首页> 外文会议>International conference on port and ocean engineering under arctic conditions >DYNAMIC ESTIMATION OF DRIFTING ICE TOPOGRAPHY OVER A 2D AREA USING MOBILE UNDERWATER MEASUREMENTS
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DYNAMIC ESTIMATION OF DRIFTING ICE TOPOGRAPHY OVER A 2D AREA USING MOBILE UNDERWATER MEASUREMENTS

机译:使用移动水下测量对2D区域漂移冰地形探测的动态估计

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We present an estimation design for monitoring a drifting underwater ice topography, for realtime acquisition of high resolution ice thickness data in a local operations area. Additionally, the feature of detection and tracking of significant ice features such as ridges, growlers, bergy bits, and icebergs frozen into the sea ice comes for free from the setup. For continuous underwater monitoring of the drifting sea-ice we are challenged by two obstacles: 1) the ice topography is a dynamic landscape, and 2) we need to communicate the measurement data in real time through a limited hydroacoustic communication channel. Representing the topography by a truncated 2D Fourier series and a spatially discretized set of measurement nodes distributed over the surveillance area, a steepest descent method is proposed to make the underwater ice topography estimate converge to the real topography. Since only a small number of Fourier coefficients is needed to represent the topography sufficiently well, it becomes possible to transmit the estimated topography in real time through the hydroacoustic communication channel and to online reconstruct and present it in a surface-based operation center. Since the nodes in the observation grid will only be measured while the mobile sensor is in range, a nonlinear observer is proposed to filter the measurements and update them dynamically in dead-reckoning when measurements are not available. The effectiveness of the estimation algorithm is simulated based on an extensive and highly varying bottom topography, emulating in our case a typical ice topography.
机译:我们提出了一种用于监控漂移水下冰地形图的估计设计,用于实时获取本地操作区域中的高分辨率冰厚度数据。此外,检测和跟踪显着的冰功能的特征,例如脊,咆哮者,溃疡位和冰山中冻结在海冰中的冰山是免费的。对于漂移的海冰的连续水下监测我们受到两个障碍的挑战:1)冰地形是一种动态景观,而且2)我们需要通过有限的水声通信通道实时地将测量数据进行传达。提出了一种截头2D傅立叶串的地形和分布在监视区域上的空间离散化测量节点,提出了一种陡峭的脱刻法,以使水下冰地形估计到实际地形的趋同。由于仅需要少量的傅里叶系数来充分地表示形状,因此可以通过水声通信信道实时地将估计的地形和在线重建并将其呈现在基于表面的操作中心。由于观察电网中的节点仅在移动传感器在移动传感器的范围内测量,因此提出了非线性观察者来滤波测量并在测量不可用时动态地更新它们。估计算法的有效性基于广泛且高度变化的底部地形来模拟,在我们的情况下模拟典型的冰地形。

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