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

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1、2345678910111213141516171819ASampleAASWordFile1.ihuaWANGCorresponding author : Lihua WANG Email: aas1Insertfootnote,andJohnSMITH2xInstituteofAtmosphericPhysics,ChineseAcademyofSciences,Beijing100029,China2InternationalPacificResearchCenter,UniversityofHawaiiatManoaHonolulu,Hawaii96822,USAABSTRACTAbr

2、ief,conciseabstractisrequiredatthebeginningofeachmanuscript.Theabstractshouldsummarizetheprincipalconclusionsarrivedatinthepaperandthemethodsusedtoreachthem.Theabstractshouldbe250wordsorlessinlength.Unlessabsolutelyessential,theabstractshouldcontainnomathematicalexpressionsandshouldrefrainfrominclud

3、ingcitationsorfootnotes,andshouldnotusethefirstperson.Thetextintheabstractandthroughoutthewholemanuscriptshouldbedouble-spaced.Keywords:4-6keywordsshouldbeprovided.ArticleHighlights: 140characterlimitincludingspaces 140characterlimitincludingspaces 140characterlimitincludingspaces(Highlightsaretwoto

4、fourresult-orientedpointsthatprovidereaderswithanat-a-glanceoverviewofthemainfindingsofyourarticle.EachHighlightmustbelessthan140characters,includingspaces,andtheHighlightstogethermustclearlyconveyonlytheresultsofthestudy.Ideas,conceptsandmethodsarebestsavedfortheabstract.)20212223242526272829303132

5、333435363738391. IntroductionThisdocumentprovidesauthorswiththebasicAdvancesinAtmosphericSciences(AAS)formattingguidelines.Thefollowingsectionsoutlinetheguidelinesandformattingfortext,figures,andtablesusingMicrosoftWord.AmorethoroughreviewofallmanuscriptrequirementscanbefoundintheAASAuthorGuide.Thel

6、engthofthemanuscriptshouldbewithin6000wordsandthereshouldbenomorethan10figures.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.evel

7、4heading2.2 MathematicalformulasandtermsMathematicalformulascanappearasdisplayequationsorin-lineequations.Displayequationsarecenteredontheirownlineandareusuallynumbered,althoughthisisnotcompulsory.In-lineequationsappearrun-oninthetext.Pleaseensureallsymbolsaredefinedinthetextthatfollowsand,whencitin

8、gdisplayequations,useEq.(X),whereXistheequationnumber.4041424344454647484950515253545556575859606162WhenusingMicrosoftWordtoprepareamanuscript,useMathTypefordisplayequationsandothercomplicatedmathematicalexpressions.EquationnumbersshouldbegivenoutsideofMathTypeandsurroundedbyparentheses,suchas(1).Th

9、roughoutthepaper,pleaseensurethatallvariablesaresetinitalicfont.Ifthereareanyvectorormatrix/tensorquantities,theseshouldbesetinitalic+boldfont.Mathematicaltermsnotsetinitalics(i.e.inromanfont)includeuppercaseGreekletters,mostmathematicalfunctions(suchassinandIn),andmostmultiple-characterquantities,e

10、.g.relativehumidity(RH).Thesequantitiesaresetromansothattheywillnotappeartobeproductsofvariables(e.g.sothatRHisnotconfusedwithRH).Similarly,subscriptsthatarewordsorabbreviationsarenormallysetasroman,evenwhenthevariablewiththesubscriptissetitalic.Superscriptsshouldbeusedtorepresentexponentsorthetrans

11、poseofamatrix.Inallothercases,subscriptsshouldbeused.Twosubscriptsshouldbeseparatedbyacomma.3Figuresandtables3.1 FiguresFiguresoftenposetoughproblemsforbotheditorsandpublishers.Inthissection,detailedinstructionsforpreparingsuccessfulfiguresareprovided.Pleasefollowthestepsbelowtoproduceacceptablefigu

