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Study on construction of local marine geomagnetic field model based on curve-surface interpolation

机译:基于曲线曲面插值的地方海洋地磁场模型建设研究

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There are many methods in building local geomagnetic field, such as polynomial method, interpolation method, Spherical Cap Harmonic Analysis and Rectangular Harmonic Analysis. Curve Surface Spine Function and Multi-surface Function are two interpolation methods. The model based on interpolation passes each node compared with fitting method. It can be proved that the interpolation method can get more accurate result compared with polynomial fitting method in building the local marine geomagnetic field model. The issue which should be researched in multi-surface function are quality control of geomagnetic data, kernel function choice, choice of the smoothing factor, model node selecting and zoning modeling method. The quality control of geomagnetic data is very important in building local marine geomagnetic field, here we introduce a kind of trend-surface methods for the quality control. The method establishes a function relative to location and uses 2sigma/3sigma principle to remove the gross error of geomagnetic data. It is proved to be very efficient in the filtering. The kernel function normally used are hyperboloid function and inverted hyperboloid function. Which one adopted in building the model needs to be verified in actual application. By experiment, we found that the accuracy of the model is higher using hyperboloid function than using inverted hyperboloid function. Smoothing factor is another important parameters in building local geomagnetic field model. Smoothing factor can improve the curvature of the model surface. Optimum smoothing factor is also required to be verified and determined in actual applications. We can find that the model's accuracy improving with the smoothing factor change from 0 to 100. We can also find there is an inflexion in the change of model accuracy. The hyperboloid function model's accuracy changes little with smoothness factor, but for the inverted hyperboloid function, corresponding model accuracy is very sensitive to smoot- hness factor. The model's accuracy is improved with the increase of node number. But the computational complexity will be increased with the node number increasing, and at the same time will lead to the unstable solution in building geomagnetic field model. Thus the node number should be appropriate in building the model. Generally, we only need small number of geomagnetic data in building the local geomagnetic field model with uniform change. However, a large number of geomagnetic data is required when geomagnetic change is more complicated. Character node is very important in building precise local geomagnetic field model. Character node represents its' surrounding geomagnetic field change. By experiment, we found that the accuracy of model constructed with selected the character node was better than that built with random geomagnetic data, especially in which geomagnetic field changes sharply. Zoning modeling method can avoid the problem, which too large nodes number lead to computational complexity in large area. The model's accuracy can be improved distinctly if we use enough and high-quality geomagnetic data. Because the model surface passes each node in building the model using Multi-surface Function, thus it can guarantee the smoothness and continuity in the common area of two adjoin modeling zones. Geomagnetic data of a marine area with 11-kilometer length and 1-kilometer width is used for the study of building local marine geomagnetic field model. In the study, we adopt above research methods and achieve the model accuracy with 8.09 nT of root mean square (RMS) in whole area. We also implement a zoning modeling experiment. In the experiment, we divide the whole area into 5 subsections, build models in these subsections, and achieve the model's accuracy with 5.29 nT in the whole area. Comparing above statistic parameters, we can find that the zoning modeling method is a kind of ideal methods in building high-accuracy local marine geomagnetic field model
机译:建立局部地质磁场等有许多方法,如多项式方法,插值法,球形帽谐波分析和矩形谐波分析。曲线表面脊柱功能和多表面功能是两个插值方法。基于插值的模型通过每个节点与拟合方法相比。可以证明,与构建本地海洋地磁场模型的多项式拟合方法相比,内插方法可以获得更准确的结果。应在多表面功能中进行研究的问题是地磁数据的质量控制,内核功能选择,选择平滑因子,模型节点选择和分区建模方法。地磁数据的质量控制在建立当地海洋地磁场中非常重要,在这里我们介绍了一种用于质量控制的趋势表面方法。该方法建立相对于位置的功能,并使用2sigma / 3sigma原理来消除地磁数据的总误差。被证明在过滤中非常有效。正常使用的内核功能是双曲面函数和反相双曲面函数。在建立模型中采用的是在实际应用中进行验证。通过实验,我们发现使用双曲面功能的模型的准确性比使用反相双曲面函数更高。平滑因子是建立局部地磁场模型的另一个重要参数。平滑因子可以改善模型表面的曲率。还需要在实际应用中验证和确定最佳平滑系数。我们可以发现模型的准确性改善了平滑因子从0到100的变化。我们还可以发现模型精度的变化有一个indlexion。双曲面函数模型的精度随着光滑的因子而变化几乎没有变化,但对于倒双曲线功能,相应的模型精度对Smoot HOOT系数非常敏感。随着节点编号的增加,模型的准确性得到改善。但是使用节点数量增加将增加计算复杂性,同时将导致建立地磁场模型中的不稳定解决方案。因此,节点编号应该适合构建模型。通常,我们只需要少量的地磁数据来构建局部变化的局部地磁场模型。然而,当地磁变化更复杂时需要大量地磁数据。字符节点在构建精确的当地地磁场模型方面非常重要。字符节点代表其“周围的地磁场变化”。通过实验,我们发现,使用选定的字符节点构造的模型的准确性优于随机地理数据构建的模型,特别是其中地质磁场急剧变化。分区建模方法可以避免问题,太大的节点数导致大面积计算复杂性。如果我们使用足够的高质量的地磁数据,可以清楚地改善模型的准确性。由于模型表面通过多表面功能将每个节点传递在构建模型时,因此它可以保证两个毗邻建模区域的公共区域中的平滑度和连续性。带11公里长度和1公里宽度的海域的地磁数据用于建设当地海上地质磁场模型的研究。在该研究中,我们采用了上述研究方法,并在整个区域中实现了8.09 nt的均方根(RMS)的模型精度。我们还实施了一个分区建模实验。在实验中,我们将整个区域划分为5个小节,在这些小节中构建模型,并在整个区域5.29 NT实现模型的准确性。比较上述统计参数,我们可以发现分区建模方法是建立高精度本地海洋地磁场模型的一种理想方法

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