DORIS DAYS 2-3 May 2000 DORIS campaigns at Dome Concordia, Antarctica in 1993 and 1999-2000 C. Vincent1, JJ. Valette2, L. Soudarin2, JF. Crétaux3, B. Legresy3, F. Rémy3, A. Capra4 1 LGGE/CNRS, Laboratoire de Glaciologie et de Géophysique de l’Environnement, Grenoble, France 2 CLS, Collecte Localisation Satellites, Ramonville, France 3 LEGOS/GRGS (CNES/CNRS-UPS), Toulouse, France 4 Istituto de Topografia, Geodesia e Geofisica Mineraria, Universita de Bologna C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. Dome Concordia Titre: GMT v3.0 Document f rom grdcont our Auteur: legres y benoit -grgs 62956Aperç u: Cette image EPS n'a pas été enregis trée avec un aperç u int égré. Commentaires: Cette image EPS peut êt re imprimée s ur une imprimante PostScript mais pas s ur un aut re t ype d'imprimante. Base on the Antarctic continent open from December to February since 1996, permanent by 2003 Management by IFRTP Concordia : French - Italian glaciological research project (LGGE/DISTART,...) topics : snow accumulation, ice thickness, ice flowing … EPICA : European project for deep ice coring topics : ice cap response to global climate changes, north-south hemisphere coupling... C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. Why a drilling location there? Interests of this continental dome : T < -25°C, no summer ice melting excellent location for a whole Antarctic record 3300 m thickness long and continuous climate record 400 Ka least disturbed ice sequence at the dome summit (minimal ice flow correction) C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. Main geodetic informations needed Questions 1996 Position of the dome summit ? Technique ERS-1 altimeter (Rémy) GPS (Ceffalo) Airbone VHF radar (Tabacco) for layering 2000 Absolute 3D ice surface velocity ? local deformation ? C. VINCENT LGGE/CNRS DORIS 1993 and 1999-2000 (C. Vincent) GPS 1995-1998 (A. Capra) ERS-1 Insar 1996 (B. Legrésy) DORIS DAYS 2-3 May 2000 Toulouse, France. Charming but constraining place (1) Equipment suffering : beacon specification from -20° to +55°C gradient < 10°/hr Generator failures USO drift of a few 10-11/jr (still under specification) C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. Charming but constraining place (2) Scientist suffering : Dry but freezing summertime (4 g/cm2 equivalent water a year) What geodetic « monumentation » ? How to prevent from stake subsidence? How to measure snow accumulation ? C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. CLS DORIS Data Processing Center, Toulouse Onboard instrument control Telemetry acquisition and preprocessing Operational orbit and stations position (48 h delay) 2 days delay Dome C operational location (height) Spot 4 data validation C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. DORIS campaigns 10 km 5 m isolines Drilling site D1 Doris main site (IERS id. : 66009 in 93 - 66013 in 99) D2 Doris ancillary site (66014) DORIS observations at main point (D1) C. VINCENT LGGE/CNRS 1993 : 16 days (11/26 – 12/5) SPOT 2 85 pass. / 2097 obs. 1999-2000 : 27 days (12/8 – 1 /2) SPOT 2 and 4 498 pass./ 13164 obs. DORIS DAYS 2-3 May 2000 Toulouse, France. Data processing At GRGS/CLS DORIS data analysis center for IERS and IDS with GINS/DYNAMO software and the most recent models : GRIM5 (Biancale et al.), atmospheric effects Geodetic parameters : satellites orbit, stations position and velocity Empirical coefficients : air drag, solar pressure radiation, Hill residual forces, zenital tropospheric delay Instrumental parameters : USO frequency bias C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. Absolute velocity corrections Antarctic plate tectonic motion deduced from DORIS at Dome Concordia : in latitude : -9.4 mm/yr in longitude : 0.4 mm/yr Titre: GMT v3.0 Document from ps coas t Auteur: laurent s oudarin grgs p 62925 Aperç u: Cette image EPS n'a pas été enregis trée avec un aperç u intégré. Commentaires: Cette image EPS peut être imprimée s ur une imprimante PostScript mais pas s ur un autre type d'imprimante. (Crétaux et al. 1998) Post glacial rebound uplift : less than 1-3 mm/yr C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. Preliminary DORIS results 2 months global network solutions (Nov-Dec 93 and 99) Typical precision : Permanent station 1 satellite 2 cm 2 satellites 1 cm Dome C 3 cm (1993) 1.5 cm (1999) 7 parameters Helmert transformation (versus solution 1993) 3D coordinates changes over 6 years (same réf. point, plate motion is removed) C. VINCENT LGGE/CNRS Latitude Longitude Height - 3.6 cm - 10.8 cm -57.4 cm DORIS DAYS 2-3 May 2000 Toulouse, France. Contribution to ice core analysis (1) DORIS 3D absolute velocity gives an input for numerical ice flow model in depth. Essential for cores dating. DORIS results in horizontal : 0.6 cm/yr in latitude -1.8 cm/yr in longitude Titre: GMT v3.0 Doc ument from ps basemap Auteur: legresy benoit -grgs 62956Aperçu: Cette image EPS n'a pas été enregis trée av ec un aperçu intégré. Commentaires : Cette image EPS peut être imprimée sur une imprimante Pos tSc ript mais pas sur un autre ty pe d'imprimante. agree with balance model between snow accumulation and ice flow induced by gravity (figure) (Legresy) C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. Contribution to ice core analysis (2) DORIS results in vertical : -9.6 cm/yr Probably the first absolute determination of the vertical velocity observed snow accumulation at the top of the stake (height level change) : 35 cm over the 6 years while 10 cm/yr is expected (Petit et al.) Error observation or snowfall anomaly ? Mass balance between snowfall and ice flow towards the ocean ? Sea level and climat changes implications C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. Contribution to radar remote sensing observations SAR Interferometry maps relative surface velocity in the line of sight ERS SAR interferogram (69 days interval) shows maximum of 3 cm/yr DORIS gives the absolute ITRF tie of the velocity fields Space Radar Altimetry maps ice topography within 10-20 cm but an in-situ calibration is needed, moreover the signal penetration depends on the snow structure DORIS gives the height reference and its variations in time C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. Conclusions DORIS (93-99) component of CONCORDIA project confirms that a very low absolute horizontal ice surface velocity affects the EPICA drilling (< 2 cm/yr). Also vertical flow determination as a first. DORIS absolute geodetic approach fully completes GPS survey and calibrates radar satellite remote sensing techniques (with future missions ERS2, ENVISAT, IceSat, CRYOSAT). Proposal to IDS for repeated DORIS campaigns at Dome Concordia C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France.