12、resthathelpfacilitateasmoothpublicationprocess.AuFiguresFAQsisalsoprovided(below),whichgivesanswerstothemostcommonproblemsrelatingtofiguresthatoccurduringthepublishingprocess.Mostimportantly,vector-basedgraphics(e.g.PS,PDF,AdobeIllustrator)arepreferred.Eachfigureshouldbeembeddedinthebodyofthemanuscr

13、iptascloseaspossibletoitscitationfollowingaparagraphorsection.63646566676869707172737475763.1.1 Tipsforauthorswhenpreparingfigures(1) Aimtoproduceyourfiguresat100%thepublicationsize.Figuresareadjustedintotwosizesforthepublishedproduct:one-columnsizingatapproximately60-80mmwide(Fig.1);andtwo-columnsi

14、zingatapproximately120-160mmwide.Step1.Tbresizeapicture,onthePictureToolsFormattab,intheSizegroup,enterthenewmeasurementsintotheHeightandWidthboxes.Pleaseproducethefiguresas100%ofthepublicationsize.Forthepublicationsize,figuresareadjustedintothreesizes,one-columnsizeofabout70mmwideztwo*columnsizeofa

15、bout140mmwideandthree-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,andchangesthesizeoft

16、hefontto9.Fig.1.Figuresareadjustedintotwosizesforthepublishedproduct:one-columnsizingatapproximately60-80mmwide;andtwo-columnsizingatapproximately120-160mmwide.(2) Ensureallannotation/labellinginyourfiguresisreadableinthefbntsfntsizesyouhaveused.ThepreferredfontandsizeforfigureIabeIlingZannotationis

17、Arial9pt.Ifotherfontsarepreferred/necessary,pleasechoosethemcarefullyandensurethattheyareallembedded.Ifitisdifficultforyoutoembedallthefonts,pleaseconvertthemtopaths77787980818283848586878889909192(oroutlines).Forexample,pleasecreatefontoutlinesforfiguresdrawninAdobeAcrobatIllustratortoavoidthembein

18、gtransformedorremoved(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 b

19、e “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 obse

20、rvations 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-inchresolut

21、ion(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 t

22、o (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 pre

23、ceding (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 2.1051061071081091101111121131141151161

24、17118119120121122(4) Inalmostallcircumstances,thelinethicknessforlines,numbers,andwordsshouldbeatleast0.2pt.Otherwise,theymayappearbrokenordisappearcompletelyinthefinalpublication.Pleasenotethatareductioninfiguresizewillmakethelineweightthinner.Forexample,a1-ptlinescaledat50%becomes0.5-pt(Fig.4).Fig

25、.4.(a)Observed(black)andsimulated(blue)TCtrackandobservedSSTat0000UTC16July2014.(b)Observed(solid)andsimulated(dashed)TCintensity,intermsofmaximumsustained10-mwindspeed(black;units:ms_1)andcentralminimumsealevelpressure(gray;units:hPa).(5) Informationthatisclearlyexplainedinthefigurecaptionshouldnot

26、berepeatedinthefigureannotation.Pleaseaimtomakeyourfiguresbothreadableandconcise.(6) Foraxistitles,pleaseonlycapitalizethefirstletterofthefirstword(unlesssubsequentwordsarepropernouns).(7) Itisbettertodenotecombinedunitswithanegativeexponentthanasolidus(forward-slash).Pleasealsoensurethereisaone-let

27、terspacebetweenunitswithdifferentsymbols.123124125126127128129130131132133134135136137138139140141142143144145(8) Forsubfigures,letteredlabels,i.e.(a),(b),(c)etc.,shouldbepositioned(preferablyinthecorners)inawaythatdoesnotobscureotherpartsofthefigure,andthepositioningshouldbeconsistentamongallsubfig

28、ures.(9) Forcolorfigures,CMYKisrequiredfortheprintversionofthejournal.Authorsshouldclearlyindicatewhichfiguresareintendedtobepublishedincolorwhensubmitting.Forfiguresincolorbutnotintendedtobepublishedincolor,itisstronglyrecommendedthatyoureproducetheminblackandwhitetoensuregoodqualityprinting.3.1.2

