简介:ByimplementingtheARGOprogram,alargenumberofT-Sprofilescanbeobservedintheworldocean.However,itisverydifficulttoexaminechangesofthesensitivityofthesensorsequippedattheARGOfloats,becauseitisdifficulttounderstandtheirconditionintheseaandthereliabilityofthedata.Qualitycontrolmustbedoneinordertoavoidthewrongconclusiondeducedfromthewrongdata.OneoftherealisticmethodsforqualitycontroloftheARGOdataisthecomparisonwiththelocalclimatology.HighqualityclimatologicalT-SmodelsinnorthwestPacifichavebeenbuiltbasedontheNansenbottledataandCTDdataforthequalitycontrolinNMDIS.ThemodelsareusedtochecktheARGOdatainthisareaandhavegotgoodresult.
简介:通过对TOGA—COARE期间的一组锚系仪器阵列资料的分析得出:在赤道西太平洋1°45’S,156°E。海域存在显著的半日潮频内波,它的水平波数(波长)、垂向波数、水平传播速度和垂向传播速度分别约为:3.3×10^-2km^-1(210km),-1.6×10^-3m^-1,2.0m/s,-3.8cm/s。波形向斜下方传播,亦即波能向斜上方传输。它在观测点西南方生成后,向东北方向传播,到达观测海区。流速矢量旋转谱水平随深度的变化呈马鞍形,低谷及深处的峰所在深度分别与南赤道流及赤道潜流的南边界所在深度大体一致。旋转椭圆主轴方位角随深度变化,在浅层(40m处)为北偏东30°,到深处(324m)转为东偏南14°。总体上呈东北方向,表明波来自西南方向。