GOCE/GRACE GGM evaluation over Greece with GPS/Leveling and gravity data G.S. Vergos, V.D. Grigoriadis, I.N. Tziavos, D.A. Natsiopoulos, E.A. Tzanou.

Slides:



Advertisements
Similar presentations
NADIR workshop - October 25-26, 2011page 1 / 16 Density and Winds Inferred from GOCE Accelerometer (thrusters) Data Sean Bruinsma CNES, Toulouse Eelco.
Advertisements

A Comparison of topographic effect by Newton’s integral and high degree spherical harmonic expansion – Preliminary Results YM Wang, S. Holmes, J Saleh,
Ocean circulation estimations using GOCE gravity field models M.H. Rio 1, S. Mulet 1, P. Knudsen 2, O.B. Andersen 2, S.L. Bruinsma 3, J.C. Marty 3, Ch.
Datums, Heights and Geodesy Central Chapter of the Professional Land Surveyors of Colorado 2007 Annual Meeting Daniel R. Roman National Geodetic Survey.
National report of LITHUANIA THE 4th BALTIC SURVEYORS FORUM, 2013, Ventspils, LATVIA Eimuntas Parseliunas Geodetic Institute of Vilnius Technical University.
The Four Candidate Earth Explorer Core Missions Consultative Workshop October 1999, Granada, Spain, Revised by CCT GOCE S 43 Science and.
An example of gravimetric geoid computation: The Iberian Gravimetric Geoid of 2005.
The Four Candidate Earth Explorer Core Missions Consultative Workshop October 1999, Granada, Spain, Revised by CCT GOCE S 59 Performance.
COMBINED MODELING OF THE EARTH’S GRAVITY FIELD FROM GOCE AND GRACE SATELLITE OBSERVATIONS Robert Tenzer 1, Pavel Ditmar 2, Xianglin Liu 2, Philip Moore.
ARCGICE WP 1.4 ERROR ESTIMATES IN SPATIAL AND SPECTRAL DOMAINS C.C.Tscherning, University of Copenhagen,
ARCGICE WP 5.2 Plan for development of Atctic geoid using GOCE C.C.Tscherning, University of Copenhagen,
Dynamic Planet 2005 Cairns, Australia August 2005
NOAA’s National Geodetic Survey USGG2009 & GEOID09: New geoid height models for surveying/GIS ACSM-MARLS-UCLS-WFPS Conference FEB 2009 Salt Lake.
G13A Towards a New Vertical Datum Daniel R. Roman 1, Xiaopeng Li 2, Simon A. Holmes 3, Vicki A. Childers 4, and Yan M. Wang 1 1. Geosciences Research.
Use of G99SSS to evaluate the static gravity geopotential derived from the GRACE, CHAMP, and GOCE missions Daniel R. Roman and Dru A. Smith Session: GP52A-02Decade.
Geoid improvement over Alaska/Yukon area by GRACE and GOCE models X Li 1, JL Huang 2, YM Wang 3, M Véronneau 2, D Roman 3 1 ERT Inc USA 2 Geodetic Survey.
Error Analysis of the NGS Gravity Database Jarir Saleh, Xiaopeng Li, Yan Ming Wang, Dan Roman and Dru Smith, NOAA/NGS/ERT Paper: G , 04 July 2011,
Advances and Best Practices in Airborne Gravimetry from the U.S. GRAV-D Project Theresa M. Damiani 1, Vicki Childers 1, Sandra Preaux 2, Simon Holmes 3,
Calibration in the MBW of simulated GOCE gradients aided by ground data M. Veicherts, C. C. Tscherning, Niels Bohr Institute, University of Copenhagen,
1 Assessment of Geoid Models off Western Australia Using In-Situ Measurements X. Deng School of Engineering, The University of Newcastle, Australia R.
ESA Living Planet Symposium, Bergen, T. Gruber, C. Ackermann, T. Fecher, M. Heinze Institut für Astronomische und Physikalische Geodäsie (IAPG)
NKG Working Group for Geodynamics Copenhagen, 23 –24 April, Tasks of a new Working Group on Absolute Gravimetry Herbert Wilmes Federal Agency for.
1 Geoid and Geoid Change: Discussion Topics Roger Haagmans, Boulder, 21October 2009.
C.C.Tscherning, University of Copenhagen, Denmark. Developments in the implementation and use of Least-Squares Collocation. IAG Scientific Assembly, Potsdam,
Integration of Future Geoid Models Dan Roman and Yan M. Wang NOAA/NGS Silver Spring, MD USA December 3-4, 2008.
Improved Covariance Modeling of Gravimetric, GPS, and Leveling Data in High-Resolution Hybrid Geoids Daniel R. Roman, Ph.D. Research Geodesist.
Data Requirements for a 1-cm Accurate Geoid
Numerical aspects of the omission errors due to limited grid size in geoid computations Yan Ming Wang National Geodetic Survey, USA VII Hotine-Marussi.
Spectral characteristics of the Hellenic vertical network - Validation over Central and Northern Greece using GOCE/GRACE global geopotential models Vassilios.
Effect of High Resolution Altimetric Gravity Anomalies on the North America Geoid Computations Yan M. Wang and D. Roman National Geodetic Survey NOAA Montreal,
Progress in Geoid Modeling from Satellite Missions
Case study on heterogeneous geoid/ quasigeoid based on space borne and terrestrial data combination with special consideration of GOCE mission data impact.
AUSGeoid Richard Bean Robyn Stevens 26 May Geoid 3D surface of equal gravity (Equipotential) Not smooth like an ellipsoid Transformation needed.
