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Mean surface geostrophic circulation of the Mediterranean Sea estimated from GOCE geoid models and altimetric mean sea surface: initial validation and accuracy assessment

机译:通过GOCE大地水准面模型和高空平均海面估算的地中海平均地表营养环流:初步验证和准确性评估

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摘要

Different combinations of the EGM2008 global model and the GOCE spacewise solution are used to estimate the geodetic mean dynamic topography and the corresponding surface geostrophic circulation of the Mediterranean Sea. In order to assess the accuracy of the GOCE-derived products for oceanographic applications, the mean currents obtained from the geoid models are compared with the mean surface geostrophic velocities measured by drifters and satellite altimetry data. The mean dynamic topographies based on GOCE data combined with EGM2008 generally describe the main circulation patterns and dynamical features in the Mediterranean Sea, except in few coastal regions and in the semi-enclosed Adriatic and Aegean Seas, and improve the results obtained with previous geoid models. The root mean square differences between the geostrophic velocities and the GOCE/EGM2008-derived currents are smaller than 10 cm/s in all the sectors of the Mediterranean basin, whereas they are larger than 12 - 15 cm/s using the EGM2008 solution. The minimum discrepancies and the best complex correlation coefficient are achieved from the EGMSPWbc solution based on an order-wise block diagonal approximation of the GOCE error covariance structure.
机译:EGM2008全局模型和GOCE空间解的不同组合用于估计大地平均动态地形和相应的地中海表层地转环流。为了评估GOCE衍生产品在海洋学中的准确性,将从大地水准面模型获得的平均电流与通过漂移器和卫星测高仪数据测得的平均表面地转速度进行了比较。基于GOCE数据和EGM2008的平均动态地形一般描述了地中海的主要环流模式和动力学特征,除了少数沿海地区以及半封闭的亚得里亚海和爱琴海,并改进了以前的大地水准面模型获得的结果。在地中海盆地的所有地区,地转速度和GOCE / EGM2008衍生的洋流之间的均方根差小于10 cm / s,而使用EGM2008解决方案则大于12-15 cm / s。基于GOCE误差协方差结构的顺序块对角线近似,从EGMSPWbc解获得了最小差异和最佳复相关系数。

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