@article{nordman_using_2014,
	title = {Using the Nordic Geodetic Observing System for land uplift studies},
	volume = {5},
	issn = {1869-9510},
	url = {https://www.solid-earth.net/5/673/2014/},
	doi = {10.5194/se-5-673-2014},
	abstract = {{\textless}p{\textgreater}{\textless}strong{\textgreater}Abstract.{\textless}/strong{\textgreater} Geodetic observing systems have been planned and developed during the last decade. An ideal observing system consists of a network of geodetic observing stations with several techniques at the same site, publicly accessible databases, and as a product delivers data time series, combination of techniques or some other results obtained from the data sets. Globally, there is the International Association of Geodesy ({IAG}) Global Geodetic Observing System ({GGOS}), and there are ongoing attempts to create also regional observing systems. In this paper we introduce one regional system, the Nordic Geodetic Observing System ({NGOS}) hosted by the Nordic Geodetic Commission ({NKG}). {\textless}br{\textgreater}{\textless}br{\textgreater} Data availability and accessibility are one of the major issues today. We discuss in general data-related topics, and introduce a pilot database project of {NGOS}. As a demonstration of the use of such a database, we apply it for postglacial rebound studies in the Fennoscandian area. We compare land uplift values from three techniques, {GNSS}, tide gauges and absolute gravity, with the Nordic Geodetic Commission {NKG}2005LU land uplift model for Fennoscandia. The purpose is to evaluate the data obtained from different techniques and different sources and get the most reliable values for the uplift using publicly available data. {\textless}br{\textgreater}{\textless}br{\textgreater} The primary aim of observing systems will be to produce data and other products needed by multidisciplinary projects, such as Upper Mantle Dynamics and Quaternary Climate in Cratonic Areas ({DynaQlim}) or the European Plate Observing System ({EPOS}), but their needs may currently exceed the scope of an existing observing system. We discuss what requirements the projects pose to observing systems and their development. To make comparisons between different studies possible and reliable, the researcher should document what they have in detail, either in appendixes, supplementary material or some other available format.{\textless}/p{\textgreater}},
	pages = {673--681},
	number = {2},
	journaltitle = {Solid Earth},
	author = {Nordman, M. and Poutanen, M. and Kairus, A. and Virtanen, J.},
	urldate = {2020-01-27},
	date = {2014-07-17},
	note = {Number: 2}
}

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Globally, there is the International Association of Geodesy (IAG) Global Geodetic Observing System (GGOS), and there are ongoing attempts to create also regional observing systems. In this paper we introduce one regional system, the Nordic Geodetic Observing System (NGOS) hosted by the Nordic Geodetic Commission (NKG). \\textlessbr\\textgreater\\textlessbr\\textgreater Data availability and accessibility are one of the major issues today. We discuss in general data-related topics, and introduce a pilot database project of NGOS. As a demonstration of the use of such a database, we apply it for postglacial rebound studies in the Fennoscandian area. We compare land uplift values from three techniques, GNSS, tide gauges and absolute gravity, with the Nordic Geodetic Commission NKG2005LU land uplift model for Fennoscandia. The purpose is to evaluate the data obtained from different techniques and different sources and get the most reliable values for the uplift using publicly available data. \\textlessbr\\textgreater\\textlessbr\\textgreater The primary aim of observing systems will be to produce data and other products needed by multidisciplinary projects, such as Upper Mantle Dynamics and Quaternary Climate in Cratonic Areas (DynaQlim) or the European Plate Observing System (EPOS), but their needs may currently exceed the scope of an existing observing system. We discuss what requirements the projects pose to observing systems and their development. 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We compare land uplift values from three techniques, {GNSS}, tide gauges and absolute gravity, with the Nordic Geodetic Commission {NKG}2005LU land uplift model for Fennoscandia. The purpose is to evaluate the data obtained from different techniques and different sources and get the most reliable values for the uplift using publicly available data. {\\textless}br{\\textgreater}{\\textless}br{\\textgreater} The primary aim of observing systems will be to produce data and other products needed by multidisciplinary projects, such as Upper Mantle Dynamics and Quaternary Climate in Cratonic Areas ({DynaQlim}) or the European Plate Observing System ({EPOS}), but their needs may currently exceed the scope of an existing observing system. We discuss what requirements the projects pose to observing systems and their development. 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