GOCE Research in Germany: From Sensor Analysis to Earth System Science
|
|
- Frederick Lawrence
- 6 years ago
- Views:
Transcription
1 GOCE Research in Germany: From Sensor Analysis to Earth System Science Reiner Rummel, Jakob Flury and Thomas Gruber Institut für Astronomische und Physikalische Geodäsie Technische Universität München 3. International GOCE User Workshop ESA-ESRIN Frascati Rome November 2006
2 Contents: GOCE Science Objectives and Research Challenges GOCE-GRAND-2 second phase GOCE related research activities in Germany GOCE project office
3 GOCE Mission Objectives Acronym: Gravity and Steady-State Ocean Circulation Explorer Mission Objectives: Geoid std.dev. 1cm Gravity (anomalies) std. dev. 1mGal Spatial resolution: 100 km (Lmax= 200) Launch: September 2007
4 applications of static gravity field solid earth ocean ice geodesy sea level gravity anomalies seismic tomograpy geoid gravity anomalies geoid ocean altimetry ice topography positioning (GPS) tide gauges altimetry topography deformations laboratory mean ocean circulation bedrock topography levelled heights post glacial rebound unified height system mean ocean circulation anomalous density structure constraints on mass & heat transport mass balance of ice sheets gravity anomalies ice mass balance orbits unified height systems INS orbits
5 science requirements SOLID EARTH APPLICATION ACCURACY SPATIAL RESOLUTION Geoid (cm) Gravity (mgal) half wavelength - D (km) lithosphere / upper mantle density continental lithosphere sedimentary basins rifts tectonic motions seismic hazards ocean lithosphere / asthenosphere short scale OCEANOGRAPHY basin scale ~ rock basement ICE SHEETS ice vertical movements levelling by GPS unified height systems GEODESY INS ~ orbits ~ Many of the above applications, SEA LEVEL CHANGE with their specific requirements, are relevant to studies of sea level change Gravity Field and Steady-State Ocean Circulation Mission ESA, SP-1233 (1), 1999, p.80
6 GOCE and steady-state ocean circulation requires two surfaces and therefore two satellite sensor systems to be globally consistent at the cm-level satellite altimetry GOCE
7 GRACE: maximum precision (geoid <!m) GOCE: maximum resolution (s= 80 km)
8 error Power Density Spectrum for {zz}-component noise filter MBW
9 GOCE High Level Processing Facility GOCE Standards Doc. No.: GO-TN-HPF-GS-00xx Issue: 1 Revision: 0 Date: October / 2006 Prepared by: The European GOCE Gravity Consortium EGG-C
10 GOCE gravity model: global spherical harmonic series terrestrial gravity data: regional pointwise, block averages
11 Calibration and Validation GOCE CAL/VAL data sets spatial represention global regional local spatial represention global regional local long wavelength short spectral representation long wavelength short spectral representation
12 Calibration and Validation GOCE CAL/VAL data sets spatial represention global regional local spatial represention global regional local long wavelength short spectral representation long wavelength short spectral representation
13 Regional Validation and Combination Experiment Observations of vertical deflections (courtesy IFE Hannover)
14
15 A Selection of Research Challenges: take into account pecularities of sensor system get lowest harmonics right get altimetry and GOCE into one consistent reference system ensure definition and implementation of adequate standards revisit theory of geodetic boundary value problem work on optimal combination of geopotential models and on their combination with terrestiral data develop appropriate validation methods and experiments
16 GOCE related activities in Germany Participation in ESA GOCE processing (ESA contracts): PDS, HPF, CMF, CAL/VAL, GUTs, studies Connection to GT Theme 2 Observation of Earth System from Space Participation in DFG Priority Programme 1257 Mass Transport and Mass Distribution in System Earth Involvement in IAG Pilot Project: GGOS (will belong to IGOS and GEO)
17 GOCE-Grand 2 Financed by German Research Ministry through GeoTechnologyProgramme its Theme 2 Observation of Earth System from Space U Bonn U Hamburg U Hannover BKG Frankfurt U Stuttgart GFZ Potsdam TU München
18 GOCE Gravity Field Processing Adaptive Refinements in GOCE Gravity Field Modelling and Implementation of the Operational Software pcgma GOCE Gravity Field Modelling Further Methodology Investigation on Alternative Estimation Procedures SST and SGG Gravity Analysis Realization of the Actual GOCE Sensor Concept The Polar Gap Problem Solution Strategies and Influence on the GOCE/GRACE Combination Solution Regionally Adapted Global Gravity Field Determination by SGG and SST Data Results of GOCE-GRAND I Combined Gravity Modelling Calibration and Validation High Resolution Global Combination Solutions Quality Assessment of GOCE Gradients Gravity Field Validation with Terrestrial Geoid and Gravity Anomalies Regional Validation and Combination Experiment Gravity Field Validation Using Ocean Data and Ocean Dynamics Integral Motion and its Role for Consistency Validation of Force Functions and Orbits Other Geotechnology II Projects: Optimized GRACE Level-1 and Level-2 Products More Precise and Faster Gravity Field Products (CHAMP,GRACE) IAPG ITG GFZ GIS BKG & IFE IFE IFM
19
20 GOCE-GRAND-2 Working Groups GOCE Standards System Transformations; Geometrical Models; Dynamical Models. GOCE and Surface Data GOCE and Applications Combination & Validation; Corrections to be applied; Data Weighting; Aliasing & Filtering Techniques. Identification of Needs; Reference Potential W 0 ; Derived Gravity Field Quantities on Ellipsoid or Earth Surface.
