摘要
Onthebisisofdeterminingthethereelementsofthemocline(depth[upperbounddepth],thicknessandintensity)andthemaximumverticaltemperaturegradientofthesurveyingstation,thepapercalculatesthemeantemperatureoftheNanshadeep-watersurveyingstationwithintheupper-bounddepthlayerofthermoclineandthemeantemperaturebelowthelowerbounddepthofthermoclinebetweenthe300mand800mlayers,respectively.AnalysisindicatesthatthehorizontaldistributionofmeanseawatertemperatureshowsadistincttrendofthelowtemperatureseawaterslowlymovingfromtbenortheasttothesoutheastofNansha,whichseemstohavebeendrivenbytheNortheastMonsoon.Thelargertheverticaltemperatureradientis,thegreaterisitscapabilityofpreventingtheheatoftheupperseawaterfromdiffusingintothedeeperlayersontheverticaldirection.
出版日期
2001年02月12日(中国Betway体育网页登陆平台首次上网日期,不代表论文的发表时间)