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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