21 Proposal to German Research Foundation (DFG) coordinator: : K-H Ilk granted: : 2005
22 Mass Transport in the Earth System gravity field missions ocean transport (mass/heat) ocean surface circulation (altimetry - geoid) deep ocean circulation (bottom pressure) sea level mass vs. volume change (altimetry / gravity) atmosphere CHAMP GRACE GOCE altimetry missions Envisat CryoSat Jason-1 ICESat complementary remote sensing TerraSAR, topography, sea surface temperature, winds, salinity, soil moisture (SMOS) etc. from satellite sensor data to mass signals combination of geometry and gravity in space and time in one reference system, data preparation for model assimilation, terrestrial/ airborne data, separation of signal effects, complementary data hydrological cycle continental water budget, closure of global and regional water balance, water storage variation, trends and climate change ice mass balance and sea level ice surface: height change, velocities, mass budget of ice sheets, bottom topography, sea level rise from melting, dynamic ice models, sea ice: coverage, thickness dynamics of mantle and crust mantle dynamics and geoid signal, geoid time variation from glacial isostatic adjustment, plumes, slabs, gravity signal of crustal and lithosphere structure
23 IAG Pilot Project: Global Geodetic Observing System
24 Coordination of GOCE activities by GOCE project office financed by DLR (German Aerospace Center) responsible for: activation of user community coordination of GOCE activities public relations contact with industry and funding agencies
25
26
27
28
29 GGOS: Geodesy and System Earth Gravity field missions and variations in l.o.d. CHAMP GRACE GOCE Altimetry missions Geometry 3D+T: shape of Envisat land surfaces Jason-1 ice shields oceans ICESat Earth Rotation Precession/ nutation polar motion CryoSat Oceanic transport ocean circulation (quasi-static and time v ariation), mass and heat transport, eddies, sea lev el: mass and v olume change From satellite space sensor and terrestrial data to Geodetic Earth data system to Earth consistent System combination Parameters of Space geodetic data, reference sy stems, Consistent models data preparation for model assimilation, Separation of effects regional representation, filtering, error models, Data separation processing of signal Data components, combination mass balance, filtering complementary data Continental hydrology Continental w ater budget, closure of w ater balance (global, regional) w ater storage v ariation, trends and climate change Atmosphere and Ionosphere Composition of ionoshere Atmospheric sounding (T,H, P) Tropospheric models Mass balance atmosphere Ice mass balance and sea level ice surface: height change, v elocities, mass budget of ice sheets, sea lev el rise from melting, dy namic ice models, sea ice: cov erage, thickness Complementary remote sensing TerraSAR (2005) Gravity/ Geoid Topography 3D+T: detailed Sea temperature geoid Wind, Salinity, and gravity anomaly field Soil moisture, SMOS, etc Dynamics of mantle and crust mantle dy namics and geoid signal, time v ariation from global isostatic adjustment, plumes, slabs, grav ity signal of crustal and lithospherie structures Earth Deep Interior Core-Mantle Coupling Mantle anelasticity ICB flattening (after Ilk KH et al., 2005) From Earth to Planets Moments of Inertia Fluid core? Isostatic (un)equilibrium Shape and gravity field
30 GOCE ground segment level 0 GOCE Cal/Val Team CMF PDS HPF GOCE-GRAND-2 GOCE User Toolbox ILRS IGS ECMWF level 1a/1b level 2 GOCE Application Studies GOCE Users level 3
31 GOCE ground segment level 0 CMF PDS ILRS IGS level 1a/1b ECMWF GOCE Cal/Val Team HPF level 2 GOCE User Toolbox GOCE Application Studies GOCE Users level 3
32 Users (Science and Application) solid Earth physics physical oceanography and climate research geodesy sea level research
33 Sensor Measurements Gravity gradients " xx, " yy, " zz in instrument system and inside MBW (measurement bandwidth) 3-axis gravity gradiometer Angular accelerations (highly accurate around y-axis, less accurate around x, z axes) Common mode accelerations Star sensors GPS receiver Drag control with 2 ion thrusters Angular control with magnetic torquers Orbit altitude maintenance Internal calibration of gradiometer (and quadratic factors) High rate and high precision inertial orientation Orbit trajectory with cm-precision Based on common mode accelerations from gradiometer data Based on angular rates from star sensors and gradiometer Based on GPS orbit Random shaking with cold gas thrusters (and random pulses)
34 Status of GOCE development newly developed GPS receiver laser tracking
35 Status of GOCE development Attitude and Drag-free control
36 accelerometers, 1-axis gradiometer 3-axis gradiometer Status of GOCE development
37
38
39 GRACE: maximum precision (geoid <!m) GOCE: maximum resolution (s= 80 km)
40
41 Klassische Bilanzgleichungen Impulsbilanz Drehimpulsbilanz Energiebilanz MR&! K = 0 MR&! K = 0 MR&! K = 0 vektorielle Multiplikation mit R skalare. Multiplikation mit R MR " R&! R " K = 0 M& R " R&! K " R& = 0 Zeitintegration Zeitintegration Zeitintegration t M R &! " Kdt = P t 0 0 t M R! R& " # R! Kdt = L t MR & 2 t " # K! R& dt = E t 0 Impuls = Anfangsimpuls + integrierte Kraft Drehimpuls = Anfangsdrehimpuls + integriertes Drehmoment Energie = kinetische Energie - integrierte Arbeit
