海洋通报
海洋通報
해양통보
MARINE SCIENCE BULLETIN
2009年
6期
19-25
,共7页
葛苏放%申双和%张新厂%潘玉萍
葛囌放%申雙和%張新廠%潘玉萍
갈소방%신쌍화%장신엄%반옥평
COARE算法%海面空气动力粗糙度%动量通量
COARE算法%海麵空氣動力粗糙度%動量通量
COARE산법%해면공기동력조조도%동량통량
COARE algorithm%aerodynamic roughness length%wind stress
利用福建沿海海域南日岛、金门岛与广东南澳岛的近海面气象、水文观测资料及台湾海峡西南部与南部的浮标观测资料,通过COARE(Coupled-Ocean Atmosphere Response Experiment) 算法(V3.0),计算了台湾海域近海面空气动力粗糙度、曳力系数及海气表面动量通量,并研究它们关于水平风速的分布规律.结果得出:摩擦速度与10 m风速基本上呈线性分布,线性拟合系数在0.042~0.045之间.曳力系数对10m风速的线性分布与过去研究结果相近,线性拟合系数在0.064~0.067之间.海面空气动力粗糙度对10 m风速的线性拟合系数在0.053~0.058之间.海面动量通量与10 m风速呈明显的二次关系,其线性与非线性拟合系数对于进一步了解台海地区大气湍流结构,建立和完善台海地区数值预报模式可提供重要的参数依据.
利用福建沿海海域南日島、金門島與廣東南澳島的近海麵氣象、水文觀測資料及檯灣海峽西南部與南部的浮標觀測資料,通過COARE(Coupled-Ocean Atmosphere Response Experiment) 算法(V3.0),計算瞭檯灣海域近海麵空氣動力粗糙度、抴力繫數及海氣錶麵動量通量,併研究它們關于水平風速的分佈規律.結果得齣:摩抆速度與10 m風速基本上呈線性分佈,線性擬閤繫數在0.042~0.045之間.抴力繫數對10m風速的線性分佈與過去研究結果相近,線性擬閤繫數在0.064~0.067之間.海麵空氣動力粗糙度對10 m風速的線性擬閤繫數在0.053~0.058之間.海麵動量通量與10 m風速呈明顯的二次關繫,其線性與非線性擬閤繫數對于進一步瞭解檯海地區大氣湍流結構,建立和完善檯海地區數值預報模式可提供重要的參數依據.
이용복건연해해역남일도、금문도여엄동남오도적근해면기상、수문관측자료급태만해협서남부여남부적부표관측자료,통과COARE(Coupled-Ocean Atmosphere Response Experiment) 산법(V3.0),계산료태만해역근해면공기동력조조도、예력계수급해기표면동량통량,병연구타문관우수평풍속적분포규률.결과득출:마찰속도여10 m풍속기본상정선성분포,선성의합계수재0.042~0.045지간.예력계수대10m풍속적선성분포여과거연구결과상근,선성의합계수재0.064~0.067지간.해면공기동력조조도대10 m풍속적선성의합계수재0.053~0.058지간.해면동량통량여10 m풍속정명현적이차관계,기선성여비선성의합계수대우진일보료해태해지구대기단류결구,건립화완선태해지구수치예보모식가제공중요적삼수의거.
The data collected at the Nanri,Jinmen and Nan'ao Islands of Fujian coastal area,and the buoy data used from the southwest and south of Taiwan Strait.By use of the COARE(Coupled-Ocean Atmosphere Response Experiment) algorithm(version 3.0),we calculated the frictional speed,drag coefficient,aerodynamic roughness length and wind stress,and studied their distributions with 10m wind speed above the sea surface.The frictional speed turned out to be linearly related to the 10 m wind speed.The linear fitness coefficient is between 0.042 and 0.045.Similarly,linear relationships between the drag coefficient,roughness length and 10m wind speed were found.The linear fitness coefficients are 0.064-0.067 and 0.053-0.058 respectively.Wind stress performed good quadratic change with wind speed.The linear fitness coefficients and nonlinear fitness coefficients might be valuable to be referenced to providing the basis for parameter value determination for further understanding sea-air interface energy transport,constructing and improving models of climate,wave and sea wind.