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Volles Gewicht einer im Refraktionsmilieu gemessenen Grösse (Teil I)

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As regards the concept of complete weight p with which an observed quantity (e.g., the direction of theA–G net) should enter the net adjustment, according to Eq.(1), apart from the fundamental weight p0), determined by the number of repetitions, it should also contain the time parameter pt according to Eq.(11), where c>1 is a constant, and t is the number of days of observation, and also the refraction factor pr according to Eqs(17, 18), where q is the structural weight of the direction. The condition for being able to determine pr with the directions is observation by means of the three-directional vertex method[2], because it is not possible to localize lateral refraction by angular methods. The theory of complete weight is in favour of observations with a high fundamental weight p0 which automatically yield higher values of t, and also of pt. The introduction of the complete weight into the experimental directional net in Fig. 2 caused the mean value of the uneliminated refraction error to decrease from 0.24″ to 0.12″, the mean square error of the adjusted direction being 0.17″. The value of the constant c was investigated and the method of determining the parameter pr was derived also for lengths measured electro-optically. Mention is made of the effect of complete weights on the length adjustment of a net in[6].

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Kučera, K. Volles Gewicht einer im Refraktionsmilieu gemessenen Grösse (Teil I). Stud Geophys Geod 15, 132–140 (1971). https://doi.org/10.1007/BF01623910

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  • DOI: https://doi.org/10.1007/BF01623910

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