Regional Enhancement of the Mean Dynamic Topography using GOCE Gravity Gradients Matija Herceg 1 and Per Knudsen 1 1 DTU Space, National Space Institute,
International Symposium on Gravity, Geoid and Height Systems GGHS 2012, Venice, Italy 1 GOCE data for local geoid enhancement Matija Herceg Per Knudsen.
Full Resolution Geoid from GOCE Gradients for Ocean Modeling Matija Herceg & Per Knudsen Department of Geodesy DTU Space living planet symposium 28 June.
C.C.Tscherning, Niels Bohr Institute, University of Copenhagen. Improvement of Least-Squares Collocation error estimates using local GOCE Tzz signal standard.
Lecture 7 – Gravity and Related Issues GISC February 2008.
A comparison of different geoid computation procedures in the US Rocky Mountains YM Wang 1, H Denker 2, J Saleh 3, XP Li 3, DR Roman 1, D Smith 1 1 National.
Investigation of the use of deflections of vertical measured by DIADEM camera in the GSVS11 Survey YM Wang 1, X Li 2, S Holmes 3, DR Roman 1, DA Smith.
ESA living planet symposium Bergen Combination of GRACE and GOCE in situ data for high resolution regional gravity field modeling M. Schmeer 1,
Improving Regional Geoid by optimal Combination of GRACE Gravity Model and Surface Gravity Data YM Wang, DR Roman and J Saleh National Geodetic Survey.
Mayer-Gürr et al.ESA Living Planet, Bergen Torsten Mayer-Gürr, Annette Eicker, Judith Schall Institute of Geodesy and Geoinformation University.
ESA Living Planet Symposium 28 June - 2 July 2010, Bergen, Norway A. Albertella, R. Rummel, R. Savcenko, W. Bosch, T. Janjic, J.Schroeter, T. Gruber, J.
Nic Donnelly – Geodetic Data Analyst 5 March 2008 Vertical Datum Issues in New Zealand.
1 NGA Mission - Data – Collaboration 2009 Workshop on Monitoring North American Geoid Change 21 Oct 2009 NGA Mission - Data – Collaboration 2009 Workshop.
4.Results (1)Potential coefficients comparisons Fig.3 FIR filtering(Passband:0.005~0.1HZ) Fig.4 Comparison with ESA’s models (filter passband:0.015~0.1HZ)
The use of absolute gravity data for validation of GOCE-based GGMs – A case study of Central Europe 1), 2) Walyeldeen Godah 2) Jan Krynski 2) Malgorzata.
Scientific Roadmap towards Height System Unification with GOCE 5th International GOCE User Workshop, Paris, Th. Gruber (1), R. Rummel (1), M.
An oceanographic assessment of the GOCE geoid models accuracy S. Mulet 1, M-H. Rio 1, P. Knudsen 2, F. Siegesmund 3, R. Bingham 4, O. Andersen 2, D. Stammer.
Use of topography in the context of the GOCE satellite mission – some examples Moritz Rexer, Christian Hirt, Sten Claessens, Carla Braitenberg 5 th INTERNATIONAL.
GOCE Gravity Field Models – Overview and Performance Analysis Th. Gruber*, R. Rummel* & High Level Processing Facility (HPF) Team *Institute of Astronomical.
Integration of Gravity Data Into a Seamless Transnational Height Model for North America Daniel Roman, Marc Véronneau, David Avalos, Xiaopeng Li, Simon.
Evaluation of the Release-3, 4 and 5 GOCE-based Global Geopotential Models in North America M. G. Sideris (1), B. Amjadiparvar (1), E. Rangelova (1), J.
D.N. Arabelos, M. Reguzzoni and C.C.Tscherning HPF Progress Meeting # 26, München, Feb , Global grids of gravity anomalies and vertical gravity.
GOCE geoids and derived Mean Dynamic Topography in the Arctic Ocean Ole B. Andersen & Per Knudsen. DTU Space – Copenhagen, Denmark.
ESA Living Planet Symposium, 29 June 2010, Bergen (Norway) GOCE data analysis: the space-wise approach and the space-wise approach and the first space-wise.
Astronomical Institute University of Bern 1 Astronomical Institute, University of Bern, Switzerland * now at PosiTim, Germany 5th International GOCE User.
1 UPWARD CONTINUATION OF DOME-C AIRBORNE GRAVITY AND COMPARISON TO GOCE GRADIENTS AT ORBIT ALTITUDE IN ANTARCTICA Hasan Yildiz (1), Rene Forsberg (2),
B. Amjadiparvar(1), E. Rangelova(1), M. G. Sideris(1) , C. Gerlach(2)
An overview of spectral methods for the optimal processing of satellite altimetry and other data I.N. Tziavos1, M.G. Sideris2, G.S. Vergos1, V.N. Grigoriadis1,
Dynamic Planet 2005 Cairns, Australia August 2005
Per Knudsen & Ole Andersen, DTU Space, Jerome Benveniste, ESA/ESRIN,
Estimating the cost to Helmert heights of a lateral approximation of the topographical density distribution Robert Kingdon1, Artu Ellmann1, Petr Vanicek1,
Ionospheric Effect on the GNSS Radio Occultation Climate Data Record
D. Rieser *, R. Pail, A. I. Sharov
Martin Pitoňák1, Michal Šprlák2 and Pavel Novák1
Daniel Rieser, Christian Pock, Torsten Mayer-Guerr
Geoid Enhancement in the Gulf Coast Region
Advances and Best Practices in Airborne Gravimetry from the U. S
Presentation transcript:

GOCE/GRACE GGM evaluation over Greece with GPS/Leveling and gravity data G.S. Vergos, V.D. Grigoriadis, I.N. Tziavos, D.A. Natsiopoulos, E.A. Tzanou

Availability of several GOCE/GRACE GGMs for the Earth’s potential OUTLINE

o TIM (R1, R2, R3, R4, R5) o DIR (R1, R2, R3, R4, R5) o GOCO (01s, 02s, 03s) o EIGEN*s/c (51c, 6s/c, 6s/c2, 6c3stat) o ITG-GOCE02s, GOGRA02s/04s, JYY_GOCE02s/04s OUTLINE

Availability of several GOCE/GRACE GGMs for the Earth’s potential o TIM (R1, R2, R3, R4, R5) o DIR (R1, R2, R3, R4, R5) o GOCO (01s, 02s, 03s) o EIGEN*s/c (51c, 6s/c, 6s/c2, 6c3stat) o ITG-GOCE02s, GOGRA02s/04s, JYY_GOCE02s/04s Validation of the GOCE/GRACE GGMs and Wo determination OUTLINE

OUTLINE Availability of several GOCE/GRACE GGMs for the Earth’s potential o TIM (R1, R2, R3, R4, R5) o DIR (R1, R2, R3, R4, R5) o GOCO (01s, 02s, 03s) o EIGEN*s/c (51c, 6s/c, 6s/c2, 6c3stat) o ITG-GOCE02s, GOGRA02s/04s, JYY_GOCE02s/04s Validation of the GOCE/GRACE GGMs and Wo determination o External validation over Greece with collocated GPS/Leveling BMs and gravity anomaly data

METHODOLOGY Combined GGM differences to n max =216,000 evaluation of GOCE/GRACE GGMs every 1 degree from a 3  DTM over Greece

METHODOLOGY Combined GGM differences to n max =216,000 evaluation of GOCE/GRACE GGMs every 1 degree from a 3  DTM over Greece o Mean Tide to Tide Free conversion for orthometric heights o GGM Zero Tide to Tide Free when necessary o All computations in GRS80 o N o relative to the IERS W o of m 2 /s 2

METHODOLOGY Combined GGM differences to n max =216,000 evaluation of GOCE/GRACE GGMs every 1 degree from a 3  DTM over Greece o Free-air gravity anomalies o GRS80/IGSN71 o Clean database after LSC-based blunder detection and removal