29、FiguresFAQs(1) Whyismyfigurelabellingfuzzyorsaw-toothed?Figuresareconvertedinto.epsformatbeforebeingadaptedintoourtypesettingsystem.As.epsformatisvector-based,forfiguresinpixel-basedformats(e.g.jpg,.bmp,.psd,.gif),afterconversion,thequalitywillbegreatlydiminishedandmightappearfuzzy.(2) Whyisthereash

30、adowinmyfigure?InsertionoffiguresintowordorPPTmightcreateashadow.Tryprovidingusthefiguresinsourceformat.(3) Whyshouldlinethicknessesbeatleast0.2pt?Theprintresolutionislowerthanthefigureitself.ThelineswillappearbrokeninsteadOfcontinuousinthefinalprintedproductforlinethicknesseslowerthan0.2pt.(4) What

31、isCMYK?CMYK(cyan,magenta,yellow,black)figuresarewidelyusedforprinting.(5) Whydoallthefontsneedtobeembeddedorconvertedtopathsoroutlines?Itisrecommendedthatallfontsareembeddedwhenfirstcreated.Ifitisdifficulttoembedthefontsinthefigure-drawingsoftware,thealternativeistocreateoutlinesforthefontsused.Inso

32、mecases,ifthefontsarenotembeddedorcreatedwithoutlines,theywillbeconvertedtoatotallydifferentfontorbecomelostwhenconvertedtoanotherformat.3.2 TablesTablesshouldbenumbered,haveacaption(abovethetable),andmentionedspecificallyinthetext(Table1),captionsshouldbedouble-spaced.Tablesshouldbeembeddedinthebod

33、yofthemanuscriptascloseaspossibletoitscitationfollowingaparagraphorsectionbreak(WeunderstandthisplacementmaynotalwaysbepossibleforauthorsusingLaTeX).Table1.Thisisasampletablecaptionandtablelayout.Enterasmanytablesasnecessaryattheendofyourmanuscript.Trendintheatmosphericheatsource/sinkEanditscomponen

34、tsovertheCE-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.

35、1-8.4-8.40.1-4.21461471481491501511521531541551561571581591601611621631641651661671681691701711721731741751761771781791801811821831841851861871884.CitationsandreferencesFollowingtheguidelinesforcitationsandreferencescanexpeditethetimetakentoprocessyourmanuscript.4.1 InstructionsforcitationsCitations

36、tostandardreferencesinthetextshouldconsistofthenameoftheauthorandtheyearofpublication-forexample,Wang(1990)or(Wang,1990).Iftherearethreeormoreauthors,statethefirstauthor,ssurname,followedby,etal.andtheyearofpublication一forexample,Wangetal.(1990)or(Wangetal.,1990).Whentherearetwoormorepapersbythesame

37、authororauthorsinthesameyear,distinguishingletters(a,b,c,etc.)shouldbeaddedtotheyearinboththecitationinthetextandthereferencelisting-forexample,Wang(1990a).Formultiplecitationsbyoneauthor,separateyearsbycommas一forexample,Wang(1989,1990)or(Wang,1989,1990).Separatemultiplecitationsbydifferentauthorswi

38、thinthesameparenthesesbysemicolonsforexample,(Wang,1990;Li,1991)or(Wang,1989,1990;Li,1991).4.2 InstructionsforreferencesReferencesshouldbelistedalphabetically,withoutnumbering,attheendofthepaper.Referencesmustbecompleteandproperlyformatted,andonlyliteraturecitedinthetextshouldbelisted.(1) Journalpap

39、ers: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),publica

40、tionyear: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:Mechanismsofinterannualvariationsinasim

41、pleairseacoupledmodelinthetropics.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:194

42、8-1983,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.,and

43、Coauthors,2005:THORPEXInternationalResearchImplementationPlan.WMO/TD-No.1258,96pp.212213214215216217218219220221222223224225226227228229230231232233Acknowledgments.Keeptheacknowledgementssectionasbriefaspossiblebyacknowledgingonlydirectassistanceinyourresearchandwriting.Financialsupportfortheworksho

44、uldbeacknowledgedhereratherthanasfootnotestothetitle.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.,

45、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,

46、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.WM

47、O/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