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卫星大地测量探测技术及应用 许厚泽 中国科学院测量与地球物理研究所 2009年10月 中国石油大学

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卫星大地测量探测技术及应用 许厚泽 中国科学院测量与地球物理研究所 2009年10月  中国石油大学. 报告内容. 卫星大地测量探测技术在资源勘探、环境变化及灾害监测中的应用. 卫星大地测量探测技术. 全球卫星导航系统 GNSS 包括 GPS, Glonass, Galileo, 北斗等 卫星测高系统, Topex, Jason 及 HY-II( 中国) 冰卫星测高技术 Icesat 合成孔径雷达干涉系统 InSar 重力卫星系统 CHAMP, GRACE, GOCE 测量分为两类 地球形状和位置变化 地球质量分布及迁移. - PowerPoint PPT Presentation

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  • 200910

  • GNSS GPS Glonass GalileoTopex, JasonHY-II Icesat InSar CHAMP, GRACE GOCE

  • GPSSLRVLBISASGAG

  • VLBI25VLBI

  • VLBI NETWORK

  • SLRLageos-1

  • SLR NETWORK

  • GPS GPS

  • GPS , , , , :: 2420000km. , 4, 55, , 11h58m: : , (), , 4, 4.t, x, y, z, , >4, .

  • GPS Satellite

  • ( ) , L1 1575.42MHz L2 1227.6MHz L P C/A D ()L1 P, C/A, D L2 PDP, 10mC/A, 30m (SA100m)

  • , () , ,

  • (), , . ., , .(), :h

  • GEOSAT1985-3-12

  • ERS-1 1991-7-17

  • Topex/Poseidon1992-8-10

  • ERS-21995-4-21

  • GFO(Geosat-Follow-On) 1998-2-10

  • JASON(T/P-follow-on) 2000-5-18

  • ENVISAT2000-5

  • Sea Surface Topography observed from Topex/Poseidon

  • M2

  • When La Nia 98 takes over El Nio 97

  • An altimetric view of the seafloor

  • (October 1992)Wind speed (October 1992) (October 1992)

  • T/PTide Gauge

  • 1.2.

  • 16th Century17th18th19th20th21stEarths Gravity MeasurementHistory

  • Satellite Gravity MeasurementPrinciple

  • CHAMPGOCEGRACEInternational Satellite Gravity Missions

  • SSTSGG 1969 SST 1979 GRM 1980 1985 Geosat 1987 , 1990-91 AristotelesGradio 1992 Topex/PoseidonGPS 1995 CHAMP 1996 GRACE GOCE 1997 1998 22IUGG IAG2NASAESAGRACE GOCE 2000.7.15 CHAMP 2002.3.19 GRACE 2009.3 GOCE

  • Launch: July 2000

  • SST - hlGPS SatellitesEarthMassanomaly3-D accelerometerCHAMP ConceptH = 470 - 300 km,polar, circular orbitT = 5 years,High-Low-SST(d = 20 000 km) + accelerometryd

  • Launch: March 20021cm-geoid with a spatial resolution of 200 km and temporal variations

  • May 3, 2003Gravity anomaly and intersatellite range changes when GRACE flying the Qinghai-Tibet Platean

  • SST - hlGPS SatellitesEarthMassanomalySST - llGRACE ConceptH = 470 - 300 km,polar, circular orbitT = 5 years,Low-low-SST(d = 250 km, sd=10 mm) + accelerometryd

  • H = 240 kmdrag-freesun-synchronouslaunch: 2006T = 20 monthsgradiometry1cm-geoid with a spatial resolution of 100 km

  • SGGEarthMassanomalyGPS SatellitesSST - hlGOCE ConceptGradiometry: differential accelerometry within the satellited = 30 cmsa = 8 mEd1 E = 1 Etvs = 10-9 s-2

  • Main points of satellite technique Low orbit (400km) Near polar orbit GPS space borne receiver (cm accuracy) 3D accelerometer to measure and substract the non-conservation forces Satellite-satellite range and range-rate measurement Gravity gradiometer

  • CHAMP GRACE GOCE GFZ NASA DLR ESA 2000.7.15 2002.3.17 2009.3 (y)5 ~ 105 ~ 102 (km)454 ~ 300500 ~ 300250 ~ 240 (o)878996.5 < 0.004 < 0.004 < 0.001 (km) 22050 SST-HL SST-HL/LL SST-HL/SGG

  • CHAMP GRACE GOCE GPS (cm) 1031 (m/s2 )310-9 310-10 K (m/s) 10-6 (/s2) 310-12

  • CHAMP, GRACE, GOCE

  • Cumulative Geoid Height Errors (10-2 m)

    Degree(L)EIGEN-CHAMP03SCHAMP(Energy)EIGEN-GRACE02SGRACE(Energy)GRACE(Semi-analytic)GOCE(SGG)200.4560.3730.0760.0450.0660.625504.0854.2260.2280.2110.1991.18670 18.419 17.2730.8130.8120.8061.7131005.7564.8855.5032.228120 18.938 17.316 18.3952.4312004.6822509.055

  • Before satellite gravity (20 years data)Advances in Earths Gravitational FieldGRACE mission(111 days measurements)GRACE mission(13 months measurements

