Linking GPS to Tide Gauges and Tide Gauge Benchmarks Tilo Schöne GeoForschungsZentrum Potsdam Understanding Sea-level Rise and Variability, WCRP Workshop,

Slides:



Advertisements
Similar presentations
The Geoscience Australia’s Online GPS Processing Service (AUSPOS)
Advertisements

Philip L. Woodworth Permanent Service for Mean Sea Level With an enormous amount of assistance from Norman Teferle and Richard Bingley University.
Geodesy at a Tide Gauge Where the Tide Gauge Operator meets the Surveyor Tilo Schöne GeoForschungsZentrum Potsdam Phil Woodworth (PSMSL) & Simon Williams.
Reference Frames for GPS Applications and Research
Effect of Surface Loading on Regional Reference Frame Realization Hans-Peter Plag Nevada Bureau of Mines and Geology and Seismological Laboratory University.
2-3 November 2009NASA Sea Level Workshop1 The Terrestrial Reference Frame and its Impact on Sea Level Change Studies GPS VLBI John Ries Center for Space.
LINDA MORGAN PRINCIPAL CONSULTANT – SPATIAL POSITIONING WESTERN AUSTRALIA SURVEYING CONFERENCE 2013 Geodetic Stuff You Need to Know: Datums, Standards.
OLG LAC Reprocessing EPN 2006 G. Stangl 1, C. Aichhorn 2, S. Krauss 2 (1) Federal Office of Metrology and Surveying (BEV)‏ (2) Space Research Institute,
Tide Gauge Benchmark Monitoring Need for Reprocessing in Europe Tilo Schöne & the IGS TIGA Working Group.
International Terrestrial Reference Frame - Latest Developments Horst Müller 16th International Workshop on Laser Ranging, Poznan, Poland, October
2015 Height Modernization Partner Meeting April 14, 2015.
EPN LAC Workshop 2008 Frankfurt Main, Germany, October, 2008 ASI Local Analysis Center Report C. Ferraro, Telespazio/CGS Matera R. Pacione, e-GEOS/CGS.
ILRS Workshop, Poznan, Poland, October Status of ITRF Development and SLR Contribution Zuheir Altamimi Xavier Collilieux David Coulot IGN France.
Better Positions and Improved Access to the National Spatial Reference System  Multi-Year CORS Solution  National Adjustment of 2011  New NGS Datasheet.
The IGS contribution to ITRF2014 Paul Rebischung, Bruno Garayt, Zuheir Altamimi, Xavier Collilieux 26th IUGG General Assembly, Prague, 28 June.
The Global Sea Level Observing System (GLOSS) 2012 Mark Merrifield University of Hawaii Requirements Status Strategies Partnerships Emerging technologies.
Workshop, Miami, June 2008 ITRF2005 residuals and co-location tie issues Zuheir Altamimi IGN, France Some features of ITRF2005 residuals ITRF2005 vs IGS05.
IGS Analysis Center Workshop, Miami Beach, 2-6 June 2008 M. Fritsche, R. Dietrich, A. Rülke Institut für Planetare Geodäsie (IPG), Technische Universität.
AUSPOS Online GPS Processing Service John Manning, John Dawson.Ramesh Govind Geoscience Australia.
Recent IERS Site Survey of Multiple Co-located Geodetic Techniques by NGS Kendall Fancher, Dru Smith, Steve Breidenbach, Jeff Olsen, Nagendra Paudel NOAA’s.
IGS Analysis Center Workshop, Miami Beach, June 2008 Comparison of GMF/GPT with VMF1/ECMWF and Implications for Atmospheric Loading Peter Steigenberger.
RFWG report ______________________ IGS 39th Governing Board Meeting San Francisco, 3 December
WEGENER Nice 2006 OLG Monitoring of the Eastern Mediterranean and Arabia Velocitiy Estimations of Permanent GPS Stations 1Space Research Institute, Austrian.
1 North American Reference Frame (NAREF) Working Group Mike Craymer Geodetic Survey Division, Natural Resources Canada 2nd SNARF Workshop Montreal, May.
A New & Improved National Spatial Reference System Refinements of the North American Datum of 1983 through the Multi-Year CORS Solution and the National.
NGS GPS ORBIT DETERMINATION Positioning America for the Future NATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION National Ocean Service National Geodetic.
Reference Frame Theory and Practice Kristine Larson University of Colorado.
Regional and Global Measurements: The Reference Frame for Understanding Observations Geoff Blewitt University of Nevada, Reno, USA Zuheir Altamimi IGN,
October 8, session 2REFAG2010 Paris1 Distributed processing systems for large geodetic solutions IAG WG “Comparison and combination of precise.
1/17 REFAG Symposium 6 October 2010 – Marne-la-Vallée, France Recent Results from the IGS Terrestrial Frame Combinations __________________________________________________________________________________________________.
Space Geodesy (1/3) Geodesy provides a foundation for all Earth observations Space geodesy is the use of precise measurements between space objects (e.g.,
IGS Analysis Center Workshop, 2-6 June 2008, Florida, USA GPS in the ITRF Combination D. Angermann, H. Drewes, M. Krügel, B. Meisel Deutsches Geodätisches.
Geodetic Networks: The Supporting Framework Terrestrial Reference Frame is ‘Critical Infrastructure’ for all Earth science research and applications. Global.
