Joint GSTM and DFG SPP Symposium, GFZ-Potsdam 15-17 October 2007 ESA’s supporting Activities Related to Mass Transport in the Earth System Roger Haagmans.

Slides:



Advertisements
Similar presentations
Global Ocean Tide Models – Assesment of Errors and their Impact on GRACE gravity fields Roman Savcenko and Wolfgang Bosch Deutsches Geodätisches Forschungsinstitut.
Advertisements

Earth Science Division
“SAMOSA” an ESA SAR Altimetry Ocean, Coastal Zones and Inland Water Development Study Jérôme Benveniste ESA Jérôme Benveniste ESA Presented at the Coastal.
NERC & Earth Observation  The UK is a founder member of the European Space Agency. Despite ambivalence about some aspects of space policy, the UK has.
Effect of Surface Loading on Regional Reference Frame Realization Hans-Peter Plag Nevada Bureau of Mines and Geology and Seismological Laboratory University.
GRACE GRAVITY FIELD SOLUTIONS USING THE DIFFERENTIAL GRAVIMETRY APPROACH M. Weigelt, W. Keller.
ESA’s Living Planet Programme: Overview & Status Mark R. Drinkwater European Space Agency Earth Observation Programmes.
Frank Martin Seifert EO Science and Applications Division ESA Earth Observation Programme SDCG-6 | 23 October 2014 | Oslo The European Copernicus Programme.
Satellite geodesy. Basic concepts. I1.1a = geocentric latitude φ = geodetic latitude r = radial distance, h = ellipsoidal height a = semi-major axis, b.
GRACE “Gravity Recovery and Climate Experiment” Use in measuring Earth’s gravitational field and geoids By Jacob Launder.
The Four Candidate Earth Explorer Core Missions Consultative Workshop October 1999, Granada, Spain, Revised by CCT GOCE S 59 Performance.
ICESat dH/dt Thinning Thickening ICESat key findings.
A-SCOPE Advanced Space Carbon and Climate Observation of Planet Earth MAG: F.M. Breon, H. Dolman, G. Ehret, P. Flamant, N. Gruber, S. Houweling, M. Scholze,
J. Ebbing & N. Holzrichter – University of Kiel Johannes Bouman – DGFI Munich Ronny Stolz – IPHT Jena SPP Dynamic EarthPotsdam, 03/04 July 2014 Swarm &
Planetary Magnetic Fields Presentation by Craig Malamut September 18, 2012 Stevenson (2003) Illustration courtesy of NASA (
MTR, swarm E2E study, Nov 11, 2003, DSRI Copenhagen, nio #1 7-Sep-15 swarm End-To-End Mission Performance Study Mid Term Review The swarm E2E Consortium.
Kick off meeting, swarm E2E study, nio #1 8-Sep-15 Development Approach Task 1: Industrial Module –to be used by industry for their system simulation –Output:
→ Potential ESA- Roscosmos Cooperation in Education Activities.
Icebase: A proposed suborbital survey to map geothermal heat flux under an ice sheet Michael Purucker SGT at Planetary Geodynamics Lab, Goddard Space Flight.
Österreichische Akademie der Wissenschaften (ÖAW) / Institut für Weltraumforschung (IWF), Graz, Austria, T +43/316/ , iwf.oeaw.ac.atDownload:2013.
Agency, version?, Date 2012 Coordination Group for Meteorological Satellites - CGMS Add CGMS agency logo here (in the slide master) Coordination Group.
Tielong Zhang On behalf of the CGS Team in the Institute of Geology and Geophysics, Chinese Academy of Science Spacecraft System and Payload China Geomagnetism.
23 rd CEOS Plenary I Phuket, Thailand I 3-5 November 2009 Status of the ESA Earth Observation Programmes Dr. Simonetta Cheli Head of Earth Observation.
T SPP1788 “DynamicEarth“ Workshop, GFZ Potsdam, 3 July 2014 No. 1 Calibration/Validation of Swarm Data Products: German activities Hermann Lühr and Cal/Val.
Using GRACE to estimate changes in land water storage: present limitations and future potential John Wahr, Sean Swenson, Isabella Velicogna University.
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.
OC3522Summer 2001 OC Remote Sensing of the Atmosphere and Ocean - Summer 2001 Active Microwave Radar.
Chapter 8: The future geodetic reference frames Thomas Herring, Hans-Peter Plag, Jim Ray, Zuheir Altamimi.
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.,
Hydrological mass changes inferred from high-low satellite- to-satellite tracking data Tonie van Dam, Matthias Weigelt Mohammad J. Tourian Nico Sneeuw.
