GOCE Gravity Gradients in Instrument and Terrestrial Frames

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010 GOCE Gravity Gradients in Instrument and Terrestrial Frames J. Bouman , Th. Gruber, S. Rispens, E. Schrama, C.C. Tscherning, M.Veicherts, P. Visser

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GOCE Gravity Gradients in Instrument and Terrestrial Frames. J. Bouman , Th. Gruber, S . Rispens , E. Schrama , C.C. Tscherning , M.Veicherts , P. Visser. This presentation. Analysis of GOCE gravity gradients Instrument and Earth related frames - PowerPoint PPT Presentation

Transcript of GOCE Gravity Gradients in Instrument and Terrestrial Frames

Page 1: GOCE Gravity Gradients in Instrument and Terrestrial Frames

Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

GOCE Gravity Gradients in Instrument and Terrestrial Frames

J. Bouman, Th. Gruber, S. Rispens, E.

Schrama, C.C. Tscherning,

M.Veicherts, P. Visser

Page 2: GOCE Gravity Gradients in Instrument and Terrestrial Frames

Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

This presentation

Analysis of GOCE gravity gradients• Instrument and Earth related frames• Data: 31 October 2009 – 11 January

2010• First GOCE gravity field solutions

use same data period (next three presentations)

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

Gravity Gradient Preprocessing

Temporal corrections

Outliers, data gaps External calibration

EGG_NOM_2

Frame trafo

EGG_TRF_2

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

EGG_NOM_2 & EGG_TRF_2

• EGG_NOM_2:– Given in instrument frame (GRF)

– Accurate: VXX, VYY, VZZ, VXZ; less accurate: VXY, VYZ

– Error increase at long wavelengths– Used in gravity field recovery

• EGG_TRF_2:– Given in Local North-Oriented Frame

– GGs VXY, VYZ: GOCE gravity model

– Long wavelength GG signal: GOCE gravity model– GG error expected to be more homogeneous

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

EGG_NOM_2 & EGG_TRF_2

• EGG_NOM_2:– Given in instrument frame (GRF)

– Accurate: VXX, VYY, VZZ, VXZ; less accurate: VXY, VYZ

– Error increase at long wavelengths

• EGG_TRF_2:– Given in Local North-Oriented Frame

– GGs VXY, VYZ: GOCE gravity model

– Long wavelength GG signal: GOCE gravity model– GG error expected to be more homogeneous

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

EGG_NOM_2:3 revolutions November 1, 2009

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

VZZ time series, 1 day

SD VZZ, 1 day

SDs VZZ temporalcorrections, 1 day

Temporal gravity field variations

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

External calibration

Three methods for GG calibration:1. Global gravity field models2. GOCE GPS data3. Terrestrial gravity data• GG scale factors 10-2 – 10-3

• See Poster 014-D3:External Calibration of the GOCE Gravity Gradients at the High-Level Processing Facility (Wednesday)

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

Estimated GG error SDsVXX, VYY, VZZ

MeasurementBand (MB)

GOCE QL gravity model:• GGs and GPS tracking• Data from November and

December 2009• SH degree 200• Error assessment using

GG residuals

• VXX and VYY same noise level in MB, VZZ 2x larger• Noise reduction in upper MB is “work in progress”

(see Fehringer et al, Floberghagen, this morning)

(Pail & Mayrhofer 2010)

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

EGG_NOM_2 & EGG_TRF_2

• EGG_NOM_2:– Given in instrument frame (GRF)

– Accurate: VXX, VYY, VZZ, VXZ; less accurate: VXY, VYZ

– Error increase at long wavelengths

• EGG_TRF_2:– Given in Local North-Oriented Frame

– GGs VXY, VYZ: GOCE QL gravity field model

– Long wavelength GG signal: GOCE gravity model– GG error expected to be more homogeneous

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

EGG_NOM_2 & EGG_TRF_2:3 revolutions November 1, 2009

EGG_NOM_2 EGG_TRF_2

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

EGG_TRF_2: VXX

GOCE - EIGEN5C (N=360) Binned averages

31 October 2009 - 11 January 2010

GOCE - EGM2008 (N=360)Binned averages

31 October 2009 - 11 January 2010

Color scale: -15 mE to +15 mE

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

EGG_TRF_2: VYY

GOCE - EIGEN5C (N=360) Binned averages

31 October 2009 - 11 January 2010

GOCE - EGM2008 (N=360)Binned averages

31 October 2009 - 11 January 2010

Color scale: -15 mE to +15 mE

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

EGG_TRF_2: VZZ

GOCE - EIGEN5C (N=360) Binned averages

31 October 2009 - 11 January 2010

GOCE - EGM2008 (N=360)Binned averages

31 October 2009 - 11 January 2010

Color scale: -15 mE to +15 mE

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Bouman et al, GOCE Gravity Gradients, ESA Living Planet Symposium 2010

Summary

• GOCE gravity gradients in GRF and LNOF (EGG_NOM_2 & EGG_TRF_2)

• November 2009 – January 2010 timeframe

• Differences with EIGEN5C & EGM2008(Africa, Himalaya, …)

• Error level VZZ about 2x that of VXX, VYY in MB

• Spurious tracks VYY close to magnetic poles:

– Not well understood

– Very likely related to interaction between attitude control and magnetic field

– Seems to diminish after in-flight calibration 11/12 January 2010

• Overall, GG data look very good