ECGN - Development of the European Combined Geodetic Network in Austria

Similar documents
Status. EUREF TWG Meeting November 8 9, 2004, Praha

GGOS, ECGN and NGOS: Global and regional geodetic observing systems. Markku Poutanen Finish Geodetic Institute

ABSOLUTE GRAVITY MEASUREMENTS

Establishment of a Global Absolute Gravity Network

Fundamental Station Wettzell - geodetic observatory -

Geodetic Observing Systems: tools in observing the Glacial Isostatic Adjustment. Markku Poutanen Finnish Geodetic Institute

Development of the Czech National Geodetic Control

EUREF 2007 Symposium. National Report of Austria

Gravity Monitoring with a Superconducting Gravimeter in Vienna

Borowa Gora (BG) IGETS Station Report

REGIONAL REFERENCE FRAMES: THE IAG PERSPECTIVE

To the best of our knowledge, the FG5 gravimeter represents the current state-of-the-art in the measurement of absolute gravity.

Densification of the GGOS infrastructure in Poland in the framework of EPOS-PL

NATIONAL REPORT OF POLAND TO EUREF 2011

GG S Global Geodetic Observing System (GGOS): Status and Future. Markus Rothacher, Ruth Neilan, Hans-Peter Plag

Measuring integral soil moisture variations using a geoelectrical resistivity meter

European Vertical Reference System (EVRS) 2007 a Combination of UELN and ECGN

GG S. Internal Vision of GGOS. Markus Rothacher. GFZ Potsdam

Mount Stromlo Gravity Station Gravimetry at the ANU

Geodetic applications of GNSS in the Black Sea region

GGSP: Realisation of the Galileo Terrestrial Reference Frame

Gravimetric Tide observation at Lake Nasser Region, Aswan, Egypt

geodynamics

Consideration of a Global Vertical Reference System (GVRS) in the IERS Conventions

Warkworth geodetic station as a potential GGOS core site in New Zealand

EUREF 05: National Report of Switzerland

Onsala Space Observatory IVS Network Station Activities during

GGOS Bureau for Standards and Conventions

Absolute gravimetry. Gabriel Strykowski Geodynamics Department DTU-Space (formerly Danish National Space Center)

Intermediary Report - August Prof. Dr. Olivier Francis and Prof. Dr. Tonie Van Dam

Comparison between measurements with the superconducting gravimeter T020 and the absolute gravimeter FG5-221 at Metsähovi, Finland in

Global Mapping Function (GMF): A new empirical mapping function based on numerical weather model data

geodynamics

The Global Mapping Function (GMF): A new empirical mapping function based on numerical weather model data

Torsten Mayer-Gürr Institute of Geodesy, NAWI Graz Technische Universität Graz

A Unique Reference Frame: Basis of the Global Geodetic Observing System (GGOS) for Geodynamics and Global Change

Using Signals Emitted by Global Navigation Satellite Systems

Reference Systems Realization for the Territory of Bulgaria - Status and Perspectives

INTERNATIONAL SLR SERVICE

New satellite mission for improving the Terrestrial Reference Frame: means and impacts

Use of ground-based GNSS measurements in data assimilation. Reima Eresmaa Finnish Meteorological Institute

GPS time series and sea level

Earth gravity field recovery using GPS, GLONASS, and SLR satellites

The Global Geodetic Observing System (GGOS) of the International Association of Geodesy, IAG

Publ. Astron. Obs. Belgrade No. 91 (2012), REALIZATION OF ETRF2000 AS A NEW TERRESTRIAL REFERENCE FRAME IN REPUBLIC OF SERBIA

GNSS-specific local effects at the Geodetic Observatory Wettzell

REFINED AND SITE-AUGMENTED TROPOSPHERIC DELAY MODELS FOR GNSS

ABSOLUTE GRAVITY MEASUREMENTS IN LOMONOSOV, SAINT-PETERSBURG, RUSSIA

On Integrated Geodetic Monitoring for Sinkhole-Induced Surface Deformation and Mass Dislocation

