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Towards a Semi-Kinematic Datum for Egypt

机译:走向埃及的半运动基准

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Since 1990, positioning technology has undergone a dramatic improvement in terms of accuracy and accessibility. Prior to 1990, national geodetic datums were considered to be static with fixed coordinates assigned to the datum origin by convention. Datum coordinates were dynamic only as a consequence of re-observation and re-adjustment, or localized disturbance. This strategy has been suitable for terrestrial surveys within stable continental areas. The accessibility of Precise Point Positioning “PPP” is now widespread with the provision of free online processing facilities by various geodetic agencies. Such ready accessibility to a global datum has serious implication for this technology with static geocentric datums. The Geocentric Datum of Egypt (ITRF1994 Epoch 1996 based on GPS Observation Campaign 1996), for example, is now offset by -42.0 to +32.0cm from the ITRF2008 Epoch 2015 due to the inexorable tectonic movements of the Nubian plate since the datum realization in 1996. Unless the local geocentric datums are kept in step with global terrestrial reference frames, discrepancies between the two will increase in magnitude over time and will become discernable, even using PPP. The PPP users nowadays are unaware of this datum offset and incorrectly assume that a coordinated datum monument is in error if there is found to be a disagreement greater than the level of accuracy of the positioning technique. In this study, to avoid the discrepancies between the applied datum and On-Line GNSS Services, a semi-kinematic datum and related deformation mode are proposed for Egypt. The result also confirmed that the PMM model was giving good performance for the other parts out of Egypt. The evaluation study shows the best performances for the Egyptian deformation model over the ITRF2008 PMM.
机译:自1990年以来,定位技术在准确性和可及性方面已经历了巨大的进步。在1990年之前,国家大地基准被认为是静态的,并且按照惯例将固定坐标指定给基准原点。基准坐标仅在重新观测和重新调整或局部干扰后才是动态的。该策略适用于稳定大陆地区的地面勘测。随着各种大地测量机构提供免费的在线处理工具,精确点定位“ PPP”的可访问性现已广泛普及。对静态基准的这种技术的现成可访问性对该技术具有严重的意义。例如,埃及的地心基准面(基于GPS观测运动1996的ITRF1994纪元1996)现在从ITRF2008纪元2015偏移了-42.0至+ 32.0cm,这是由于自从实现了努比亚板块以来努比亚板块的不可阻挡的构造运动。 1996年。除非局部地心基准与全球地面参考系保持一致,否则即使使用PPP,两者之间的差异也会随着时间的推移而增加,并且变得可辨别。如今,PPP用户尚未意识到该基准偏移,并且如果发现差异大于定位技术的精度水平,则错误地认为协调基准标记是错误的。在这项研究中,为避免应用的基准与在线GNSS服务之间的差异,针对埃及提出了半运动基准和相关的变形模式。结果还证实,PMM模型为埃及以外的其他地区提供了良好的性能。评估研究显示,在ITRF2008 PMM上,埃及变形模型的最佳性能。

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