42
43
44
45
46 Mass Transport in the Earth System gravity field missions ocean transport (mass/heat) ocean surface circulation (altimetry - geoid) deep ocean circulation (bottom pressure) sea level mass vs. volume change (altimetry / gravity) atmosphere CHAMP GRACE GOCE altimetry missions Envisat CryoSat Jason-1 ICESat complementary remote sensing TerraSAR, topography, sea surface temperature, winds, salinity, soil moisture (SMOS) etc. from satellite sensor data to mass signals combination of geometry and gravity in space and time in one reference system, data preparation for model assimilation, terrestrial/ airborne data, separation of signal effects, complementary data hydrological cycle continental water budget, closure of global and regional water balance, water storage variation, trends and climate change ice mass balance and sea level ice surface: height change, velocities, mass budget of ice sheets, bottom topography, sea level rise from melting, dynamic ice models, sea ice: coverage, thickness dynamics of mantle and crust mantle dynamics and geoid signal, geoid time variation from glacial isostatic adjustment, plumes, slabs, gravity signal of crustal and lithosphere structure
47
48
49 GOCE design elements: GOCE design elements: 3-axis gravity gradiometer GPS (orbit + low harmonics) star sensor (orientation in space) active attitude control (magnetic torquers) active drag compensation (along-track) stable and rigid material x now: magnetic torquers
50 Instrument Concept translational forces angular forces GPS/GLONASS SST -hl star sensors * * A B GRAVITY GRADIOMETER measures: gravity gradients angular accelerations common mode acc. drag control angular control
51 unified height systems sea surface topography ocean mass transport sea level changes glacial isostatic adjustment earthquakes slow component bathymetry continental lithosphere
52 GOCE Mission Characteristics: orbit altitude: 250 km inclination: one orbit cycle:! 30 to 40 days mission duration: gradiometer: orbit: launcher: 20 months 3 me/"hz 1-3 cm Rockot class
53
54 Electrostatic Gravity Gradiometer
55 GOCE ground segment CMF PDS HPF ILRS IGS ECMWF
56 Auslenkung der tatsächlichen Meeresoberfläche (gemessen mit Satellitenaltimetie) bezüglich der Niveaufläche auf Meeresniveau, dem Geoid (berechnet aus Schwerefeldmodell) = dynamische Meerestopographie
GOCE-GRAND-2 Project Overview and Status of the GOCE Mission
GOCE-GRAND-2 Project Overview and Status of the GOCE Mission Reiner Rummel, Thomas Gruber & Jakob Flury Institut für Astronomische und Physikalische Geodäsie Technische Universität München Geotechnologien
More informationMASS TRANSPORT AND MASS DISTRIBUTION IN THE EARTH SYSTEM
MASS TRANSPORT AND MASS DISTRIBUTION IN THE EARTH SYSTEM Jakob Flury (1) and Reiner Rummel (1) (1) German GOCE Project Bureau Institute for Astronomical and Physical Geodesy Technische Universität München,
More informationGOCE. Gravity and steady-state Ocean Circulation Explorer
GOCE Gravity and steady-state Ocean Circulation Explorer Reiner Rummel Astronomical and Physical Geodesy Technische Universität München rummel@bv.tum.de ESA Earth Observation Summerschool ESRIN/Frascati
More informationA Mission to Planet Mars Gravity Field Determination
A Mission to Planet Mars Gravity Field Determination Department for Theoretical Geodesy Graz University of Technology and Space Research Institute Austrian Academy of Sciences Gravity field CHAMP GRACE
More informationFuture Satellite Gravity Missions
Towards a Roadmap for Future Satellite Gravity Missions, Graz, September 2009 Future Satellite Gravity Missions Activities in Germany Jürgen Müller 1, Nico Sneeuw 2, Frank Flechtner 3 1 Institut für Erdmessung,
More informationGRACE impact in geodesy and geophysics. R. Biancale (GRGS-CNES Toulouse), M. Diament (IPG Paris)
GRACE impact in geodesy and geophysics R. Biancale (GRGS-CNES Toulouse), M. Diament (IPG Paris) Improvement of gravity models Since 2002 the GRACE mission has changed some goals in geodesy. It has become
More informationA Unique Reference Frame: Basis of the Global Geodetic Observing System (GGOS) for Geodynamics and Global Change
SRTM (InSAR) A Unique Reference Frame: Basis of the Global Geodetic Observing System (GGOS) for Geodynamics and Global Change Hermann Drewes President IAG Commission 1 Reference Frames Deutsches Geodätisches
More informationGG S. Internal Vision of GGOS. Markus Rothacher. GFZ Potsdam
Internal Vision of GGOS Markus Rothacher GFZ Potsdam GGOS Retreat DGFI in Munich February 15-16, 2006 Contents Motivation Four Levels of Products of the IAG Services: First Level: Raw Data Collection Second
More informationThe Global Geodetic Observing System (GGOS) of the International Association of Geodesy, IAG
The Global Geodetic Observing System (GGOS) of the International Association of Geodesy, IAG Hans-Peter Plag (1), Markus Rothacher (2), Richard Gross (3), Srinivas Bettadpur (4) (1) Nevada Bureau of Mines
More informationThe Earth Explorer Missions - Current Status
EOQ N 66 July 2000 meteorology earthnet remote sensing solid earth future programmes Earth Observation Quarterly The Earth Explorer Missions - Current Status G. Mégie (1) and C.J. Readings (2) (1) Institut
More informationTHE STATUS OF THE GOCE HIGH-LEVEL PROCESSING FACILITY