  • Static satellite gravity field

  • OutlineGRACE data span now >6 yrsSeveral Science Data System (SDS) centers (e.g. CSR, GFZ, JPL, CNES)

    post-processing improvement (Spectrum interference )Mass changes detection (Three Gorges region, Sumatra earthquake, sea level changes, etc) stripe

  • Cumulative Geoid Error CurvesError curves provided by GFZ Potsdam

  • Inversion of gravity modelDynamic orbit integration methodEnergy conservation method

    Gravity models GGM01C (CSR MODEL) EIGENGRACE02 (GFZ MODEL)

  • IGG MODELGRACE data:Level 1B data products, including K-band range and range rate, orbit , accelerometer and star camera assembly data et al.Dynamic models Plantetary Ephmerides:DE-200 Background static gravity field:GGM01C Solid tidal corrections:Wahr(1981) Ocean tidal corrections:CSR3.0 Polar motion:IERSC04 Uniform time system: all change to UTC

  • 1 Problems with GRACE L2 data

  • Stokes

  • 22)

  • 22

  • 2005321.63 mGal 2.92 mGal0.69 mGal2.0 mGal1.0-2.0 mGal

  • 228000 222.9 mGal3-5mGal

  • ETOPO5 Obtained from altimetric graivty anomaly

    A Shaded-relift image of the bathymetry over the East China Sea

  • 183mETOPO5252m

  • Tectonic setting

  • mGal

    ABCD1795231917922125-5.3-4.8-6.9-7.95.24.42.16.70.9-0.4-2.0-0.51.81.72.12.92.01.72.92.9

  • The interrelation of gravity, gravity variation, mass transports and mass anomalies

  • Science, Wahr, 2006

  • GRACE(without PGR)PGR model Mass changes over AntarcticaPGR correction applied, Paulson et al. 2007 (a) East Antarctica Ice Sheet;b West Antarctica Ice Sheet;cLarsen Ice Sheet (Point C)GRACE(with PGR)GRACE

  • MODISICESat, GRACE2003-2008GRACEICEsat2

  • The Greenland ice sheet is the 2nd largest ice cap on Earth, and contains ~ 2.5 million cubic kilometers or 10% of total global ice mass. The glacial complex in southeast Greenland is among the most active glaciers.Science, Chen, 2006

  • IAG, Ramillien, 2006

  • +++--5

  • Water Storage Changes over China landNorth Niemeng region (-), North China(-), Lower Reaches of Yangtze river (-), Middle and Upper Reaches of Yangtze river (+), Tian mountain snowfield (-), Himalayas Icefield (-).Tian mountain snowfield Himalayas IcefieldNorth NiemengNorth ChinaLower Reaches of Yangtze riverMiddle and Upper Reaches of Yangtze riverWenchuan Earthquake??

  • (400).

  • GRACEGRACE23.29/.,,! 77.80,33.20.

  • GRACE- 19.32/48/42/197640/

  • GRACE- 17.82/,

  • ,GRACE15.3/.80.60,42.1081.50,42.4082.30,42.80

  • ,5~10,11~4,

  • ,,.

  • IPCC WG1 Fourth Assessment Report,2006 192021

  • 10 40

  • SLVtotal = SLVsteric + SLVmass + GRACE

  • Seasonal Variations Removed60-Day SmoothingGIA Correction AppliedRate = +3.3 0.4 mm/year(GIA Correction Applied)http://sealevel.colorado.edu

    22 1mm/600km

  • 2.60.4 mm/yr2.8 mm/yr ICE-4G)()C.K. Shum, 2007,IUGGIB correction (ECMWF) applied

  • GRACE1.4 mm/yrBouhours)

  • GIA: -0.3mm/yr GIA: +1.4mm/yr2003-2006GRACE

  • +3.2 0.6 mm/yrGRACE : ocean mass variations from GSMAltimetry SLA minus GRACE : steric height variationsTotal Sea level variation budgetSteric Component (by combining altimetry and gravimetry data) : ~ 1.9 0.3 mm/yr Ishii: steric component+1.9 0.1mm/yr (Willis)Before 2003, not afterAltimetry SLA

  • CMONOC ,

  • GRACE Observed Gravity Change (15 gal)Seismic Model Predicted Gravity ChangeGalGal2005Nature, Han & Shum, 2006

  • ABSumatra-earthquake regionSumatra-earthquake region

  • 122 20073210633 35.681.6 7.3 ----1 2008-05-12 14:28 31.0, 103.4 8.0 7-------7

  • GRACE show that a rising rate is 12.1 mm/y.An notable change: water storage or solid mass redistribution? (2008.5.12,M7.9,N30.99,E103,36,Depth 19.0km)Wenchuan Earthquake

  • globalDynamicSteric4-D3-DRegionalSpaceGroundGlobal changes:Sea level change, Ice balanceocean currents and water storage etc.

    Disaster monitoring:Earthquake, volcano, ionosphere etc.National defence:Spaceflight technology improvement.ApplicationsPowerful geodesy

  • Thank you!

    ******Slide to introduce the sea level change time series from altimetry (note that this has some animations - modify this if you dont like it).Point out the change in MSL during the 1997-98 ENSO event.**