NKG Working Group for Geodynamics Copenhagen, 23 –24 April, Tasks of a new Working Group on Absolute Gravimetry Herbert Wilmes Federal Agency for.
1 AOGS 2012, Singapore, Aug 13-17, 2012 Surveying co-located GNSS/VLBI/SLR Stations In China Xiuqiang Gong, Yunzhong Shen, Junping Chen, Bin Wu Shanghai.
The IGS contribution to ITRF2013 – Preliminary results from the IGS repro2 SINEX combinations Paul Rebischung, Bruno Garayt, Xavier Collilieux, Zuheir.
SPACE GEODESY NETWORK & ITRF Z Minchul LEE 1.
Deformation Analysis in the North American Plate’s Interior Calais E, Purdue University, West Lafayette, IN, Han JY,
Tide gauge stations: requirements, status, and issues Mark Merrifield University of Hawaii Sea Level Center.
TERRESTRIAL REFERENCE SYSTEMS FOR GLOBAL NAVIGATION SATELLITE SYSTEMS
AGU Fall meeting Quality assessment of GPS reprocessed Terrestrial Reference Frame 1 IGN/LAREG and GRGS 2 University of Luxembourg X Collilieux.
National Geodetic Survey – Continuously Operating Reference Stations & Online Positioning User Service (CORS & OPUS) William Stone Southwest Region (UT,
Earth, Atmospheric and Planetary Sciences Massachusetts Institute of Technology 77 Massachusetts Avenue | Cambridge MA V F
Earth Sciences Sector SLIDE 1 NAREF & CBN Velocity Solutions for a New Version of SNARF Mike Craymer Joe Henton Mike Piraszewski 8th SNARF Workshop AGU.
Calibration of geodetic (dual frequency) GPS receivers Implications for TAI and for the IGS G. Petit.
Assessment of Reference Frame Stability trough offset detection in GPS coordinate time series Dragan Blagojević 1), Goran Todorović 2), Violeta Vasilić.
Recommendation 1 The IGS shall develop a standard protocol for exchanging information about IGS stations. The associated machine-readable database should.
The International GNSS Service (IGS), June 2008: Perspectives and Key Issues John M. Dow Chair, IGS Governing Board.
Introduction Ian Thomas, Matt King, Peter Clarke, Nigel Penna, David Lavallée Global GPS Processing strategy Conclusions and Future Work The preliminary.
1/16 ITRF2008-P: Some evaluation elements and impact on IGS RF products Paul Rebischung, Bruno Garayt, 16 April 2010 ITRF2008-P: SOME EVALUATION ELEMENTS.
NGOS NORDIC GEODETIC OBSERVING SYSTEM NKG Task Force Markku Poutanen, Per Knudsen, Mikael Lilje, Hans-Peter Plag, Hans-Georg Scherneck.
International Workshop on Laser Ranging, October 2008, Poznań (Poland) Quality assessment of the ILRS EOP „Daily” Product G. Bianco Agenzia Spaziale.
Earth Surface and Interior Focus Area Space Geodetic Networks for Maintaining the Reference Frame Geodesy's Critical Contributions to NASA (Earth Science)
Reprocessing GPS data at the observation level for tide gauge monitoring: G. Wöppelmann, Tilo Schöne IGS Analysis Center Workshop 2008, 2-6 June 2008,
View on GPS and Galileo ‘From across the Atlantic…’ Ruth E. Neilan International GNSS Service (IGS) Central Bureau Jet Propulsion Laboratory/California.
A proposal for a consistent model of air pressure loading as part of the International Terrestrial Reference System (ITRS) Conventions Plag, H.-P. (1),
Geodetic Networks: The Supporting Framework Terrestrial Reference Frame is ‘Critical Infrastructure’ for all Earth science research and applications. Global.
Workshop, Miami, June 2008 IGS Contribution to ITRF Zuheir Altamimi & Xavier Collilieux IGN, France.
Vertical velocities at tide gauges from a completely reprocessed global GPS network of stations: How well do they work? G. Wöppelmann 1, M-N. Bouin 2,
Armasuisse Swiss Federal Office of Topography swisstopo Determination of Tectonic Movements in the Swiss Alps using GNSS and Levelling E. Brockmann, D.
NAPEOS: The ESA/ESOC Tool for Space Geodesy
Importance of SLR in the Determination of the ITRF Zuheir Altamimi IGN, France Geoscience Australia, Canberra, August 29, 2005 SLR Strength: its contribution.
Software Development: Massive, Rapid Network Processing with Ambiguity Resolution Geoff Blewitt.
Canada’s Natural Resources – Now and for the Future Reference Frames Panel Discussion M. Craymer Geodetic Survey Division, Natural Resources Canada IAG.
29 August 2005Geosciences Australia1 Space Geodesy, SLR and Global Sea Level Change John Ries Canberra, Australia August 29,,2005.
IERS Combination WG and CPP Meeting, April 27, 2005, TU of Vienna, Austria Status and Future of the IERS Combination Efforts Markus Rothacher GeoForschungsZentrum.
IERS Combination WG and CPP Meeting, April 27, 2005, TU of Vienna, Austria Strategies for Weekly Routine Generation of Combined IERS Products Markus Rothacher.
IERS Directing Board Meeting No.39, BIPM Paris, September 23, 2004 IERS2005: Plan “Integrated Earth orientation parameters, Radio sources, and Site coordinates.
Real-Time Working Group
GPS Network: Status GFZ
Presentation transcript:

Linking GPS to Tide Gauges and Tide Gauge Benchmarks Tilo Schöne GeoForschungsZentrum Potsdam Understanding Sea-level Rise and Variability, WCRP Workshop, UNESCO, June 2006, PARIS

Why the Vertical * Long-term stable and consistent frame to relate ALL globally distributed sea level related measurements Long-term stable and consistent frame to relate ALL globally distributed sea level related measurements Short-term control in earthquake-prone areas Short-term control in earthquake-prone areas Provide pointwise constraints for e.g. uplift modelers Provide pointwise constraints for e.g. uplift modelers * Workshop related issues

From Tide Gauges to First (known) continuous measurements in Europe by the Royal Society of London (founded in 1660) Description of a “floating tide gauge device” by Athanasius Kircher in the horologium aestus marini (around 1665) After 1880 increase in number of tide gauges … After 1980 the GPS system was developed Since 2000 increase in number of GPS equipped tide gauges

From the past to the present GAVDOS Project Mertikas et al., SPIE conference, 2002 A. Ott (Kempten) (1885)

Tide Gauges and GPS Tide gauges have a long technical and measurement history Tide gauges have a long technical and measurement history Well maintained and with a stable local network of benchmarks Well maintained and with a stable local network of benchmarks Local water level changes only, even with ties to 1st order leveling networks Local water level changes only, even with ties to 1st order leveling networks Sea level and changes required in long-term stable global reference frames Sea level and changes required in long-term stable global reference frames GPS is the easy-to-use technique to solve for this problem, but … GPS is the easy-to-use technique to solve for this problem, but …

IGS-GPS network and IGS network: Geographically balanced Some clustering in populated areas Optimized point distances Strict requirements on latency (minutes to a few days) Sites along coastlines Many clusters in Europe, Japan, USA Short GPS baselines, sometimes multiple receivers at one site Many remote and manually operated sites © IGSCB However, the IGS is the best source for GPS time series for many sites

Problems with IGS-solutions and more generally More tide gauges equipped with GPS than available within IGS (completeness) More tide gauges equipped with GPS than available within IGS (completeness) Strict timeliness in GPS data provision (latency) Strict timeliness in GPS data provision (latency) Currently, accuracy and continuity of GPS time series is limited (accuracy of the vertical) Currently, accuracy and continuity of GPS time series is limited (accuracy of the vertical) Tide gauge / GPS operators are of different agencies Tide gauge / GPS operators are of different agencies Frequent reprocessing of GPS and inclusion of high-latency data is still a challenging task Frequent reprocessing of GPS and inclusion of high-latency data is still a challenging task

GFZ-AC (IGS) versus GFZ- Reprocessing Differences due to Software developments Better correction models Improved processing strategies More complete station coverage