Supporting GS Elements Core GS Elements GOCE Mission Management 199 THE STATUS OF THE GOCE HIGH-LEVEL PROCESSING FACILITY Radboud Koop 1, Thomas Gruber 2, Reiner Rummel 2 1 SRON Netherlands Institute for
More informationESA s supporting Activities Related to Mass Transport in the Earth System
ESA s supporting Activities Related to Mass Transport in the Earth System Roger Haagmans Mission Science Division European Space Agency Swarm mission: 3D-Mantle Conductivity (A. Jackson ETH Zürich, DNSC,
More informationGeodetic Observing Systems: tools in observing the Glacial Isostatic Adjustment. Markku Poutanen Finnish Geodetic Institute
Geodetic Observing Systems: tools in observing the Glacial Isostatic Adjustment Markku Poutanen Finnish Geodetic Institute Glacial Isostatic Adjustment Land uplift is just one consequence of the physical
More information1
Daniel.Schuetze@aei.mpg.de 1 Satellite gravimetry Mapping the global gravity field Static and dynamic components Many applications in geosciences Techniques Orbit determination and tracking Satellite-to-satellite
More informationActive microwave systems (2) Satellite Altimetry * the movie * applications
Remote Sensing: John Wilkin wilkin@marine.rutgers.edu IMCS Building Room 211C 732-932-6555 ext 251 Active microwave systems (2) Satellite Altimetry * the movie * applications Altimeters (nadir pointing
More informationRoadmap Towards Future Satellite Gravity Missions in Support of Monitoring of Mass Redistribution, Global Change, and Natural Hazards
Roadmap Towards Future Satellite Gravity Missions in Support of Monitoring of Mass Redistribution, Global Change, and Natural Hazards STRATEGIC TARGET A multi-decade, continuous series of space-based observations
More informationGOCE QUICK-LOOK GRAVITY FIELD ANALYSIS: TREATMENT OF GRAVITY GRADIENTS DEFINED IN THE GRADIOMETER REFERENCE FRAME
GOCE QUICK-LOOK GRAVITY FIELD ANALYSIS: TREATMENT OF GRAVITY GRADIENTS DEFINED IN THE GRADIOMETER REFERENCE FRAME Roland Pail Institute of Navigation and Satellite Geodesy, Graz University of Technology,
More informationGGOS Bureau for Standards and Conventions
GGOS D. Angermann (1), T. Gruber (2), J. Bouman (1), M. Gerstl (1), R. Heinkelmann (1), U. Hugentobler (2), L. Sánchez (1), P. Steigenberger (2) (1) Deutsches Geodätisches Forschungsinstitut (DGFI), München
More informationEarth system. space. planets. atmosphere. ice sheets. ocean. biosphere, technosphere. solid Earth. gravitation on. orbit, spin, tides
third lecture Three Lectures: One ESA explorer mission GOCE: earth gravity from space Two Signal Processing on a sphere Three Gravity and earth sciences Earth system space sun moon planets gravitation
More informationNew satellite mission for improving the Terrestrial Reference Frame: means and impacts
Fourth Swarm science meeting and geodetic missions workshop ESA, 20-24 March 2017, Banff, Alberta, Canada New satellite mission for improving the Terrestrial Reference Frame: means and impacts Richard
More informationThe GOCE User Toolbox
The GOCE User Toolbox Jérôme Benveniste - ESA Earth Observation Science and Applications Department Per Knudsen - Danish National Space Center and the GUT TEAM 37th COSPAR Scientific Assembly 2008, Montreal
More informationGG S Global Geodetic Observing System (GGOS): Status and Future. Markus Rothacher, Ruth Neilan, Hans-Peter Plag
2020 Global Geodetic Observing System (GGOS): Status and Future Markus Rothacher, Ruth Neilan, Hans-Peter Plag GeoForschungsZentrum Potsdam (GFZ) Jet Propulsion Laboratory (JPL) University of Nevada, Reno
More informationHigh-Harmonic Geoid Signatures due to Glacial Isostatic Adjustment, Subduction and Seismic Deformation
High-Harmonic Geoid Signatures due to Glacial Isostatic Adjustment, Subduction and Seismic Deformation L.L.A. Vermeersen (1), H. Schotman (1), M.-W. Jansen (1), R. Riva (1) and R. Sabadini (2) (1) DEOS,
More informationGeophysik mittels Satellitenbeobachtungen - Von der Struktur zur dynamischen Betrachtung der Erde
Geophysik mittels Satellitenbeobachtungen - Von der Struktur zur dynamischen Betrachtung der Erde Jörg Ebbing Institut für Geowissenschaften Christian-Albrechts-Universität zu Kiel 102. Sitzung des FKPE
More informationThe GOCE Geoid in Support to Sea Level Analysis
The GOCE Geoid in Support to Sea Level Analysis The geoid is a very useful quantity for oceanographers Thomas Gruber Astronomical & Physical Geodesy (IAPG) Technische Universität München 1. Characteristics
More informationHydrological Mass Variations due to Extreme Weather Conditions in Central Europe from Regional GRACE 4D Expansions
Hydrological Mass Variations due to Extreme Weather Conditions in Central Europe from Regional GRACE 4D Expansions Florian Seitz 1, Michael Schmidt 2, C.K. Shum 3, Yiqun Chen 3 1 Earth Oriented Space Science
More informationEarth-Oriented Space Research at TU-Delft
Earth-Oriented Space Research at TU-Delft The contribution of DEOS to the South-East Asia: Mastering Environmental Research with Geodetic Space Techniques (SEAMERGES) project Kick-off meeting, Chulalongkorn
More informationConstraints on Shallow Low-Viscosity Earth Layers from Future GOCE Data
Constraints on Shallow Low-Viscosity Earth Layers from Future GOCE Data Hugo Schotman 1,2, Bert Vermeersen 2, Pieter Visser 2 1 2 3 rd International GOCE User Workshop, ESA Esrin, 7 November 2006 glacial-isostatic