Co-location of VLBI with other techniques in space: a simulation study

The BIFROST Project: 21 years of search for the true crustal deformation in Fennoscandia

Realization of the vertical datum and height system of Lithuania

Search for the Gravitational Absorption Effect Using Spring and Super-conducting Gravimeters during the Total Solar Eclipse of August 11, 1999

SLR-based orbit determination and orbit prediction of space debris objects

Final Report. January Prof. Dr. Olivier Francis

ONE YEAR WITH OUR ABSOLUTE GRAVIMETER

Brussels, BELGIUM. Bojan Stopar. Faculty of Civil and Geodetic Engineering

Application of ECGS to host the direction of the

Complex Terrain (EDUCT) experiment, conducted by the National Center for Atmospheric

Towards a Rigorous Combination of Space Geodetic Techniques

The 2008 Local-tie Survey at the Onsala Space Observatory

TOWARDS ROBUST LOCALIZATION OF RTK-GPS TOPOGRAPHIC SURVEYS 23

Height systems. Rüdiger Gens

Università degli Studi di Napoli Federico II, Dipartimento di Scienze della Terra Napoli, Italy

Report for 15th PCGIAP Meeting at 18th UNRCC-AP Working Group 1 Regional Geodesy

Tide Gauge Benchmark Monitoring Need for Reprocessing in Europe. Tilo Schöne & the IGS TIGA Working Group

Dependences in the pillar Earth s gravity field of

A new geoid model for Bhutan. Machiel Bos Rui Fernandes

Modernization of National Geodetic Datum in China *

National report of Slovakia 2016

Global & National Geodesy, GNSS Surveying & CORS Infrastructure

THREE SEASONAL BEHAVIOUR OF THE BALKAN PENINSULA GNSS PERMANENT STATIONS FROM GPS SOLUTIONS

Status report of the BKG Gravity Group

Absolute and Relative Gravity Measurements at the Istituto Nazionale di Ricerca Metrologica (INRIM) of Turin (Italy) in June 2006

Recent and future actions about Space Weather in Austria Manuela Temmer

NEW GEODETIC REFERENCE FRAME KOSOVAREV 01

Advances in Ground-based Gravity for Hydrologic Studies

Evaluation and Improvement of the EGG97 Quasigeoid Model for Europe by GPS and Leveling Data

Height systems. Rudi Gens Alaska Satellite Facility

From Global to National Geodetic Reference Frames: how are they connected and why are they needed?

National report of Slovakia 2017

Monitoring of Precipitable Water Vapor Over the Czech Republic by GPS

GEODETIC AND GEODYNAMIC STUDIES AT DEPARTMENT OF GEODESY AND GEODETIC ASTRONOMY WUT

On the use of meteo data. How to raise the value of EPN s

The National Spatial Reference System of the Future

The PaTrop Experiment

Integration of space and terrestrial techniques to study crustal deformation. Examples in northeastern Italy

The Global Geodetic Observing System (GGOS) of the International Association of Geodesy (IAG)

Exploitation of ground based GPS for Climate and Numerical Weather Prediction applications COST action 716

Characterization of an Atom Interferometer Gravimeter with Classical Sensors for the Use in Geodesy and Geophysics

Earth gravity field recovery using GPS, GLONASS, and SLR satellites

Case study of Japan: Reference Frames in Practice

2 Sofia University, Sofia, Bulgaria. C Hackman 1, Guergana Guerova 2, S Byram 1, J Dousa 3 and U Hugentobler 4

FIELD TESTS OF THE PORTABLE ABSOLUTE GRAVIMETER FOR THE REMOTE APPLICATIONS Paper presented on AGS99

Ground-based GPS networks for remote sensing of the atmospheric water vapour content: a review

A new gravity laboratory in Ny-Ålesund, Svalbard

Determination of Current Velocity Field (Rate) of North Anatolian Fault in Izmit-Sapanca Segment

