2016
DOI: 10.1515/jogs-2016-0001
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The NKG2008 GPS campaign – final transformation results and a new common Nordic reference frame

Abstract: Abstract:The NKG 2008 GPS campaign was carried out in September 28 -October 4, 2008. The purpose was to establish a common reference frame in the NordicBaltic-Arctic region, and to improve and update the transformations from the latest global ITRF reference frame to the national ETRS89 realizations of the Nordic/Baltic countries. Postglacial rebound in the Fennoscandian area causes intraplate deformations up to about 10 mm/yr to the Eurasian tectonic plate which need to be taken into account in order to reach … Show more

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Cited by 14 publications
(5 citation statements)
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“…These effects should be considered in high-accuracy positioning by appropriately transforming the coordinates taking them into account. The Nordic Geodetic Commission (NKG) has developed the NKG coordinate transformation methodology that considers both the rigid Eurasian plate motion and the intraplate deformations [ 42 ]. In this study, we have used the NKG2020 transformation, which is the latest version of this methodology at the time of this writing and enables an accuracy of a few millimeters [ 43 ].…”
Section: Methodsmentioning
confidence: 99%
“…These effects should be considered in high-accuracy positioning by appropriately transforming the coordinates taking them into account. The Nordic Geodetic Commission (NKG) has developed the NKG coordinate transformation methodology that considers both the rigid Eurasian plate motion and the intraplate deformations [ 42 ]. In this study, we have used the NKG2020 transformation, which is the latest version of this methodology at the time of this writing and enables an accuracy of a few millimeters [ 43 ].…”
Section: Methodsmentioning
confidence: 99%
“…In addition to the rigid plate motion, there is the Glacial Isostatic Adjustment (GIA), the most notable effect of which is the postglacial rebound in the Fennoscandian area. This causes intra-plate motion as shown in Figure 6, showing the NKG RF03vel model by the Nordic Geodetic Commission (NKG) (Häkli et al, 2016). It shows that annual vertical velocities in Finland vary between 1 and 9 mm and horizontal velocities are up to 2 mm.…”
Section: Deformation Of Reference Frames In Finlandmentioning
confidence: 96%
“…One way to improve the accuracy of transformations from ITRF to EUREF-FIN is to use GIA models and GNSS time series as described in Häkli et al, 2016.…”
Section: Deformation Of Reference Frames In Finlandmentioning
confidence: 99%
“…Results from four sample regions containing these locations are given in Table 3. locations i, non-tidal (e.g. [28], [27]) ellipsoidal heightsĥ i expressed in the ETRS89 realization EUREF89 [14] have been derived from GPS observations, yielding pointwise available estimates p i of height anomalies ζ i…”
Section: Least-squares Collocationmentioning
confidence: 99%