More informationDependences in the pillar Earth s gravity field of
Reports on Geodesy, vol. 92, no. 1, 2012 Dependences in the pillar Earth s gravity field of GGOS - description using UML notation Małgorzata Paśnicka 1, Karolina Szafranek 2, Agnieszka Zwirowicz Rutkowska
More informationArctic Ocean Mean Sea Surface, Geoid and Gravity from Surface Data, Icesat and GRACE a reference for Cryosat sea-ice mapping
Arctic Ocean Mean Sea Surface, Geoid and Gravity from Surface Data, Icesat and GRACE a reference for Cryosat sea-ice mapping R. Forsberg and H. Skourup, Geodynamics Dept., DNSC rf@spacecenter.dk Arctic
More informationGeophysical Correction Application in Level 2 CryoSat Data Products
ESRIN-EOP-GQ / IDEAS IDEAS-VEG-IPF-MEM-1288 Version 2.0 29 July 2014 Geophysical Correction Application in Level 2 CryoSat Data Products TABLE OF CONTENTS 1 INTRODUCTION... 3 1.1 Purpose and Scope... 3
More informationThe Earth s time-variable gravity field observed by GOCE
The Earth s time-variable gravity field observed by GOCE GOCE+ Time-Variations, part of STSE (Theme 4, Innovative Feasibility Studies) J. Bouman, M. Fuchs, C. Haberkorn, V. Lieb, M. Schmidt T. Broerse,
More informationEVALUATING GOCE DATA NEAR A MID-OCEAN RIDGE AND POSSIBLE APPLICATION TO CRUSTAL STRUCTURE IN SCANDINAVIA
EVALUATING GOCE DATA NEAR A MID-OCEAN RIDGE AND POSSIBLE APPLICATION TO CRUSTAL STRUCTURE IN SCANDINAVIA Wouter van der Wal (1), Lin Wang (2,1), Pieter Visser (1), Nico Sneeuw (2), Bert Vermeersen (1)
More informationSatellite Geodesy and Navigation Present and Future
Satellite Geodesy and Navigation Present and Future Drazen Svehla Institute of Astronomical and Physical Geodesy Technical University of Munich, Germany Content Clocks for navigation Relativistic geodesy
More informationGOCE DATA PRODUCT VERIFICATION IN THE MEDITERRANEAN SEA
GOCE DATA PRODUCT VERIFICATION IN THE MEDITERRANEAN SEA Juan Jose Martinez Benjamin 1, Yuchan Yi 2, Chungyen Kuo 2, Alexander Braun 3, 2, Yiqun Chen 2, Shin-Chan Han 2, C.K. Shum 2, 3 1 Universitat Politecnica
More informationGlobal & National Geodesy, GNSS Surveying & CORS Infrastructure
Global & National Geodesy, GNSS Surveying & CORS Infrastructure Chris Rizos School of Surveying & Spatial Information Systems University of New South Wales, Sydney, Australia President-elect, International
More informationFundamental Station Wettzell - geodetic observatory -
Fundamental Station Wettzell - geodetic observatory - Wolfgang Schlüter Bundesamt für Kartographie und Geodäsie, Fundamental Station Wettzell Germany Radiometer Workshop, Wettzell, 10.10.06 Evolvement
More informationEarth gravity field recovery using GPS, GLONASS, and SLR satellites
13-01-08 Earth gravity field recovery using GPS, GLONASS, and SLR satellites Krzysztof Sośnica (1), Adrian Jäggi (1), Daniela Thaller (2), Ulrich Meyer (1), Christian Baumann (1), Rolf Dach (1), Gerhard
More informationInterferometric Synthetic Aperture Radar (InSAR) and GGOS. Andrea Donnellan NASA/JPL February 21, 2007
Interferometric Synthetic Aperture Radar (InSAR) and GGOS Andrea Donnellan NASA/JPL February 21, 2007 Sources for Science Objectives Fourth component of EarthScope Involvement: NSF, NASA, USGS, Universities
More informationGeodesy Part of the ACES Mission: GALILEO on Board the International Space Station
Geodesy Part of the ACES Mission: GALILEO on Board the International Space Station 1 Svehla D, 2 Rothacher M, 3 Salomon C, 2 Wickert J, 2 Helm A, 2 Beyerle, G, 4 Ziebart M, 5 Dow J 1 Institute of Astronomical
More informationThe Global Geodetic Observing System (GGOS) of the International Association of Geodesy (IAG)
The Global Geodetic Observing System (GGOS) of the International Association of Geodesy (IAG) Hermann Drewes Representative of the International Union of Geodesy and Geophysics (IUGG) to the Cartographic
More informationCalibration/validation of GOCE data by terrestrial torsion balance observations
Calibration/validation of GOCE data by terrestrial torsion balance observations Gy. Tóth 1, J. Ádám 1, L. Földváry 1,4, I.N. Tziavos 2, H. Denker 3 1 Department of Geodesy and Surveying, Budapest University
More informationOverview and Status of ESA Earth Observation Programmes
Overview and Status of ESA Earth Observation Programmes Maurice Borgeaud, ESA Head of the Science, Applications and Future Technologies Department Directorate of Earth Observation Programmes ADM-Aeolus
More informationESA training. Gravity, magnetics and gradients for mapping and modelling. Jörg Ebbing. Department of Geosciences Kiel University
ESA training Gravity, magnetics and gradients for mapping and modelling Jörg Ebbing Department of Geosciences Kiel University Contributions from: Eldar Baykiev (Trondheim), Des Fitzgerald (Melbourne),
More informationStrategy for the Realization of the International Height Reference System (IHRS)
Deutsches Geodätisches Forschungsinstitut (DGFI-TUM) Technische Universität München Strategy for the Realization of the International Height Reference System (IHRS) Laura Sánchez 1, Johannes Ihde 2, Roland
More informationPaper Reprint: Gruber Th., Rummel R., Koop R.: The GOCE High Level Processing Facility
Paper Reprint: Gruber Th., Rummel R., Koop R.: The GOCE High Level Processing Facility 42 43 44 Supporting GS Elements Core GS Elements GOCE Mission Management The GOCE High Level Processing Facility Th.
