Reprocessed height time series for GPS stations

Precise weekly positions of 403 Global Positioning System (GPS) stations located worldwide are obtained by reprocessing GPS data of these stations for the time span from 4 January 1998 until 29 December 2007. The processing algorithms and models used as well as the solution and results obtained are...

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Main Authors: S. Rudenko, N. Schön, M. Uhlemann, G. Gendt
Format: Article
Language:English
Published: Copernicus Publications 2013-01-01
Series:Solid Earth
Online Access:http://www.solid-earth.net/4/23/2013/se-4-23-2013.pdf
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spelling doaj-b78a30d984e14ddda174461269d4cf012020-11-25T01:15:06ZengCopernicus PublicationsSolid Earth1869-95101869-95292013-01-0141234110.5194/se-4-23-2013Reprocessed height time series for GPS stationsS. RudenkoN. SchönM. UhlemannG. GendtPrecise weekly positions of 403 Global Positioning System (GPS) stations located worldwide are obtained by reprocessing GPS data of these stations for the time span from 4 January 1998 until 29 December 2007. The processing algorithms and models used as well as the solution and results obtained are presented. Vertical velocities of 266 GPS stations having a tracking history longer than 2.5 yr are computed; 107 of them are GPS stations located at tide gauges (TIGA observing stations). The vertical velocities calculated in this study are compared with the estimates from the co-located tide gauges and other GPS solutions. The formal errors of the estimated vertical velocities are 0.01–0.80 mm yr<sup>−1</sup>. The vertical velocities of our solution agree within 1 mm yr<sup>−1</sup> with those of the recent solutions (ULR5 and ULR3) of the Université de La Rochelle for about 67–75 per cent of the common stations. Examples of typical behaviour of station height changes are given and interpreted. The derived height time series and vertical motions of continuous GPS at tide gauges stations can be used for correcting the vertical land motion in tide gauge records of sea level changes.http://www.solid-earth.net/4/23/2013/se-4-23-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. Rudenko
N. Schön
M. Uhlemann
G. Gendt
spellingShingle S. Rudenko
N. Schön
M. Uhlemann
G. Gendt
Reprocessed height time series for GPS stations
Solid Earth
author_facet S. Rudenko
N. Schön
M. Uhlemann
G. Gendt
author_sort S. Rudenko
title Reprocessed height time series for GPS stations
title_short Reprocessed height time series for GPS stations
title_full Reprocessed height time series for GPS stations
title_fullStr Reprocessed height time series for GPS stations
title_full_unstemmed Reprocessed height time series for GPS stations
title_sort reprocessed height time series for gps stations
publisher Copernicus Publications
series Solid Earth
issn 1869-9510
1869-9529
publishDate 2013-01-01
description Precise weekly positions of 403 Global Positioning System (GPS) stations located worldwide are obtained by reprocessing GPS data of these stations for the time span from 4 January 1998 until 29 December 2007. The processing algorithms and models used as well as the solution and results obtained are presented. Vertical velocities of 266 GPS stations having a tracking history longer than 2.5 yr are computed; 107 of them are GPS stations located at tide gauges (TIGA observing stations). The vertical velocities calculated in this study are compared with the estimates from the co-located tide gauges and other GPS solutions. The formal errors of the estimated vertical velocities are 0.01–0.80 mm yr<sup>−1</sup>. The vertical velocities of our solution agree within 1 mm yr<sup>−1</sup> with those of the recent solutions (ULR5 and ULR3) of the Université de La Rochelle for about 67–75 per cent of the common stations. Examples of typical behaviour of station height changes are given and interpreted. The derived height time series and vertical motions of continuous GPS at tide gauges stations can be used for correcting the vertical land motion in tide gauge records of sea level changes.
url http://www.solid-earth.net/4/23/2013/se-4-23-2013.pdf
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