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Estimating Station Specific Zenith Tropospheric Delay in a Local GPS Network from Observed Surface Meteorology

机译:观察到地表气象学局部GPS网络中估算站特异性Zenith对流层延迟

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The total zenith tropospheric delay (ZTD) is an important parameter of the atmosphere which directly or indirectly give reflection of the atmospheric condition in a local GPS network. The use of the global tropospheric models such as the Saastamoinen model, Hopfield model, Neil model etc in estimating the tropospheric effects at the local level leaves much to be desired. These models are derived using data from available radiosonde obtained from Europe and North America continents. The global atmospheric condition used as constants in these models provides a broad approximation of the tropospheric conditions, but ignores the actual atmospheric conditions on a given location i.e. do not take into account the latitudinal and seasonal variations in the atmosphere. It is necessary to assess the effects of the troposphere on geodetic measurements based on ground meteorological measurements including temperature, pressure, and relative humidity. Daily RINEX GPS data from eight (8) Malaysian Real Time Kinematic GPS Network (MyRTKnet) stations in Southern Malaysia from year 2006 to June 2008 thus; covering 2? years were processed. A computer program for modelling 2? years of local meteorology within the network was developed and called MetMOD, similarly a program, call SaastroMOD was developed to estimate the local zenith hydrostatic delay. The results showed that, the estimated local tropospheric delay considered the temporal and spatial variation of the network thus; giving true reflection of the tropospheric delay in a local GPS network as against the standard atmosphere which ignores the actual local condition with a standard deviation of 0.18 m having a maximum zenith tropospheric delay (ZTD) of about 2.6 m. The best zenith hydrostatic delay (ZHD) comes from station JHJY with a standard deviation of 0.353 cm, while the best zenith wet delay (ZWD) comes from station TGRH with a standard deviation of 5.943 cm. The models show that, while parameters evolved for ZHD are constant at different locations, however, those parameters evolved for ZWD show significant variations from one location to the other. Hence then use of the local meteorological parameter in modelling tropospheric delay improves GPS positional accuracy.
机译:总Zenith对流层延迟(ZTD)是大气的重要参数,直接或间接地反映了本地GPS网络中的大气状况。使用全球对流层模型,如萨斯马努恩模型,Hopfield模型,尼尔模型等,估计局部水平的对流层效果很大。这些模型使用来自欧洲和北美洲的可用无线电电池的数据来源。作为这些模型中的常数使用的全局大气条件提供了对流层条件的广泛近似,但忽略了给定位置的实际大气条件即,请勿考虑到大气中的纬度和季节性变化。有必要根据基于包括温度,压力和相对湿度的地面气象测量来评估对流层对大地测量的影响。从2006年到2008年6月到2008年6月,每日八(8)马来西亚实时运动GPS网络(MYRTKNET)站的每日Rinex GPS数据为2006年6月至2008年6月;覆盖2?多年来被处理。用于建模2的计算机程序?网络内的多年的当地气象是开发并称为Metmod,同样是一个程序,呼叫SaStromod是开发的,以估计当地的Zenith静水延迟。结果表明,估计的局部对流层延迟被认为是网络的时间和空间变化;对本地GPS网络中的对流层延迟的真正反映为与标准气氛忽略了实际局部条件的标准偏差,标准偏差为0.18米,具有约2.6米的最大Zenith对流层延迟(ZTD)。最佳的静静压延迟(Zhd)来自车站JHJY,标准偏差为0.353厘米,而最佳的Zenith湿延迟(ZWD)来自站TGRH,标准偏差为5.943厘米。该模型表明,在不同位置处于ZHD演进的参数时,对于ZWD而演化的那些参数显示出与另一个位置的显着变化。因此,随着局部气象参数在模拟对流层延迟的模拟中提高了GPS位置精度。

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