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Zenith Tropospheric Delay Modeling Method for Sparse Reference Station Network Considering Height Difference

机译:考虑高度差异的稀疏参考站网络的Zenith对流层延迟建模方法

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A new method of zenith tropospheric delay modeling (HTIM) for sparse reference station network is put forward in this paper. The zenith tropospheric hydrostatic delay (ZHD) is calculated by the UNB3m model. In addition, the zenith tropospheric wet delay (ZWD) with high precision is estimated by conventional precise point positioning (PPP) using ionosphere-free combination. Considering the relationship between height factor and zenith tropospheric delay (ZTD) in UNB3m model, the zenith tropospheric delay is divided into two parts, the height weakly correlated and the height strongly correlated. The new method of zenith tropospheric delay modeling is established using the two parts of the zenith tropospheric delay. Based on the results of regional modeling, the zenith tropospheric delay of rover station is augmented. The new method is compared with conventional modeling methods. The results show that the new zenith tropospheric delay modeling method is superior to other methods in the undulated region only using four reference stations, RMS is 0.020 m and the absolute deviation is nearly within 0.03 m. It also shows that the RMS is 0.008 m and the rate of absolute deviation within 0.01 m reaches 75.95 % in the sparse reference station network. In the new method, the interpolation precision is not limited by the number of reference stations and three reference stations also can be used to get the interpolation results with high reliability. The results show that the new zenith tropospheric delay modeling method is superior to conventional methods, especially for the undulated region in a sparse reference station network.
机译:本文提出了一种新的Zenith对流层延迟建模(HTIM)的新方法。 Zenith对流层水压延迟(Zhd)由UNB3M型号计算。此外,通过无常规的精确点定位(PPP)估计具有高精度的Zenith对流层湿延迟(ZWD)使用离子层的组合来估计。考虑到UNB3M模型中高度因子和Zenith对流层延迟(ZTD)之间的关系,Zenith对流层延迟分为两部分,高度弱相关,高度强烈相关。利用Zenith对流层延迟的两部分建立了Zenith对流层延迟建模的新方法。基于区域造型的结果,罗孚站的Zenith对流层延迟增强。将新方法与传统的建模方法进行比较。结果表明,新的Zenith对流层延迟建模方法仅使用四个参考站的起伏区域中的其他方法,RMS为0.020 m,绝对偏差几乎在0.03米范围内。它还表明,RMS为0.008米,0.01米内的绝对偏差速率在稀疏参考站网络中达到75.95%。在新方法中,插值精度不受参考站的数量的限制,并且还可以使用三个参考站来获得高可靠性的插值结果。结果表明,新的Zenith对流层延迟建模方法优于传统方法,特别是对于稀疏参考站网络中的波状区域。

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