简介：在南方印度洋的年度subduction率被分析数据吸收(苏打)在19502008的时期输出的简单海洋计算。为潜在的密度班的subduction率普查在南方印度洋副热带的旋回的西南的部分显示出相应于印度洋副热带的模式水(IOSTMW)的一座山峰。混合层深度越深，在现在的气候学的混合层前面和联系相对更快的发行量越sharper导致了更大的侧面的正式就职，它首先dominantsIOSTMWsubduction率，当时与从垂直的抽的仅仅次要的贡献。没有概论的损失，通过在最小的垂直温度坡度(LMVTG)的层的水特征的小心的分析，作者建议IOSTMW作为thermostad被识别，与低潜在的涡度的侧面的最小(PV，吗不到200湯漠?敌????猯'T￣牯嘠污猼扵?????汁?桴獥??晲捡楴獮栠摡猠杩楮楦慣瑮愠瑣癩瑩?湡?瑳'L汩瑩?景攠畭獬晩捩瑡潩?湵敤?慶楲畯???牦浯??琠?㈱??琠浥数慲畴敲爠湡敧?牦浯㈠‰潴ㄠ?讬鶝??顟????醰??????颮鑈？？

简介：Anoptimalactiveslidingmodecontrollerwithspecifieddecayratedesignisproposedtocontrolthewave-inducedoffshorejacket-typeplatformwithactivemassdamper(AMD).IrregularwaveloadingisapproximatedbyfinitesumsofFourierseries,anditsdynamiccharacteristicsaregovernedbyanexosystemderivedfromthelinearizedMorisonequation.Theoffshoreplatformsystemisfirstdecomposedintotwovirtualsubsystemsbasedonalineartransformation.ByconsideringthevelocityofAMDasavirtualcontrolforceforthefirstsubsystem,theoptimalvirtualcontrollerisderived.Furthermore,anoptimalslidingmodesurfacewithspecifieddecayrateisproposed.Then,theactiveslidingmodecontrollerisdesignedtoensurethatthestatetrajectoriesreachtheslidingsurfaceinfinitetimeandremainonitthereafter.Numericalsimulationisemployedtoverifytheeffectivenessoftheproposedapproach.

简介：Astructurefunctionapproachisappliedtoestimatetheturbulentkineticenergy(TKE)dissipationrateinthebottomboundarylayerofthePearlRiverEstuary(PRE).SimultaneousmeasurementswithanacousticDopplervelocimeter(ADV)suppliedindependentdatafortheverificationofthestructurefunctionmethod.Theresultsshowthat,1)thestructurefunctionapproachisreliableandsuccessfullyappliedmethodtoestimatetheTKEdissipationrate.Theobserveddissipationratesrangebetween8.3×104W/kgand4.9×106W/kginYM01andbetween3.4×104W/kgand4.8×107W/kginYM03,respectively,whileexhibitingastrongquarter-diurnalvariation.2)Thebalancebetweentheshearproductionandviscousdissipationisbetterachievedinthestraightriver.Thisfirst-orderbalanceissignificantlybrokenintheestuarybynon-shearproduction/dissipationduetowave-inducedfluctuations.

简介：StandardmetabolicratesofSchlegelsblackrockfishwithdifferentbodyweightsaredeterminedinlaboratorybyusingtheflow-throughrespirometerat11.2℃,14.7℃,18.0℃and23.6℃.Theresultsindicatethatthestandardmetabolicratesincreasewiththeincreaseofbodyweightatdifferenttemperatures.RelationshipbetweenthemcouldbedescribedasRs=aInWb.Themeanofstandardmetabolicrateissignificantlydifferentamonggroups,butthebvaluesarenot.Thestandardmetabolicratesofamendedstandardbodyweightsdecreasewiththeincreaseoftemperature,andthemeanofstandardmetabolicrateisalsosignificantlydifferentamonggroupswhenthestandardbodyweightsare48.6g,147.9g,and243.1g.RelationshipbetweenthemcouldbedescribedasRsw=me-bT.Therelationsofstandardmetabolicrate(Rs)orrelativemetabolicrate(Rs)tobodyweightandtemperatureyieldthefollowingequations:Rs=1.160W0.752e-9.494/7andRs1=1.160W0.254e-9.494/7.

简介：ThetimeseriesofannualandseasonalgrowthrateoftwocoralPorites,collectedatdifferentsitesoffringereefintheSanyaBay,HainanIslandhavebeenobtainedbyanalyzingX-radiographofskeletalband.Thereareobviousseasonalvariationsofthegrowthrateintwocorals,theaveragelowrateinwinterandtheaveragehighratefromspringtoautumn.Comparedwiththetimeseriesofenvironmentalvariables,thecoralgrowthrateisonlycorrelatedstatisticallywithseawatertemperatureandnotrelatedtorainfallandsunshine.Furthermore,thegrowthrateinspringandsummeriscorrelateddirectlywithseawatertemperatureofthewinter-earlyspring(betweenDecemberandMarch)andtheotherseasonalgrowthratehasnorelationshipwithseasonalvariationsofseawatertemperature.Weproposethatseawatertemperatureisoneofthefactorsaffectingthecoralgrowthrateintheareaandthelowseawatertemperatureisaprimarycontroloftheseasonalgrowthrate.