Impact of A Priori Gradients on VLBI-Derived Terrestrial Reference Frames

Impact of A Priori Gradients on VLBI-Derived Terrestrial Reference Frames

GRAVITY MEASUREMENTS IN THE GEODYNAMIC NETWORK SUDETY

Transcription:

ECGN - Development of the European Combined Geodetic Network in Austria Diethard Ruess 1, Gelöscht: BEV Dept. Control Survey Abstract Austria takes part in the European Combined Geodetic Network - Project with three different stations: Graz, Trafelberg and Pfänder. One of them - Graz (= IGS) - is the oldest station and therefore it has got a very long time series for the position and the combination of GPS and laser instruments, whereas Trafelberg, a very new station, combines geodetic, gravimetric and seismic measurement devices. The presentation will concentrate on the present state of the three stations in Austria. ECGN - Aims / topics: Investigation of the long time stability of the European Terrestrial Reference System ETRS89 In-situ combination of geometric information (3-D coordinates measured by GPS with physical information (heights and other Earth gravity parameters) with an accuracy level of <±1 cm The ECGN is an European network for the integration of time series of spatial/geometric observations (GNSS GPS/ GLONASS and in the future GALILEO), gravity field related observations and parameters (gravity, tides, ocean tides), and supplementary information (meteorological parameters, surrounding information of the stations e.g. eccentricities and ground water level). Fig. 1: Distribution of ECGN-stations in Europe (Ihde, 2005) ECGN Stations in Austria There are 3 different ECGN stations established in Austria. (Fig. 2) 1 Federal Office of Metrology and Surveying, Schiffamtsgasse 1-3, A-1025 Vienna, Austria, diethard.ruess@bev.gv.at Formatiert: Englisch (Großbritannien) Formatiert: Englisch (Großbritannien)

The main station is situated in Graz at the space laboratory on Lustbühel connected to the SLR station. The second station is on the mount Pfänder near Bregenz in Vorarlberg. This station has been part of the Austrian Geodynamic Reference Network (AGREF) since 1992. The permanent GPS observations have been run since 1997. The third station is situated near Vienna at the new geophysical observatory of the ZAMG, where seismic and gravimetric observation are disposed. All stations are connected to the second order levelling network of Austria which is part of the UELN. Gravity values and consequently geopotential units and orthometric heights are available. All three stations are part of the Austrian Positioning Service (APOS). Gelöscht: ystem Fig. 2: The ECGN stations in connection with the levelling network in Austria Station GRAZ The station GRAZ is situated at the observatory of the Institute of Space Research of the Austrian Academy of Sciences (IWF-OeAW). (Fig. 3)

Fig. 3: ECGN station GRAZ On the roof of the observatory of GRAZ-Lustbühel there are several GPS antennas that have been operating since 1992. In 1993 the levelled benchmark below the antenna GRAZ was connected to the precise levelling network and in combination with the 2004 measured gravity value the orthometric height was obtained. In the background the astrodome of the satellite laser can be seen. (Fig. 4). Fig. 4: Antennas at the ECGN station GRAZ "GRAZ" is also a station of the International GPS Service. The SLR has been operating very successfully since 1982. Since October 2003 a new 2 khz satellite laser ranging system has been operating. Now the SLR station measures three times more returns from Lageos-1 than all other SLR stations. The results of lower satellites are much better than before, too. A lot of local ties exist around the observatory, because this location has been used for astro-geodetic observations from the very beginning. The absolute gravity station at the ground floor was established in 1998 during the UNIGRACE campaign (Fig. 5). The local gravimetric ties around the building have been 1 st order points of the ÖSGN (Österreichisches Schweregrundnetz = Austrian Gravity Base Network) since 1980. Fig. 5: JILAg-6 absolute gravity observation in GRAZ

