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1、外文原文及翻譯(一)外文原文TidalanalysisintheventureshapedareabetweenZhenhaiShenjiamenintheEastChinaSeaLuHuaqing,HUJianjiongMarineScienceSchoolofZhejiangOceanUniversityZhoushan316004,ChinaZhejiangInstituteofHydraulics&EstuaryHangzhou
2、310020ChinaAbstractIndertobetterunderstthegeneraltidalfeaturesintheventudshapedareabetweenZhenhaiShenjiameninthentherncoastalregionofZhejiangProvinceintheEastChinaSeathetidaldatawereobtainedfromthethreepermanenttidestati
3、onsofZhenhaiDinghaiShenjiamenfourtemparytidestationsofMamuChuanshanGuojuLiuhengalongwiththecurrentspeedbeingobservedatLuotouWaterway.Resultsfromharmonicanalysisshowthat:(1)Theareawasdominatedbyshallowwatertideswithirregu
4、larsemidiurnalfeaturesthesmallesttidalrangeoccurredintheareanearacrossinglinebetweenZhenhaiDinghaistationsindicatingthatatidainodeexistedinthesouthernHangzhouBay(2)Fmulae(whereHgareharmonicconstants)couldbeusedasjudgingc
5、riteriafhighIowtidalleveldiurnalinequalities(3)ThedurationdifferencebetweenebbfloodtidescouldberoughlyassessedbytheratioofHM4vsHM2thelargertheratioisthebiggerthedurationdifferenceisAtthesametimethedurationperiodcouldbeas
6、sessedby2gMgM4theepochdifferencebetweenM2M4tidalconstituents.If2gM2gM4180thentheebbdurationislongerthantheflooddurationif1802gM2gM4360theresultisreversed(4)TakingDinghaistationasacenterpointthehighesttidallevelstheaverag
7、ehightidallevelsaswellastheaveragetidalrangesatallstationsbecamehigherlargerbothsoutheastwardsnthwestwardswhilethelowesttidallevelstheaveragelowtidallevelsappearedtobelowerbothsoutheastwardsnthwestwards(5)Thetidalpattern
8、swerenotallinlinewiththetidalcurrentpatterns.AsaconclusionthesmallesttidalrangeoccurredinthenarrowpartofcurrentellipseofM2constituentintheEastChinaSea.Howeverallthesestudieswerefocusedontheopensearegionsthetidalfeaturesi
9、nthenearsheharbareasinthenthernZhejiangcoasthaveneverbeenaddressed.Therehasbeennostudytoinvestigatethetidalfeaturesinaventureshapedwaterarea.ThepredictionoftidalleveltidalcurrentinVshapedbaysestuariesistheeticallymature(
10、Zhaoeta1.1993)thepredictionisthattidallevelincreasesgraduallywiththetidalwavemovingtowardsabayanestuary.HoweverthevalidityofthistheeticalpredictionfsomespecialVshapedcoastalregionsneedstobeexamined.2MATERIALSMETHODSFtida
11、lcurrentdatacollectionusedinthisstudyfourcurrentmonitingstationswerearrangedaroundthecapeofChuanshanPeninsulawheresynchronouscurrentobservationswererecdedinmaxfloodmesominebbtides(Fig.2).Inadditionfourtemparytidestations
12、locatedatMamuChuanshanGuojuLiuhengthreepermanenttidestationslocatedatShenjiamenDinghaiZhenhaiwereedftidaldatacollection(Fig.2).AmongtheseobservingstationsthereisaLuotouWaterwaywhichislocatedbetweenthemainltheislstothesou
13、thofZhoushanIsl.TheeastsideofthewaterwayappearstobeinthelatitudinaldirectionconnectsouterwatersofthecontinentalshelfoftheECS.TothewestofDaxieIslthewaterwayappearstoflownthwestwardslinkstoJingtangWaterwayHengshuiyangSea.T
14、heentirewaterwaywaswithina100misobathsfromtheshe.2.1TideobservationstationarrangementAmongthefourtemparytidestations(MamuChuanshanGuojuLiuheng)thedatacollectionatChuanshanstationstartedfromzeroo’clockonJanuary62005to23:0
15、0pmonFebruary52005coveringa31dayperiodthedatacollectionfromtheotherthreestationsstartedfromzeroo’clockonJanuary132005to23:00pmonJanuary272005coveringa15dayperiod.Ateachtemparytidestationtidallevelswererecdedateveryhourwi
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