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A GPS water vapour tomography method based on a genetic algorithm

机译:基于遗传算法的GPS水蒸汽断层扫描方法

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摘要

Water vapour is an important substituent of the atmosphere but its spatial and temporal distribution is difficult to detect. Global Positioning System (GPS) water vapour tomography, which can sense three-dimensional water vapour distribution, has been developed as a research area in the field of GPS meteorology. In this paper, a new water vapour tomography method based on a genetic algorithm (GA) is proposed to overcome the ill-conditioned problem. The proposed approach does not need to perform matrix inversion, and it does not rely on excessive constraints, a priori information or external data. Experiments in Hong Kong under rainy and rainless conditions using this approach show that there is a serious ill-conditioned problem in the tomographic matrix by grayscale and condition numbers. Numerical results show that the average root mean square error (RMSE) and mean absolute error (MAE) for internal and external accuracy are 1.52∕0.94 and 10.07∕8.44mm, respectively, with the GAMIT-estimated slant water vapour (SWV) as a reference. Comparative results of water vapour density (WVD) derived from radiosonde data reveal that the tomographic results based on GA with a total RMSE∕MAE of 1.43∕1.19mm are in good agreement with that of radiosonde measurements. In comparison to the traditional least squares method, the GA can achieve a reliable tomographic result with high accuracy without the restrictions mentioned above. Furthermore, the tomographic results in a rainless scenario are better than those of a rainy scenario, and the reasons are discussed in detail in this paper.
机译:水蒸气是大气的重要取代基,但其空间和时间分布难以检测。全球定位系统(GPS)水蒸汽断层扫描,可以感知三维水蒸气分布,已成为GPS气象学领域的研究区域。本文提出了一种基于遗传算法(GA)的新的水蒸汽断层扫描方法来克服不良问题。所提出的方法不需要执行矩阵反转,并且它不依赖于过度约束,先验信息或外部数据。利用这种方法的多雨和无雨条件下的香港实验表明,通过灰度和条件数字在断层矩阵中存在严重的病理问题。数值结果表明,内部和外部精度的平均均方根误差(RMSE)和平均绝对误差(MAE)分别为1.52 / 0.94和10.07 / 8.44mm,配有游戏估计的倾斜水蒸气(SWV)作为a参考。源自无线电探测数据的水蒸气密度(WVD)的比较结果表明,基于GA的基于GA的分断层结果为1.43 / 1.19mm的总RMSE / MAE与无线电探测器测量非常一致。与传统的最小二乘法相比,GA可以高精度地实现可靠的断层结果,而不高度上述限制。此外,在无雨场景中的断层摄影结果比多雨场景更好,并在本文中详细讨论了原因。

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