1. The International Terrestrial Reference Frame (ITRF) needs to be made more robust and stable over multi-decadal time scales. –target accuracy is 0.1.

Slides:



Advertisements
Similar presentations
Reference Frames for GPS Applications and Research
Advertisements

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.
PNT Advisory Board| Alexandria, Virginia | November 5 – 6, 2009 | 0 Michael Pearlman Director Central Bureau International Laser Ranging Service Harvard-Smithsonian.
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.
The Four Candidate Earth Explorer Core Missions Consultative Workshop October 1999, Granada, Spain, Revised by CCT GOCE S 43 Science and.
ASIC**3 Workshop -- May 2006 Measuring Global Sea Level Rise With Satellite Radar Altimetry ASIC**3 Workshop -- May 2006 Laury Miller NOAA/NESDIS Lab for.
ILRS Workshop, Poznan, Poland, October Status of ITRF Development and SLR Contribution Zuheir Altamimi Xavier Collilieux David Coulot IGN France.
Summary: Scientific Achievement, Applications and Future Requirements Zueheir Altamimi Steve Klosko Richard Gross Aleksander Brzezinski.
GPS – Global Positioning System Space segment Control segment user segment 32 satellites World wide monitor and control stations.
Laser Ranging Contributions to Earth Rotation Studies Richard S. Gross Jet Propulsion Laboratory California Institute of Technology Pasadena, CA 91109–8099,
A changing approach to geodetic networks and standards MATT AMOS and DON GRANT.
Principles of Sea Level Measurement Long-term tide gauge records  What is a tide station?  How is sea level measured relative to the land?  What types.
Monitoring the Global Sea Level Rise Budget with Jason, Argo and GRACE Observations Eric Leuliette and Laury Miller NOAA/Laboratory for Satellite Altimetry.
DISCUSSION SESSION 3: FUTURE PPP USER SOLUTIONS GNSS PPP W ORKSHOP : R EACHING F ULL P OTENTIAL J UNE 2013, O TTAWA What will near-term PPP user.
DORIS - DAYS Toulouse May 2-3, 2000 DORIS Doppler Orbitography and Radiopositioning Integrated by Satellite  Basic system concept  Main missions  Schedules.
The Contribution to GGOS from Asian Region Jong Uk Park & Young-Hong Shin Space Geodesy Division, Korea Astronomy and Space Science Institute, Daejeon,
The Global Geodetic Observing System: Meeting the Requirements of a Global Society on a Changing Planet in 2020 Hans-Peter Plag, Reiner Rummel, Dork Sahagian,
NASA, CGMS-41, July 2013 Coordination Group for Meteorological Satellites - CGMS The Terrestrial Reference Frame by NASA Presented to CGMS-41 Working Group.
Task AR-07-03: Global Geodetic Reference Frames Report to ADC-5 prepared by Hans-Peter Plag (IAG/GGOS) Nevada Bureau of Mines and Geology and Seismological.
IGCP 565: The workshop series and recommendations Hans-Peter Plag Nevada Bureau of Mines and Geology and Seismological Laboratory, University of Nevada,
Hydrogeodesy: Can it help to reach the Millennium Development Goal for Water in Africa? Norman L. Miller IGCP 565 Fifth Annual Workshop October 2012.
Regional and Global Measurements: The Reference Frame for Understanding Observations Geoff Blewitt University of Nevada, Reno, USA Zuheir Altamimi IGN,
ILRS WorkshopEastbourne, UK October 3 -7, 2005 Global Geodetic Observing System (GGOS) A project of the IAG.
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.,
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.
Sea Level Change Measurements: Estimates from Altimeters Understanding Sea Level Rise and Variability June 6-9, 2006 Paris, France R. S. Nerem, University.
Towards the unification of the vertical datums over the North American continent D Smith 1, M Véronneau 2, D Roman 1, J L Huang 2, YM Wang 1, M Sideris.
Determination of seasonal geocenter variations from DORIS, GPS and SLR data.
SPACE GEODESY NETWORK & ITRF Z Minchul LEE 1.
Faculty of Applied Engineering and Urban Planning Civil Engineering Department Introduction to Geodesy and Geomatics Position, Positioning Modes, and the.
Estimates of Global Sea Level Rise from Tide Gauges Sea level trend,
GGOS User Requirements and Functional Specifications Richard S. Gross Jet Propulsion Laboratory, California Institute of Technology, Pasadena, USA Global.
1 Geoid and Geoid Change: Discussion Topics Roger Haagmans, Boulder, 21October 2009.
Global monitoring of runoff and lake storage: - important elements of Integrated Global Observing Systems - integral parts of water resources management.
TERRESTRIAL REFERENCE SYSTEMS FOR GLOBAL NAVIGATION SATELLITE SYSTEMS
01/0000 HEO and Daylight Ranging “Reality and Wishes” Ramesh Govind ILRS Fall Workshop, 4 th October 2005.
GGOS Presentation to the CEOS Strategic Implementation Team 28th Meeting March 14, 2013 Hampton, VA, USA Proposed: CEOS Participation in the Decade Long.
The ICRF, ITRF and VLBA Chopo Ma NASA’s Goddard Spaceflight Center.
GPS: “Where goeth thou” Thomas Herring With results from Jen Alltop: Geosystems Thesis Katy Quinn: Almost graduated Ph.D
Combining CMORPH with Gauge Analysis over
On the vision of an International Altimeter Service (IAS) Invitation to discuss the IAS Wolfgang Bosch, On the vision of an International.
NGOS NORDIC GEODETIC OBSERVING SYSTEM NKG Task Force Markku Poutanen, Per Knudsen, Mikael Lilje, Hans-Peter Plag, Hans-Georg Scherneck.
MISSISSIPPI HEIGHT MODERNIZATION PROJECT JUNE 11, 2009 By Ronnie L. Taylor Chief, Geodetic Advisor Branch NOAA, National Geodetic Survey.
Reference Frame Theory & Practice: Implications for SNARF SNARF Workshop 1/27/04 Geoff Blewitt University of Nevada, Reno.
Earth Surface and Interior Focus Area Space Geodetic Networks for Maintaining the Reference Frame Geodesy's Critical Contributions to NASA (Earth Science)
Earth Observation Support for Adaptation to an Uncertain Sea Level Rise Hans-Peter Plag Nevada Bureau of Mines and Geology & Seismological Laboratory University.
View on GPS and Galileo ‘From across the Atlantic…’ Ruth E. Neilan International GNSS Service (IGS) Central Bureau Jet Propulsion Laboratory/California.
SPP Mass Transport and Mass Distribution in the Earth System Contribution of the New Generation of Satellite Gravity and Altimetry Missions to Geosciences.
Satellite geodesy (ge-2112) Introduction E. Schrama.
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.
Earth Surface and Interior Focus Area Space Geodetic Networks for Maintaining the Reference Frame Geodesy's Critical Contributions to NASA (Earth Science)
12/12/01Fall AGU Vertical Reference Frames for Sea Level Monitoring Thomas Herring Department of Earth, Atmosphere and Planetary Sciences
NAPEOS: The ESA/ESOC Tool for Space Geodesy
11-12 April 2005NASA Sea Level Workshop1 SPACE GEODETIC MEASUREMENT SYSTEM FOR GLOBAL SEA LEVEL CHANGE "In all things it is a good idea to hang a question.
Nic Donnelly – Geodetic Data Analyst 5 March 2008 Vertical Datum Issues in New Zealand.
Importance of SLR in the Determination of the ITRF Zuheir Altamimi IGN, France Geoscience Australia, Canberra, August 29, 2005 SLR Strength: its contribution.
29 August 2005Geosciences Australia1 Space Geodesy, SLR and Global Sea Level Change John Ries Canberra, Australia August 29,,2005.
Earth Surface and Interior Focus Area Space Geodetic Networks for Maintaining the Reference Frame Geodesy's Critical Contributions to NASA (Earth Science)
Geodetic Control and Datums Where is it? How Accurately can we map it?
Ggim.un.org Positioning geospatial information to address global challenges Global and National Geodetic Reference Frames: how they are connected and why.
Last Time: Introduction to Gravity Governed by LaPlace’s equation: with solution of the form: If we have a spherical body with mass M and constant (or.
IERS Combination WG and CPP Meeting, April 27, 2005, TU of Vienna, Austria Status and Future of the IERS Combination Efforts Markus Rothacher GeoForschungsZentrum.
ESA Climate Change Initiative Sea-level-CCI project A.Cazenave (Science Leader), G.Larnicol /Y.Faugere(Project Leader), M.Ablain (EO) MARCDAT-III meeting.
Reference Frame Representations: The ITRF from the user perspective
The next 3 figures are from the Ocean Pathfinder Project at NASA/GSFC The next 3 figures are from the Ocean Pathfinder Project at NASA/GSFC. Compliments.
Presentation transcript:

