,statethefirstauthor,ssurname,followedby,etal.andtheyearofpublication一forexample,Wangetal.(1990)or(Wangetal.,1990).Whentherearetwoormorepapersbythesameauthororauthorsinthesameyear,distinguishingletters(a,b,c,etc.)shouldbeaddedtotheyearinboththecitationinthetextandthereferencelisting-forexample,Wang(1990a).Formultiplecitationsbyoneauthor,separateyearsbycommas一forexample,Wang(1989,1990)or(Wang,1989,1990).Separatemultiplecitationsbydifferentauthorswithinthesameparenthesesbysemicolonsforexample,(Wang,1990;Li,1991)or(Wang,1989,1990;Li,1991).4.2 InstructionsforreferencesReferencesshouldbelistedalphabetically,withoutnumbering,attheendofthepaper.Referencesmustbecompleteandproperlyformatted,andonlyliteraturecitedinthetextshouldbelisted.(1) Journalpapers:Author(s),publicationyear:Articletitle.Journalname,volume,pagerange.Forexample,Boville,B.A.,andJ.W.Hurrell,1998:AcomparisonoftheatmosphericcirculationssimulatedbytheCCM3andCSMl.J.Climate,11,1327-1341.189190191192193194195196197198199200201202203204205206207208209210211(2) Books:Author(s),publicationyear:BookTitle.Publisher,totalpages.Forexample,Pedlosky,J.,1987:GeophysicalFluidDynamics.2nded.,Springer-Verlag,71Opp.(3) formbookchapters:Author(s),publicationyear:chaptertitle.BookTitle,Editor(s),Publisher,pagerange.Forexample,Zhang,R.H.,andJ.P.Chao,1993:Mechanismsofinterannualvariationsinasimpleairseacoupledmodelinthetropics.ClimateVariability,D.H.Ye,etal.,Eds.,ChinaMeteorologicalPress,Beijing,236-244.(4) Multi-volumebookchapters:Author(s),publicationyear:chaptertitle.BookTitle,Editor(s),VolumeNo.,Publisher,pagerange.Tukey,J.W.,1993:Theproblemofmultiplecomparisons.MultipleComparison:1948-1983,H.I.Braun,Ed.,Vol.VIII,TheCollectedWorksofJohnW.Tnkey,ChapmanHall,1-300.(4)Otherexamples:Presentationataconference:1.hermitte,R.,andM.Gilet,1976:Acquisitionandprocessingoftri-Dopplerradardata.Preprints,17thConf.onRadarMeteorology,Seattle,WA,Amer.Meteor.Soc.,1-6.Technicalreport:Rogers,D.P.,andCoauthors,2005:THORPEXInternationalResearchImplementationPlan.WMO/TD-No.1258,96pp.212213214215216217218219220221222223224225226227228229230231232233Acknowledgments.Keeptheacknowledgementssectionasbriefaspossiblebyacknowledgingonlydirectassistanceinyourresearchandwriting.Financialsupportfortheworkshouldbeacknowledgedhereratherthanasfootnotestothetitle.REFERENCESDuan,A.M.,G.X.Wu,Y.M.Liu,Y.M.Ma,andP.Zhao,2012:WeatherandclimateeffectsoftheTibetanPlateau.Adv.Atmos.Sci.,29(5),978-992,doi:10.1007s00376-012-1220-y.Hamilton,K.,2006:Highresolutionglobalmodelingoftheatmosphericcirculation.Adv.Atmos.Sci.,23(6),842-8561.hermitte,R.,andM.Gilet,1976:Acquisitionandprocessingoftri-Dopplerradardata.Preprints,17thConf,onRadarMeteorology,Seattle,WA,Amer.Meteor.Soc.,1-6.Meixner,T.,L.A.Bastidas,H.V.Gupta,andR.C.Bales,2002:Multicriteriaparameterestimationofmodelsofstreamchemicalcomposition.WaterResour.Res.,38,1027,doi:10.10292000WR(X)0112.NWS,1999:AVisionfortheNationalWeatherService:RoadMapfortheFuture.NationalAcademyofSciences,NASPress,WashingtonD.C.,75pp.Pedlosky,J.,1987:GeophysicalFluidDynamics.2nded.,Springer-Verlag,71Opp.Rogers,D.P.,andCoauthors,2005:THORPEXInternationalResearchImplementationPlan.WMO/TD-No.1258,96pp.Tukey,J.W.,1993:Theproblemofmultiplecomparisons.MultipleComparisons:1948-1983,H.I.Braun,Ed.,Vol.VlII,TheCollectedWOYkSofJohnW.Tukey,ChapmanHall,1-300.234Yan,H.M.,C.Y.Li,andW.Zhou,2009:Influenceofsubtropicaldipolepatternin235southernIndianOceanonENSOevent.ChineseJournalofGeophysics,52(10),2362436-2449.(inChinese)2