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Orthometric correction and normal heights for Italian levelling network: a case study

机译:意大利水准网的正高校正和正常高度:一个案例研究

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Levelling increments must be corrected for gravity in order to get proper dynamic or orthometric heights. In Italy, most of the levelling lines have no associated gravity observations. Thus, only levelling increments are available, and corrections were computed only on a subset of the existing lines. However, gravity is densely observed, and thus, predictions of gravity along the levelling lines can be computed. This, in principle, would allow the estimation of corrections along the whole Italian levelling network. Furthermore, global model-derived gravity could be used for the same task (e.g. one could use the EGM2008 global geopotential model to get gravity estimates). To check for the reliability of these procedures, a test has been performed along levelling lines in the western Alps area. Both dynamic and orthometric corrections have been computed in order to finally get geopotential numbers, normal heights and orthometric heights from raw levelling increments. The results proved that reliable results can be obtained using the Italian gravity database, while predictions based on the EGM2008 model led to poorer estimates.
机译:必须针对重力校正水平增量,以获取适当的动态或正交高度。在意大利,大多数找平线都没有相关的重力观测值。因此,仅水平增量可用,并且仅在现有线的子集上计算校正。但是,密集地观察到重力,因此,可以计算出沿着找平线的重力预测。原则上,这将允许估计整个意大利水准测量网络的校正量。此外,可以将整体模型得出的引力用于同一任务(例如,可以使用EGM2008全局地势模型来获得引力估算值)。为了检查这些程序的可靠性,已经在阿尔卑斯山西部地区的水平线上进行了测试。为了从原始水准增量中最终获得地势数,法向高度和正高,已经对动态和正高校正进行了计算。结果证明,使用意大利重力数据库可以获得可靠的结果,而基于EGM2008模型的预测导致较差的估计。

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