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Geostatistical Inversion of Seismic Oceanography Data for Ocean Salinity and Temperature Models

机译:海洋盐度和温度模型地震海洋学数据地震局部逆变

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摘要

Conventional multi-channel seismic reflection data, known as seismic oceanography, has recently been used for the qualitative interpretation of meso- to large-scale hydrographic structures of interest. Seismic oceanography has been successfully imaging oceanographic structures in an intermediate scale not sampled by traditional oceanographic tools, such as conductivity, depth and temperature measurements and eXpendable BathyThermograph (XBT) data. However, few attempts have been made for successfully quantifying ocean properties, such as ocean temperature and salinity, directly from the seismic reflection data. This work presents an iterative geostatistical methodology capable of inverting conventional seismic oceanographic data simultaneously for high-resolution temperature and salinity ocean models. The proposed methodology was developed and implemented in a real set of contemporaneous XBT data and two-dimensional seismic profile acquired southwest of Portugal. The resulting high-resolution temperature and salinity models reproduce existing XBT data not used to constrain the geostatistical inversion, which permits reliable quantification of the ocean properties of interest.
机译:最近被称为地震海洋学的常规多通道地震反射数据,最近用于中学对大规模水文结构的定性解释。地震海洋学已经成功地成功地以传统海洋工具采样的中间规模成功地进行了海洋结构,例如电导率,深度和温度测量和消耗的浴室热震源(XBT)数据。然而,直接从地震反射数据成功地量化海洋性能,例如海洋温度和盐度,已经尝试了很少。这项工作提出了一种能够同时反转传统地震海洋学数据的迭代地稳态数据,用于高分辨率温度和盐度海洋模型。拟议的方法是在葡萄牙西南最真实的同时XBT数据和二维地震型材中制定和实施。由此产生的高分辨率温度和盐度模型再现现有的XBT数据,不用于限制地质统计反演,这允许可靠地量化感兴趣的海洋特性。

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