首页> 外文会议>Symposium on 20 Years of Progress in Radar Altimetry >PROBABILITY DENSITY FUNCTIONS AND HIGHER ORDER STATISTICS OF LARGE-SCALE GEOSTROPHIC VELOCITY ESTIMATES AND SEA SURFACE HEIGHT, AS SEEN FROM THE JASON-1 – TOPEX/POSEIDON TANDEM MISSION
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PROBABILITY DENSITY FUNCTIONS AND HIGHER ORDER STATISTICS OF LARGE-SCALE GEOSTROPHIC VELOCITY ESTIMATES AND SEA SURFACE HEIGHT, AS SEEN FROM THE JASON-1 – TOPEX/POSEIDON TANDEM MISSION

机译:大规模的地磁速度估计和海面高度的概率密度函数和高阶统计,如杰森-1 - Topex / Poseidon串联特派团所见

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Geostrophic velocity Probability Density Functions (PDF), Skewness (S) and Kurtosis (K) are shown for both velocity components (u, v) estimated from the 3- year long Jason-1 - TOPEX/Poseidon (JTP) Tandem Mission which allowed infer both velocity components directly from the altimeter observations. To be comparable to previous results of velocity- (w) and SSH-PDF, we include the 18.5-year time series of SSH from the TOPEX/Poseidon, Jason-1 and Jason-2 (TPJJ) missions. The differences in the PDF of both velocity components are found to be evident, with a wider shape for the zonal velocity component due to the larger variability in zonal direction. Results confirm that the exponential shape of the global velocity PDF is a consequence of the spatially inhomogeneous EKE distribution over the global ocean. Only regions with a small variance in EKE, have Gaussian shaped PDF, however, normalizing each time series with their STD results in Gaussian PDF everywhere.
机译:从允许的3年杰森-1 - Topex / Poseidon(JTP)允许的速度组件(U,V)估计,所示的速度分量(U,V)显示出地嗜速速度概率密度函数(PDF),偏斜(v)直接从高度计观察中推断出速度分量。要与先前的Velocity-(W)和SSH-PDF的结果相当,我们包括来自Topex / Poseidon,Jason-1和Jason-2(TPJJ)任务的18.5岁的SSH。发现两个速度分量的PDF的差异是显而易见的,由于纬向方向的变异性较大,具有更宽的形状。结果证实全局速度PDF的指数形状是全球海洋的空间不均匀的EKE分布的结果。然而,只有在EKE中具有小的区域,并且具有高斯形的PDF,但是,每次序列都将其STD序列归一成,结果在Gaussian PDF到处都是。

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