LOCAL DATA 1542 collocated GPS/Leveling observations

LOCAL DATA free-air gravity anomalies

GOCE GGM VALIDATION

GGMd/orangemeanstd EGM ±0.139 DIR-R5 169+EGM ±0.123 TIM-R5 166+EGM ±0.121 GOCO03s 167+EGM ±0.122 ITG-GOCE02s 166+EGM ±0.122 GOGRA04s 167+EGM ±0.122 JYY-GOCE04s 167+EGM ±0.122 Geoid height differences between GOCE/GRACE GGMs and GPS/Lev BMs. Unit [m]

GOCE GGM VALIDATION TIM-R5, DIR-R5 and EGM2008 Geoid height differences at the GPS/Lev BMs

GOCE GGM VALIDATION

GGMEGM2008TIM-R5DIR-R5N grav 0-10 km km km km km km km km km km >100 km Relative accuracy of geoid height differences. Unit [ppm]

GOCE GGM VALIDATION

GGMd/orangemeanstd EGM ±5.32 DIR-R5 214+EGM ±4.89 TIM-R5 212+EGM ±4.89 GOCO03s 193+EGM ±4.89 ITG-GOCE02s 193+EGM ±4.89 GOGRA04s 194+EGM ±4.89 JYY-GOCE04s 194+EGM ±4.89 Gravity anomaly differences between GOCE/GRACE GGMs and local data. Unit [mGal]

GOCE GGM VALIDATION TIM-R5, DIR-R5 and EGM2008 gravity anomaly differences with the local data

GOCE GGM VALIDATION Radially averaged PSD vs spatial frequency

Basic physical model (Helmert ortho heights): LS estimate of LVD’s zero-height level ‘weights’

Un-weighted LS estimate & combined GOCE/GRACE GGMs o EGM2008 (2190) o DIR-R5 (169)+EGM08 o TIM-R5 (166)+EGM08 o GOGRA04s (167)+EGM08

Un-weighted LS estimate & combined GOCE/GRACE GGMs o EGM2008 (2190) o DIR-R5 (169)+EGM08 o TIM-R5 (166)+EGM08 o GOGRA04s (167)+EGM08

Un-weighted LS estimate & combined GOCE/GRACE GGMs o DIR-R5 (169)+EGM08 o TIM-R5 (166)+EGM08 o GOGRA04s (167)+EGM08 Great consistency for the GOCE/GRACE GGMs in

o GOCE/GRACE GGM validation over Greece with GPS/Leveling and gravity data, with a remark on Wo determination CONCLUSIONS

o GOCE/GRACE GGM validation over Greece with GPS/Leveling and gravity data, with a remark on Wo determination o The latest releases are better than EGM2008 as much as 1.8 cm (1σ), reducing also the mean by 3 cm and the range by 7 cm CONCLUSIONS

o GOCE/GRACE GGM validation over Greece with GPS/Leveling and gravity data, with a remark on Wo determination o The latest releases are better than EGM2008 as much as 1.8 cm (1σ), reducing also the mean by 3 cm and the range by 7 cm o DIR-R5 and TIM-R5 are better up to d/o 230, with significant improvements in the spectral range between d/o CONCLUSIONS

o GOCE/GRACE GGM validation over Greece with GPS/Leveling and gravity data, with a remark on Wo determination o The latest releases are better than EGM2008 as much as 1.8 cm (1σ), reducing also the mean by 3 cm and the range by 7 cm o DIR-R5 and TIM-R5 are better up to d/o 230, with significant improvements in the spectral range between d/o o In terms of the gravity anomalies they are better than EGM2008 by 0.5 mGal (1σ), reducing also the mean by 0.2 mGal and the range by 7 mGal CONCLUSIONS

o GOCE/GRACE GGM validation over Greece with GPS/Leveling and gravity data, with a remark on Wo determination o The latest releases are better than EGM2008 as much as 1.8 cm (1σ), reducing also the mean by 3 cm and the range by 7 cm o DIR-R5 and TIM-R5 are better up to d/o 230, with significant improvements in the spectral range between d/o o In terms of the gravity anomalies they are better than EGM2008 by 0.5 mGal (1σ), reducing also the mean by 0.2 mGal and the range by 7 mGal o from GOCE GGMs is very robust with between the various GGMs at cm CONCLUSIONS

Funded by the European Space Agency (ESA) Scientific Experiment Development Program (PRODEX) within the General Secretariat for Research & Technology (GSRT) invitation to the Greek scientific community in response to the 1st PRODEX Programme Call for Greece. GOCESeaComb Project ACKNOWLEDGEMENT