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Single-difference Ionosphere Map Generation Based on a Reference CORS Network

机译:基于参考CORS网络的单差电离层地图生成

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This paper demonstrates a new approach to single-difference (SD) ionospheric delay estimation, based on Global Positioning System (GPS) observations from the State of Ohio Continuously Operating Reference Station (CORS) network. Once SD ionospheric delays are obtained, interpolation methods, such as Kriging, multi-quadric biharmonic functions or linear functions, etc., can be applied to provide ionospheric correction maps to users located within or in the vicinity of the regional network. Ionospheric maps can be generated, in general, in various modes, such as undifferenced, SD or double-difference (DD), mode. However, the undifferenced mode is subject to possible biases due to incorrect ambiguities resulting from the carrier-phase pseudorange smoothing process commonly used in this procedure. The process of interpolation on each level of ionosphere representation (i.e., differencing) has pros and cons due to inherent errors in GPS observations and geometric configuration between the reference network and the user, as well as spatial and temporal variation of the ionospheric features. In this paper, a fast and accurate SD approach is proposed to estimate the SD ionospheric delays that are easy to interpolate and handle by the user. In the SD approach, interchannel bias between C1 (or P1) and P2 pseudorange observables and ambiguities in phase observables are major error sources which affect the quality of the estimated SD ionospheric delay. The use of SD geometric range information is introduced here to remove the SD interchannel bias in pseudorange observables, and a bias removal technique, similar to pseudorange smoothing, is applied to remove the ambiguities in SD phase observables. As a result, SD bias-free ionospheric delay estimates are obtained from the regional GPS network. The, results are compared with the reference "truth," i.e., the DD ionospheric delays obtained from the external source with a few millimeter accuracy (Kashani et al., 2004b). The accuracy of the DD ionospheric corrections derived from the SD model is better than 15 cm in most cases.
机译:本文展示了一种新的单差(SD)电离层延迟估计的新方法,基于来自俄亥俄州的状态的全球定位系统(GPS)观察,从俄亥俄州连续操作参考站(CORS)网络)。一旦获得了SD电离层延迟,就可以应用插值方法,例如克里格,多反流性函数或线性函数等,以向位于区域网络内或附近的用户提供电离层校正图。通常,在各种模式中可以产生电离层图,例如未分化的,SD或双差(DD),模式。然而,未经定义的模式由于该过程中常用的载体相位伪常规平滑过程而导致的不正确的模糊,因此可能偏置。由于GPS观测和用户之间的GPS观测和几何配置中的固有误差以及电离层特征的空间和时间变型,因此对每个电离层表示的插值(即差异)的过程具有优点和缺点。在本文中,提出了一种快速准确的SD方法来估计用户易于插入和处理的SD电离层延迟。在SD方法中,C1(或P1)和P2伪距离观察和相位可观察的歧义之间的间隔偏压是影响估计的SD电离层延迟的质量的主要误差源。这里介绍了SD几何范围信息的使用,以删除伪奇园中的SD InterChannel偏置,并且施加类似于伪距平滑的偏置去除技术,以去除SD相位可观察到中的歧义。结果,从区域GPS网络获得了SD偏置电离层延迟估计。将结果与参考“真理”进行比较,即从外部源获得的DD电离层延迟,具有几毫米的精度(Kashani等,2004b)。在大多数情况下,从SD模型衍生的DD电离层校正的准确性优于15厘米。

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