More informationPROCESSES CONTRIBUTING TO THE GLOBAL SEA LEVEL CHANGE
Second Split Workshop in Atmospheric Physics and Oceanography PROCESSES CONTRIBUTING TO THE GLOBAL SEA LEVEL CHANGE Student: Maristella Berta Mentor: Prof. Stjepan Marcelja Split, 24 May 2010 INTRODUCTION
More informationEarth gravity field recovery using GPS, GLONASS, and SLR satellites
Earth gravity field recovery using GPS, GLONASS, and SLR satellites Krzysztof Sośnica (1), Adrian Jäggi (1), Daniela Thaller (2), Ulrich Meyer (1), Gerhard Beutler (1), Rolf Dach (1) (1) Astronomical Institute,
More informationHigh resolution geoid from altimetry & bathymetry: requirements for a future mission
High resolution geoid from altimetry & bathymetry: requirements for a future mission The GRAL team: J-Y Royer 1,2, M-F Lalancette 3, G Louis 1,2, M Maia 1,2, D Rouxel 3 & L Géli 4 Project funded by 1 2
More informationGGOS The Global Geodetic Observing System of the International Association of Geodesy
GGOS The Global Geodetic Observing System of the International Association of Geodesy Presented at the FIG Working Week 2017, May 29 - June 2, 2017 in Helsinki, Finland Hansjörg Kutterer BKG, Germany Content
More informationStatus of the European Gravimetric Quasigeoid
Status of the European Gravimetric Quasigeoid C. Voigt, H. Denker {voigt,denker}@ife.uni-hannover.de 1 Introduction 2 The European Gravity and Geoid Project (EGGP) 3 Data Sets 4 Quasigeoid Computation
More informationGeoid and MDT of the Arctic Ocean
Geoid and MDT of the Arctic Ocean Rene Forsberg, Henriette Skourup Geodynamics Dept National Space Institute Techical University of Denmark rf@space.dtu.dk Outline: Determination of MDT from remote sensing
More informationCan we see evidence of post-glacial geoidal adjustment in the current slowing rate of rotation of the Earth?
Can we see evidence of post-glacial geoidal adjustment in the current slowing rate of rotation of the Earth? BARRETO L., FORTIN M.-A., IREDALE A. In this simple analysis, we compare the historical record
More informationLecture 2 Measurement Systems. GEOS 655 Tectonic Geodesy
Lecture 2 Measurement Systems GEOS 655 Tectonic Geodesy VLBI and SLR VLBI Very Long Baseline Interferometry SLR Satellite Laser Ranging Very Long Baseline Interferometry VLBI Geometric Delay δg S Baseline
More informationEvaluation of the Earth Gravity Model EGM2008 in Algeria
Evaluation of the Earth Gravity Model EGM2008 in Algeria BENAHMED DAHO S. A. National Centre of Space Techniques, Geodetic Laboratory - BP 13 Arzew - 31200 - Algeria. E-mail: d_benahmed@hotmaii.com /Fax:
More informationContributions of Geodesy to Oceanography
Contributions of Geodesy to Oceanography B. Tapley and J. Ries Center for Space Research, The University of Texas at Austin Dynamic Planet 2005 Cairns, Australia August 22-26, 2005 August 22-26, 2005 Dynam
More informationPhysics of the Earth
Physics of the Earth Fourth edition Frank D Stacey CSIRO Exploration and Mining, Brisbane, Australia Paul M Davis Department of Earth and Space Sciences, University of California, Los Angeles, USA CAMBRIDGE
More informationTwo-step data analysis for future satellite gravity field solutions: a simulation study
BOLLETTINO DI GEOFISICA TEORICA ED APPLICATA VOL. 40, N. 3-4, pp.6-66; SEP.-DEC. 999 Two-step data analysis for future satellite gravity field solutions: a simulation study J. KUSCHE, K. H. ILK and S.
More informationSea level change recent past, present, future
Sea level change recent past, present, future Anny Cazenave LEGOS-CNES Toulouse, France CCI_Colocation meeting, ESA/ESRIN Global mean sea level rise during the 20 th century (red : tide gauges; blue :
More informationON THE ACCURACY OF CURRENT MEAN SEA SURFACE MODELS FOR THE USE WITH GOCE DATA
ON THE ACCURACY OF CURRENT MEAN SEA SURFACE MODELS FOR THE USE WITH GOCE DATA Ole B. Andersen 1, M-.H., Rio 2 (1) DTU Space, Juliane Maries Vej 30, Copenhagen, Denmark (2) CLS, Ramon St Agne, France ABSTRACT
More information(1) , 6WHYH.HQ\RQ (2) *HRG\QDPLFV 'HSW 1DWLRQDO 6XUYH\ DQG &DGDVWUH 5HQWHPHVWHUYHM '. &RSHQKDJHQ 19 'HQPDUN UI#NPV GN
*5$9,7
More informationPresented at the FIG Congress 2018, May 6-11, 2018 in Istanbul, Turkey
Presented at the FIG Congress 2018, May 6-11, 2018 in Istanbul, Turkey A Geoid model of northern Chile from airborne and surface gravity Geographic Description of Chile. Total Surface: 2,006,096 Km 2.
More informationGOCE based Gravity Field Models Signal and Error Assessment
GOCE based Gravity Field Models Signal and Error Assessment Th. Gruber, M. Willberg Institute of Astronomical & Physical Geodesy (IAPG) Technical University Munich GOCE Reprocessing Status Expected Results
More informationFinal VRF grids Date: Aug 25, 2011 Author: R. Forsberg, G. Strykowski, O. Andersen
Final VRF grids Date: Aug 25, 2011 Author: R. Forsberg, G. Strykowski, O. Andersen www.blast-project.eu 1 Authors Name Organisation Rene Forsberg National Space Institute, DTU G. Strykowski National Space
More informationEl proyecto Sistema de Observación Geodésico Global [Global Geodetic Observing System (GGOS)] de la Asociación Internacional de Geodesia (IAG)
El proyecto Sistema de Observación Geodésico Global [Global Geodetic Observing System (GGOS)] de la Asociación Internacional de Geodesia (IAG) Hermann Drewes Deutsches Geodätisches Forschungsinstitut (DGFI)
More informationGRAVITY AND ISOSTASY
GRAVITY AND ISOSTASY Gravity The Geoid is the oblate spheroid -- the sea level surface over the entire Earth's surface Physically, the Geoid is an equipotential surface for gravity (i.e. the surface for
More informationGlobal Tectonics. Kearey, Philip. Table of Contents ISBN-13: Historical perspective. 2. The interior of the Earth.