Station PFAN The ECGN station PFAN is located on the ridge of mount Pfänder at 1042 m, 646m above the Bodensee (Lake Constance). (Fig. 6) Fig. 6: ECGN station PFAN Fig. 7: Image of the permanent station PFAN and the surroundings. The absolute gravity observations are done at the garage of a farmer near by, about 30 m below the GPS-antenna. The gravity transfer to the GPS station is done by relative gravimeters. The GPS receiver (and the complete electronically equipment) is placed in the small chamber below the antenna. (Fig. 7). The absolute gravity observations are done in the very stable founded implement shed of the farmer. (Fig. 8)

Fig. 8: Absolute gravity measurements at PFAN Station TRFB The Conrad-Observatory (COBS) of the "ZAMG (Zentralanstalt für Meteorologie und Geodynamik) built on Trafelberg (TRFB) is situated about 50 km SW of Vienna in the calcareous part of the foothills of the Eastern Alps at 1044m. The remoteness of the location and the undisturbed surroundings of the underground observatory guarantee an extreme low background noise and allow special investigations and long term research projects to be conducted - tasks, which will gain importance in the near future (Fig. 9). Fig. 9: ECGN station TRFB at the geophysical underground observatory The observatory is used not only for seismic observations but also for gravimetric and in future for magnetic investigations in a separate building. The first part was opened in May 2002 and contains a 145m long tunnel with several instrument pillars for seismometers, a room with 4 vertical boreholes (50 and 100m), a gravity laboratory, an office room and the necessary adjoining rooms.

The GPS pillar was built in 2004 in front of the west-side of the building. A special room the Gravity Lab was constructed for gravimetric investigations. There a big concrete socked weighing about 80 tons was built directly on the rock. Its foundation of 8 x 2 meters allows to measure gravity with at least 3 big instruments like superconducting tidal gravimeters and free fall absolute gravimeters (see the image-picture). (Fig. 10) Fig. 10: Image of superconducting and absolute gravimeters Fig. 11: Absolute gravimetry inside the Gravity Laboratory In 2003 first absolute gravity measurements were carried out. The foundation of the place is very stable and the surroundings indeed are very quiet. Therefore a mean drop sigma of 70nm/s² (7 µgal) could be achieved (Fig. 11). Very important is the determination of the local vertical gravity gradient at the certain point res. the gravity differences between the various reference points. The superconducting tidal gravimeter GWR will be transferred from the present station Vienna to the Conrad Observatory soon. In Vienna a permanent run over the last 10 years could be achieved. Side by side simultaneous absolute observations are necessary to check the instrument factor and the drift of the SCG. (Fig. 12) Fig. 12: The SCG tidal gravimeter and the JILAg-6 absolute meter side by side One part of the Conrad Observatory consists of a tunnel of 145m length for seismic investigations and seismometer comparisons. There are several independent instrumental pillars. The tunnel is orientated exactly West to East. All pillars contain benchmarks of the precise levelling network to check the longterm stability. (Fig. 13)

Fig. 13: Tunnel for seismic observations at COBS A lot of local ties in and around the observatory allow to check the stability of the station over a long period of time. Influences and future aspects As yet no meteorological automatic equipments are implemented. To detect correlations between different observation signals, it would be of interest to measure precipitation, temperature, air pressure, humidity, etc. Also the influence of changing groundwater levels on the gravity values may not be neglected. Therefore groundwater gauges should be installed nearby. Further studies of atmospheric parameters due to zenith path delays are in progress, particularly of the integrated water vapour of the troposphere. The correlation of large pressure areas and GPS height monitoring in correlation to gravity changes could give interesting insights in the crust elastics. The repetition of absolute & relative gravity measurements and the checking of the local ties will be done periodically. References: Ihde, J., et al., 2005: The Implementation of the ECGN stations Status of the 1st Call for participation. EUREF-Symp. 2005, Vienna. Hammerl, Ch., Lenhardt, W., 2005: 100 Years Seismological Service in Austria, ZAMG, Vienna.