NKG Working Group for Geodynamics Copenhagen, 23 –24 April, Tasks of a new Working Group on Absolute Gravimetry Herbert Wilmes Federal Agency for.
Agency, version?, Date 2012 Coordination Group for Meteorological Satellites - CGMS Add CGMS agency logo here (in the slide master) Coordination Group.
Last Time: Ground Penetrating Radar Radar reflections image variations in Dielectric constant  r ( = relative permittivity )  3-40 for most Earth materials;
1 Average time-variable gravity from GPS orbits of recent geodetic satellites VIII Hotine-Marussi Symposium, Rome, Italy, 17–21 June 2013 Aleš Bezděk 1.
Patagonia Ice Field Melting Observed by GRACE Joint International GSTM and DFG SPP Symposium, October 15-17, 2007 at GFZ Potsdam J.L. Chen 1, C.R. Wilson.
Water storage variations from time-variable gravity data Andreas Güntner Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences Section.
Lesson 3: Design for Remote Sensing Your Mission 1; just like a real CubeSat.
Joint International GRACE Science Team Meeting and DFG SPP 1257 Symposium, Oct. 2007, GFZ Potsdam Folie 1 Retrieval of electron density profiles.
Sea ice thickness from CryoSat – A new data set for operational ice services? Christian Haas German CryoSat Office AWI.
Geocenter Variations Derived from GRACE Data Z. Kang, B. Tapley, J. Chen, J. Ries, S. Bettadpur Joint International GSTM and SPP Symposium GFZ Potsdam,
DORIS Days May 2-3, 2000 DORIS role in the next years P. Escudier CNES.
SE&I Pre-Proposal Meeting GSFC - JPL Systems Engineering Management Colleen McGraw.
Progress in Geoid Modeling from Satellite Missions
CEOS Plenary Session Montreal, 4 November 2013 Stephen Briggs, ESA Head, Programme Planning and Coordination Service ESA’s Earth Observation Programme.
SPP Mass Transport and Mass Distribution in the Earth System Contribution of the New Generation of Satellite Gravity and Altimetry Missions to Geosciences.
C H A M P International Laser Ranging Service - General Assembly, October 2005 Eastbourne, UK L. Grunwaldt, R. Schmidt, D. König, R. König, F.-H. Massmann.
Study on the Impact of Combined Magnetic and Electric Field Analysis and of Ocean Circulation Effects on Swarm Mission Performance by S. Vennerstrom, E.
ESA living planet symposium Bergen Combination of GRACE and GOCE in situ data for high resolution regional gravity field modeling M. Schmeer 1,
Future China Geomagnetism Satellite Mission (CGS) Aimin Du Institute of Geology and Geophysics, CAS 2012/11/18 Taibei.
Space Gravitational Wave Antenna DECIGO Project 3rd TAMA Symposium February 7, Institute for Cosmic Ray Research, Japan Seiji Kawamura National.
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.
The ESA call for the 9 th Earth Explorer mission (EE9)
Bouman et al, GOCE Calibration, ESA Living Planet Symposium 2010, Bergen, Norway Overview of GOCE Gradiometer Cal/Val Activities J. Bouman, P. Brieden,
39 th Conference of Directors of EU Paying Agencies ESTEC, 25 May 2016 M. Drusch, Principal Scientist Earth Observation Programmes Directorate Science,
Altimeter and scatterometer seminar SMHI, March 2012 Future of satellite altimeters Sentinel-3 and SWOT Julia Figa Saldaña With contributions from Sentinel-3.
SC4MGV – ESA Contract No /13/NL/MV 5th International GOCE User Workshop November 2014, Paris, France ESA SC4MGV Search strategy for.
Thomas Herring, IERS ACC, MIT
Observing Mass Distribution and Transport in the Earth System from an ESA Perspective Roger Haagmans, Pierluigi Silvestrin, Rune Floberghagen, Christian.
Swarm DISC call for ideas
ESA’s Earth Observation Programmes and GOCE
A joint study of the University of Göttingen (1) and Astrium (2)
Introduction to geodesy & accelerometry with Swarm
Session 4: GOCE for Solid Earth
Consistent Ocean Mass Time Series from LEO Potential Field Missions
OceanMag II EM-Raying the Ocean
Systems Engineering Management
Summary & recommendations multi-mission synergies session 9
Future Opportunities in Geomagnetism and Electromagnetism:
Recent Activities of the OST-VC
Laser Interferometry for a future GRACE follow-on mission
Presentation transcript:

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 ESA’s supporting Activities Related to Mass Transport in the Earth System Roger Haagmans Mission Science Division European Space Agency

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Swarm mission: 3D-Mantle Conductivity (A. Jackson ETH Zürich, DNSC, CUP) Swarm mission: gravity field potential (Christian Gerlach TUM and Pieter Visser DUT) Studies related to future ideas

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Swarm Satellite & Constellation launch after 1.5 yr after 3 yrs after 4.5 yrs launchafter 4.5 years red (C) 530 km500 km yellow (A,B) 470 km300 km GPS Patch Antennas Accelerometer Magnetic package

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October D Electrical Conductivity of the Mantle Time-varying external (inducing) magnetic fields produce induced electric currents in the conducting Earth conductivity is sensitive to composition and temperature These induced currents cause induced magnetic field variations

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October D Electrical Conductivity of the Mantle Measured on ground or in space is the total (external + induced) magnetic field Separation of external and induced fields enables determination of the electrical conductivity of the Earth’s interior 3D-Conductivity: hours to months periods, corresponding to app km depth Study team led by Andy Jackson at ETH Zürich together with DNSC Copenhagen and CUP (Prague)

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Swarm mission: 3D-Mantle Conductivity (A. Jackson ETH Zürich, DNSC, CUP) Swarm mission: gravity field potential (Christian Gerlach TUM and Pieter Visser DUT) Studies related to future ideas

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Swarm and Gravity - Constellation Observation: GPS-baseline between satellites GRACE A-B:along-track (KBR, scalar) Swarm A-B:cross-track (GPS, vector) Swarm A-C: ~ radial (GPS, vector) Geometry:

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Gravity Field Gradients along-trackcross-track radial

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 along-trackcross-track along + crossradial (1) SH-Error Characteristics from Gradients in x,y and z

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Simulation results: 1 Month A-B and A-C

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Swarm mission: 3D-Mantle Conductivity (A. Jackson ETH Zürich, DNSC, CUP) Swarm mission: gravity field potential (Christian Gerlach TUM and Pieter Visser DUT) Studies related to future ideas

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007  Enabling Observation techniques for Future Solid Earth Missions.(2003)  Laser Doppler Interferometry Mission for Determination of the Earth’s gravity field. (2005)  Gravity Gradient sensor technology for future planetary missions. (2005)  Laser Interferometry High Precision Tracking for LEO. (2006)  Monitoring and Modelling Individual Sources of Mass Distribution and Transport in the Earth’s System by Means of Satellites ( months) Courtesy: Thales Alenia Space ESA studies: future gravity field concepts

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Measurement and control elements of the SSI mission

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Future Mission Concept From: Ilk et al (2005) Future Concepts?

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Study Team Geophysical Modeling Gravity modeling Mission design SRONUtrecht, NLR. Koop++ DEOSDelft, NLP. VisserSolid earth++ IAPGMunchen, DET. Gruber M. Thomas Atmosphere Oceans ++ GISStuttgart, DEN. Sneeuw++ ULLuxemburg, LUT. van DamGravity+ AWIBremerhaven, DEM. LoschOceans BGCBristol, UKJ. BamberIce SCEGNewcastle, UKM. KingTides UCGUtrecht, NLM. BierkensHydrology

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Study logicGeophysicalmodelling Gravitymodelling Missiondesign Gravityretrieval ObservabilitySeparability

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Geophysical modelling Solid Earth TidesOceans Atmosphere Ice Hydrology Simulated “real” world ConsistentCompatibleCompleteCoupledCoordinatedDedicatedSufficientRealistic

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Current step: Gravity field modelling Geophysical model Earth OrbitObservableConstellation Input gravity Observed gravity along orbit + observation error

Joint GSTM and DFG SPP Symposium, GFZ-Potsdam October 2007 Conclusions Future Mission requires solid preparation: coordination with complementary measurement techniques from other future satellites (like SMOS, CryoSat, Sentinels e.g.) Activities in ESA complement DFG efforts and try to learn from existing analysis to understand the needs for a future mission concept