The INTIFANTE'00 sea trial: preliminary source localization and ocean tomography data analysis

S. Jesus, E. Coelho, J. Onofre, P. Picco, C. Soares, C. Lopes
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引用次数: 10

Abstract

The INTIFANTE'00 sea trial was a multidisciplinary experiment including testing of an autonomous surface vehicle, underwater communications, source localization and acoustic ocean tomography. The results shown concentrate on the source localization and ocean tomography data sets. The data gathered during a 24 hour run along a range independent track shows strong oceanographic features, possibly due to internal tide signature, both on the temperature data, as measured on the thermistor chain collocated with a vertical line array (VLA), and on the acoustic data. A range dependent track between 120 and 60 m water depth, shows a highly variable channel impulse response along time and range when the source was moving outwards from the VLA. In another acoustic track, the source was navigatated across a underwater canyon where the energy was rapidly distributed over a deep acoustic channel with sound trapped well below the thermocline. Good agreement between the modeled and measured channel responses represents the first step towards matched-fleld processing-like methods such as source localization and tracking and ocean tomography.
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INTIFANTE'00海上试验:初步震源定位和海洋断层成像数据分析
INTIFANTE’00海上试验是一项多学科实验,包括自主水面航行器、水下通信、声源定位和声学海洋断层扫描测试。结果集中在震源定位和海洋层析成像数据集上。在24小时内沿着距离独立轨道收集的数据显示出强烈的海洋学特征,可能是由于内部潮汐特征,无论是在温度数据上,还是在声学数据上,都是由与垂直线阵列(VLA)配置的热敏电阻链测量的。当震源从VLA向外移动时,在水深120至60 m之间的距离相关轨迹显示出高度可变的通道脉冲响应随时间和距离的变化。在另一个声学轨迹中,源被导航穿过一个水下峡谷,在那里能量迅速分布在一个深声通道上,声音被困在温跃层下面。模拟和测量的通道响应之间的良好一致性代表了向类似匹配场处理方法(如源定位和跟踪以及海洋层析成像)迈出的第一步。
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