TIGA Tide Gauge Benchmark Monitoring Pilot Project of the IGS

TIGA Pilot Project Initiated in 2001 Initiated in 2001 Goals are Goals are –Establish, maintain and expand a global network –Compute precise station parameters for the stations with a high latency –Reprocess all previously collected GPS data at stations, if possible back to 1993 –Promote the establishment of links to other geodetic sites which may contribute to vertical motion determination (DORIS, SLR, VLBI, AG)

TIGA Pilot Project 102 out of 280 stations contribute 102 out of 280 stations contribute Processing latency 460 days Processing latency 460 days Six analysis centers provide solutions Six analysis centers provide solutions Forward (since GPS week 1121) and backward processing on a best-effort basis Forward (since GPS week 1121) and backward processing on a best-effort basis Backward processing to 1993 Backward processing to 1993 Preparations for the combination started at GFZ; will provide a combination solution on a regular basis Preparations for the combination started at GFZ; will provide a combination solution on a regular basis

CTA DGFI ULR Geoscience Australia EUREF GFZ TIGA Network TOS fully acceptedProposed

GFZ: AC versus TIGA ITRF96 ITRF97 IGS00 TIGA Start RMS North/East/Height Residuals [mm]

Comparison of TIGA Solutions Number of Points RMS North/East/Height Residuals [mm]

TIGA: Combination for 2002 < 3 mm < 7 mm Daniela Thaller, GFZ

TIGA: Combination for 2002 Daniela Thaller, GFZ

Lessons learned (+) * Station repeatability (7mm) same level as IGS Station repeatability (7mm) same level as IGS Reduced height variability for the reprocessed data Reduced height variability for the reprocessed data More consistent, no discontinuities at ITRF-changes More consistent, no discontinuities at ITRF-changes High latency of processing allows more stations to contribute High latency of processing allows more stations to contribute Massive contribution to the new ITRF Massive contribution to the new ITRF Loading effects must be evaluated in detail Loading effects must be evaluated in detail Data useful for e.g. uplift modelers Data useful for e.g. uplift modelers * Workshop related issues

Lessons learned (-) * Solution becomes outdated (e.g. absolute pcv’s), but cleaned input data are kept Solution becomes outdated (e.g. absolute pcv’s), but cleaned input data are kept No consolidated and agreed data base on station discontinuities is available No consolidated and agreed data base on station discontinuities is available Few areas are very little represented Few areas are very little represented Meta information (especially ties) are not well documented or updated Meta information (especially ties) are not well documented or updated Loading effects are affecting GPS time series different ashore and inland Loading effects are affecting GPS time series different ashore and inland Distance between GPS and TG benchmarks are to large to be representative and accurate Distance between GPS and TG benchmarks are to large to be representative and accurate * Workshop related issues

Schedule for TIGA Starting Summer 2006, GFZ will provide a first set of coordinates/velocities for all TIGA sites based on a combined solution of the recent reprocessing Starting Summer 2006, GFZ will provide a first set of coordinates/velocities for all TIGA sites based on a combined solution of the recent reprocessing Reprocessing with absolute pcv’s and based on ITRF2005 Reprocessing with absolute pcv’s and based on ITRF2005 Studies on optimal combination of TIGA solutions Studies on optimal combination of TIGA solutions Independent checks of the results and intercomparison to TG, AG (by the community) Independent checks of the results and intercomparison to TG, AG (by the community) The goal is to turn TIGA into an IGS service The goal is to turn TIGA into an IGS service It’s a good time to open your now!

What will you get from us? Coordinates and velocities (focus on the vertical) for the GPS sites at or near tide gauges (and other GPS sites) Coordinates and velocities (focus on the vertical) for the GPS sites at or near tide gauges (and other GPS sites) Reference sites Reference sites and when? End of 2006, beginning 2007 End of 2006, beginning 2007

What do we need from you? Provision of GPS data at tide gauge sites on a regular basis Provision of GPS data at tide gauge sites on a regular basis Local ties between the GPS and tide gauge benchmark Local ties between the GPS and tide gauge benchmark Maintenance of the “system” Maintenance of the “system” Feedback! Feedback!

Thanks to the six analysis centers the six analysis centers –EUREF (etg) –Geodätisches Forschungsinstitut München (dgf) –GeoForschungsZentrum Potsdam (gft) –Geoscience Australia (aut) –Universities Canberra, ANU, and Tasmania (cta) –University La Rochelle (ulr) the numerous operators of tide gauges and GPS stations the numerous operators of tide gauges and GPS stations the surveyors carrying out the leveling the surveyors carrying out the leveling the IGS for providing support and the infrastructure the IGS for providing support and the infrastructure