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• W73124025 abstract "Geodetic datum transformation by quaternion – Datum transformation has been widelyused in geodesy and a number of different algorithms have been known and applied. However,many of them are based on the assumption of small rotations, and linearization is needed in orderto derive the datum transformation parameters. In this paper, we have used the concept ofquaternions to represent the rotation, the translation and scale parameters in the Bursa-Wolfgeodetic transformation model. The main advantage of this algorithm is that it can be applied incase of arbitrary size rotation, we do not need linearization and iteration for the computation of thedatum transformation parameters for a non-linear transformation model. |                                                                    Geodetic datum transformation by quaternion – Datum transformation has been widelyused in geodesy and a number of different algorithms have been known and applied. However,many of them are based on the assumption of small rotations, and linearization is needed in orderto derive the datum transformation parameters. In this paper, we have used the concept ofquaternions to represent the rotation, the translation and scale parameters in the Bursa-Wolfgeodetic transformation model. The main advantage of this algorithm is that it can be applied incase of arbitrary size rotation, we do not need linearization and iteration for the computation of thedatum transformation parameters for a non-linear transformation model. | A datumtranszformacio a geodeziaban alkalmazott olyan szamitasi modszer, melynek szamos kulonbozőalgoritmuson alapulo valtozata ismert. A megoldasok tobbsege kis szogelfordulasokat feltetelezes linearizalas szukseges a transzformacios parameterek meghatarozasahoz. A dolgozatkvaternio alapu datum transzformacios analitikus megoldast ismertet. Bemutatja a kvaternio szamitasahozszukseges osszefuggeseket, a kvaterniok alkalmazasat forgatas, az eltolas es meretaranyparameterek meghatarozasat a Bursa-Wolf datum transzformacios modellben. Ennek az algoritmusnaka legnagyobb előnye, hogy tetszőleges nagysagu szogelfordulasok eseteben is alkalmazhato,nincs szukseg linearizalasra es iteraciora a transzformacios parameterek szamitasahoz.                                                                                                   " @default.
• W73124025 created "2016-06-24" @default.
• W73124025 creator A5022054812 @default.
• W73124025 creator A5032937998 @default.
• W73124025 creator A5056823462 @default.
• W73124025 creator A5061163541 @default.
• W73124025 creator A5071827404 @default.
• W73124025 date "2013-01-01" @default.
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