Presentation is loading. Please wait.

Presentation is loading. Please wait.

Introduction to geodesy & accelerometry with Swarm

Similar presentations


Presentation on theme: "Introduction to geodesy & accelerometry with Swarm"— Presentation transcript:

1 Introduction to geodesy & accelerometry with Swarm
Christian Siemes and the ACC/GPSR Quality Working Group Eelco Doornbos Jose van den Ijssel Joao de Teixeira da Encarnação Aleš Bezděk Radek Peřestý & VZLU team Heike Bock Sean Bruinsma Third Swarm Science Meeting Copenhagen, Denmark 20/06/2014

2 Introduction to geodesy & accelerometry with Swarm
Consider S/C as proof-mass Orbit is shaped by gravitational and non-gravitational forces

3 Introduction to geodesy & accelerometry with Swarm
Consider S/C as proof-mass Orbit is shaped by gravitational and non-gravitational forces Earth’s gravity field g00 ~ 101 m/s2 g20 ~ 10-2 m/s2 grest ~ 10-4 m/s2 All other ~ 10-6 m/s2 and smaller Non-gravitational acceleration ~ 10-7 m/s2

4 Introduction to geodesy & accelerometry with Swarm
Consider S/C as proof-mass Orbit is shaped by gravitational and non-gravitational forces GPSR: Determine orbits  presentation by Jose vd IJssel Accelerometer: Measure non-gravitational acceleration

5 Introduction to geodesy & accelerometry with Swarm
Consider S/C as proof-mass Orbit is shaped by gravitational and non-gravitational forces GPSR: Determine orbits  presentation by Jose vd IJssel Accelerometer: Measure non-gravitational acceleration Determine the gravity field Study thermospheric density and wind  presentation by Eelco Doornbos

6 Introduction to geodesy & accelerometry with Swarm
Swarm A, B, and C High-low satellite-to-satellite tracking using GPS Swarm A and C Inter-satellite baseline processing using GPS

7 GPSR Dual-frequency GPS receiver that can track up to 8 GPS satellites
L1b data has been released to all users Higher noise level near geomagnetic poles and at South Atlantic Anomaly (still within specification, most likely due to ionospheric scintillations) SLR validation confirms high quality of L2 orbits for Swarm A, B and C Reduced dynamic orbit shows 0–3 mm mean and RMS = 2.0 cm Kinematic orbits fit the reduced-dynamic PSO solutions to ~10 cm Lucky coincidence Swarm A and C track simultaneously since 2 March 2014 (~0.2 µs, last checked on 31 May, chances: 1:9) Swarm C is flying in constellation with Swarm A since mid April Running investigations following QWG recommendations Enlarging mask that limits the antenna field-of-view (FoV) to 80 degrees Increase data rate from 0.1 Hz to 1 Hz (RINEX files) Synchronization GPS measurement epochs across satellites (simultaneous tracking) Credits: Jose vd IJssel Credits: Heike Bock

8 GPSR First gravity field results based on data of two months Credits:
Heike Bock, Adrian Jäggi, Ulrich Meyer (Astronomical Institute, University of Bern) Christoph Dahle (GFZ, German Research Centre for Geosciences, Potsdam)

9 Accelerometer Measurement principle
Accelerometer rigidly connected to satellite Cubic proof-mass free-floating in cavity (no connection to cavity) Position of proof-mass controlled by electrostatic forces applied through 6 electrodes located on the inner walls of the cavity Control voltages applied to electrodes are representative for forces acting on satellite

10 Accelerometer Specifications of the instrument
Measurement band – 100 mHz Linear acceleration range ±1 x 10-4 m/s2 Linear acceleration resolution x 10-9 m/s2 Angular acceleration range ±9.6 x rad/s2 Angular acceleration resolution x 10-7 rad/s2 Overall random error (1 sigma) x 10-9 m/s2 Accuracy of linear acceleration better than 0.2% No dedicated temperature control (conscious decision in mission design) Raw accelerometer data is sensitive to on-board temperature variations On-ground characterization of temperature dependency Full testing of performance not possible on-ground Instrument is designed for micro-g environment Control voltages do not have the capability to lift proof-mass in 1-g environment

11 Accelerometer status All accelerometer instruments are working

12 Accelerometer status All accelerometer instruments are working, however: Unexpectedly large temperature dependency Instrument bias discontinuities (steps) and other disturbances (spikes, pulses) Swarm C: Along-track acceleration Swarm B: ACC temperature versus along-track acceleration

13 Accelerometer status First promising results for temperature correction model (work in progress) The heat transfer model relates temperature measured at sensor locations to temperature at sensitive points Credits: Radek Peresty & VZLU team

14 Accelerometer status Swarm B Next talk: Comparison of Swarm A and C
First promising results for temperature correction model (work in progress) Swarm B Next talk: Comparison of Swarm A and C Credits: Eelco Doornbos

15 Accelerometer status Example for steps & other Swarm C

16 Accelerometer status Example for steps & other
Swarm C: Nadir acceleration

17 Accelerometer status Example for steps & other AOCS thruster firings

18 Accelerometer status Example for steps & other ?

19 Summary GPSR L1b data released to general users High quality L2 orbits
Consistent performance of Swarm A, B, and C Accelerometer Swarm C provides significantly better accelerometer data than Swarm A and B Large temperature dependency observed on Swarm A and B New temperature correction gives promising first results, in particular for along-track axis (ongoing investigations) Accelerometer data contains unexpectedly large number of steps and other disturbances that are not understood Physical cause not clear Treatment of steps under investigation Accelerometer data not yet ready for general user community (release date unclear) Industry, science and ESA are working hard to solve the problems!


Download ppt "Introduction to geodesy & accelerometry with Swarm"

Similar presentations


Ads by Google