1. The International Terrestrial Reference Frame (ITRF) needs to be made more robust and stable over multi-decadal time scales. –target accuracy is 0.1 mm/yr in the realization of the center of mass of the entire Earth system (“geocenter stability”), –0.01 ppb in scale stability, 0.6 mm/yr This requires strong connections between the reference frames of the various geodetic systems Geodetic Observations - Recommendations

The strong connections between the reference frames of the various geodetic systems require: a.Implement more sites of every technique with a good (even) global distribution b.Collocate different techniques c.Sustain and evolve support for the scientific services (i.e., IERS, IGS, IVS, ILRS, IDS), d.Place laser retro-reflectors on all future GNSS satellites, e.Support Global Geodetic Observing System (GGOS) as the new paradigm f.Conduct research into understanding biases g.Conduct research towards improving tropospheric delay models. Geodetic Observations - Recommendations

3. Ensure long term stability and consistency in the measurements of sea level by altimetry and of mass by GRACE-type missions, (a) analogues of current altimeter and gravity missions be continued indefinitely with sufficient overlap between missions, and with no gaps between missions; (b) a world vertical datum be established 4. Tide gauges be monitored for height variations using continuous GPS systems installed directly at the tide gauge - additional tide gauges, co-located with GPS, be installed in areas with poor tide gauge coverage. 5. Research and development of comprehensive Earth models that can assimilate all geodetic data types (including tide gauge data) that are relevant to determining sea level change. At the next level, the models should be integrated with terrestrial hydrological models, cryospheric models, and ocean/atmospheric circulation models. 6. In order to achieve the goal of determining sea level changes at the level of 0.1 mm/yr, support for the recommended systems and research activities must be brought up to a level capable of meeting that goal, and the support must at least be sustained for decades. Geodetic Observations - Recommendations