Global Tectonics Kearey, Philip ISBN-13: 9781405107778 Table of Contents Preface. Acknowledgments. 1. Historical perspective. 1.1 Continental drift. 1.2 Sea floor spreading and the birth of plate tectonics.
More informationUpdate on the International Terrestrial Reference Frame (ITRF) : ITRF2014. Zuheir Altamimi
Update on the International Terrestrial Reference Frame (ITRF) : ITRF2014 Zuheir Altamimi Head of the IERS ITRF Product Center IAG Vice President IGN, France E-mail: zuheir.altamimi@ign.fr Key Points Introduction:
More informationHydrological balance in the large Russian river basins from GRACE satellites
Hydrological balance in the large Russian river basins from GRACE satellites Leonid Zotov 1,2, Natalya Frolova 3, E. Kyzyngasheva 1, C.K. Shum 4,5 1 NRU Higher School of Economics, Russia 2 SAI Moscow
More informationRelationships between mass redistribution, station position, geocenter, and Earth rotation: Results from IGS GNAAC analysis
Relationships between mass redistribution, station position, geocenter, and Earth rotation: Results from IGS GNAAC analysis Geoff Blewitt Mackay School of Earth Sciences and Engineering University of Nevada,
More informationRadio occultation at GFZ Potsdam: Current status and future prospects
Radio occultation at GFZ Potsdam: Current status and future prospects J. Wickert, T. Schmidt, G. Beyerle, S. Heise, R. Stosius GFZ German Research Centre for Geosciences, Potsdam, Germany The CHAMP, GRACE,
More information1 The satellite altimeter measurement
1 The satellite altimeter measurement In the ideal case, a satellite altimeter measurement is equal to the instantaneous distance between the satellite s geocenter and the ocean surface. However, an altimeter
More informationGravity Advanced Package (GAP) : a «null bias» electrostatic accelerometer for fundamental physics missions in the Solar System
Gravity Advanced Package (GAP) : a «null bias» electrostatic accelerometer for fundamental physics missions in the Solar System B. Christophe (ONERA, Châtillon, France) on behalf of the GAP Instrument
More informationB. Loomis, D. Wiese, R. S. Nerem (1) P. L. Bender (2) P. N. A. M. Visser (3)
Possible mission architectures for a GRACE follow-on mission including a study on upgraded instrumentation suites, and multiple satellite pairs in moderately-inclined orbits B. Loomis, D. Wiese, R. S.
More informationSatellite Gravimetry and its Application to Glaciology by Anthony Arendt for the UAF Summer School in Glaciology, June post-glacial rebound
Satellite Gravimetry and its Application to Glaciology by Anthony Arendt for the UAF Summer School in Glaciology, June 2010 1 Overview The Earth is a dynamic system in which components of the core, surface
More informationA Factor of 2-4 Improvement in Marine Gravity and Predicted Bathymetry from CryoSat, Jason-1, and Envisat Radar Altimetry: Arctic and Coastal Regions
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. A Factor of 2-4 Improvement in Marine Gravity and Predicted Bathymetry from CryoSat, Jason-1, and Envisat Radar Altimetry:
More informationGGOS, ECGN and NGOS: Global and regional geodetic observing systems. Markku Poutanen Finish Geodetic Institute
GGOS, ECGN and NGOS: Global and regional geodetic observing systems Markku Poutanen Finish Geodetic Institute Contents GGOS, ECGN, NGOS Why? How? Future? (geodesy) GGOS Structure GGOS Structure European
More informationGravimetry as a tool for hydrologic research at the Sutherland Observatory
Gravimetry as a tool for hydrologic research at the Sutherland Observatory Andreas Güntner, Christoph Förste, Theresa Blume GFZ German Research Centre for Geosciences Gaathier Mahed, Maarten De Wit, Moctour
More informationRegional Gravity field modeling as multi-resolution representation estimated from the combination of heterogeneous data sets
Regional Gravity field modeling as multi-resolution representation estimated from the combination of heterogeneous data sets Verena Lieb 1, Klaus Börger 2, Wolfgang Bosch 1, Johannes Bouman 1, Kirsten
More informationCopernicus Today and Tomorrow GEO Week Group on Earth Observation Geneva, 16 January 2014 The Copernicus Space Infrastructure
Copernicus Today and Tomorrow GEO Week Group on Earth Observation Geneva, 16 January 2014 The Copernicus Space Infrastructure Thomas Beer, Policy Coordinator, Copernicus Space Office, ESA-ESRIN, Frascati
More informationGRAVITY ANOMALY ASSESSMENT USING GGMS AND AIRBORNE GRAVITY DATA TOWARDS BATHYMETRY ESTIMATION
GRAVITY ANOMALY ASSESSMENT USING GGMS AND AIRBORNE GRAVITY DATA TOWARDS BATHYMETRY ESTIMATION A Tugi a, A H M Din a,b *, K M Omar a, A S Mardi a, Z A M Som a, A H Omar a, N A Z Yahaya a, N Yazid a a Geomatic
More informationGE SPACE. Geomagnetic Earth Observation from SPAce
GE SPACE Geomagnetic Earth Observation from SPAce Fit to NERC s Science Priorities Understanding the complex interactions and feedbacks within the Earth system over a range of space and time scales Fit
More informationAccelerometers for GNSS Orbit Determination
Accelerometers for GNSS Orbit Determination Urs Hugentobler, Anja Schlicht Technische Universität München 5th International Colloquium on Scientific and Fundamental Aspects of the Galileo Programme October
More informationGPS-ONLY GRAVITY FIELD RECOVERY FROM GOCE
GPS-ONLY GRAVITY FIELD RECOVERY FROM GOCE A. Jäggi, H. Bock, and U. Meyer Astronomical Institute, University of Bern, 3012 Bern, Switzerland ABSTRACT The Gravity field and steady-state Ocean Circulation
More informationTorsten Mayer-Gürr Institute of Geodesy, NAWI Graz Technische Universität Graz
GGOS and Reference Systems Introduction 2015-10-12 Torsten Mayer-Gürr Institute of Geodesy, NAWI Graz Technische Universität Graz Torsten Mayer-Gürr 1 Course and exam Lecture Monday 14:00 16:00, A111 (ST01044)
More informationESA s Juice: Mission Summary and Fact Sheet
ESA s Juice: Mission Summary and Fact Sheet JUICE - JUpiter ICy moons Explorer - is the first large-class mission in ESA's Cosmic Vision 2015-2025 programme. Planned for launch in 2022 and arrival at Jupiter
More informationOriginally published as:
Originally published as: Bruinsma, S., Förste, C., Abrikosov, O., Marty, J. C., Rio, M. H., Mulet, S., Bonvalot, S. (2013): The new ESA satellite only gravity field model via the direct approach. Geophysical
More informationDTM2018 IN THE FRAMEWORK OF THE H2020 PROJECT SWAMI
This project has received funding from the European Union s Horizon 2020 research and innovation programme under grant agreement No 776287 DTM2018 IN THE FRAMEWORK OF THE H2020 PROJECT SWAMI Sean Bruinsma
More informationGeomagnetic Field Modeling Lessons learned from Ørsted and CHAMP and prospects for Swarm
Geomagnetic Field Modeling Lessons learned from Ørsted and CHAMP and prospects for Swarm Nils Olsen RAS Discussion Meeting on Swarm October 9 th 2009 Nils Olsen (DTU Space) Ørsted, CHAMP, and Swarm 1 /
More informationValidation of GRACE time-variable gravity field by ICESat, GPS, WGHM and altimetry satellites
Validation of GRACE time-variable gravity field by ICESat, GPS, WGHM and altimetry satellites Christian Gruber 1, Andreas Groh 2, Elisa Fagiolini 1, Christoph Dahle 1, Sergei Rudenko 1 (1) German Research
More informationA new era of geodetic big data - challenges and opportunities Tim Wright (COMET, University of
A new era of geodetic big data - challenges and opportunities Tim Wright (COMET, University of Leeds) S @NERC_COMET N A New Era of Geodetic Big Data? GEM Strain Rate Model 17,491 GNSS sites included in
More informationAdvances in Geosciences
Advances in Geosciences (2003) 1: 57 63 c European Geosciences Union 2003 Advances in Geosciences Integrated sensor analysis for GRACE development and validation B. Frommknecht 1, H. Oberndorfer 1, F.
More informationLoan 867. Calibration and validation of the CryoSat radar altimeter: field studies on the Greenland Ice Sheet.
Loan 867. Calibration and validation of the CryoSat radar altimeter: field studies on the Greenland Ice Sheet. Elizabeth M. MORRIS Scott Polar Research Institute, Lensfield Road, Cambridge CB2 1ER, UK.
More informationInternational Union of Geodesy and Geophysics. Resolutions
International Union of Geodesy and Geophysics Resolutions ADOPTED BY THE COUNCIL AT THE XXVI GENERAL ASSEMBLY PRAGUE, CZECH REPUBLIC (22 JUNE 2 JULY 2015) 0 Page Resolution 1: Role of Ocean in Climate
More informationNGS is Scheduled to Replace NAVD 88 and NAD 83 In 2022
NGS is Scheduled to Replace NAVD 88 and NAD 83 In 2022 Indiana Society of Professional Land Surveyors Conference January 2017 John Ellingson NGS Geodetic Advisor john.ellingson@noaa.gov 202-306-6904 1
More informationTracing rays through the Earth
Tracing rays through the Earth Ray parameter p: source receiv er i 1 V 1 sin i 1 = sin i 2 = = sin i n = const. = p V 1 V 2 V n p is constant for a given ray i 2 i 3 i 4 V 2 V 3 V 4 i critical If V increases
More informationIMPACT OF CROSS WINDS IN POLAR REGIONS ON GOCE ACCELEROMETER AND GRADIOMETER DATA
IMPACT OF CROSS WINDS IN POLAR REGIONS ON GOCE ACCELEROMETER AND GRADIOMETER DATA Nadja Peterseim 1, Anja Schlicht 2, Claudia Stummer 1, and Weiyong Yi 1 1 Institut für astronomische und physikalische
More informationEvaluation of the EGM2008 Gravity Field by Means of GPS- Levelling and Sea Surface Topography Solutions
Evaluation of the Gravity Field by Means of GPS- Levelling and Sea Surface Topography Solutions Thomas Gruber Institute of Astronomical and Physical Geodesy Technical University Munich, Germany e-mail:
More informationChapter 2. The Planet Oceanus
Chapter 2 The Planet Oceanus Composition of the Earth The Earth consists of a series of concentric layers or spheres which differ in chemistry and physical properties. There are two different ways to describe
More informationContribution of non-tidal oceanic mass variations to Earth rotation determined from space geodesy and ocean data
Earth FOR584 rotation Earth and rotation global and dynamic global processes dynamic processes Contribution of non-tidal oceanic mass variations to Earth rotation determined from space geodesy and ocean
More information