Magnetic Splinter Meeting

Slides:



Advertisements
Similar presentations
MAE 5410 – Astrodynamics Lecture 5 Orbit in Space Coordinate Frames and Time.
Advertisements

4 th Swarm DQW – Magnetic Session 23 Dec 2014Potsdam (D) ELM – “EXTENDED” LESUR MODEL OF DISTURBANCE CHARACTERISATION AND VFM CALIBRATION Lars Tøffner-Clausen,
GN/MAE155B1 Orbital Mechanics Overview 2 MAE 155B G. Nacouzi.
Time & Frequency Products R. Peřestý, J. Kraus, SWRM 4 th Data Quality Workshop 2-5 December 2014 GFZ Potsdam Recent results on ACC Data Processing 1 SWARM.
Status update of ASM on Swarm Charlie Swarm 4th DATA QUALITY WORKSHOP 2 December 2014 GFZ Potsdam Jean-Michel Léger.
DEFINITION, CALCULATION, AND PROPERTIES OF THE Dst INDEX R.L. McPherron Institute of Geophysics and Planetary Physics University of California Los Angeles.
Monitoring of auroral oval location and geomagnetic activity based on magnetic measurements from satellites in low Earth orbit. S. Vennerstrom Technical.
C. Papadimitriou 1,2,G. Balasis 1, I. A. Daglis 2,1 R. Haagmans 3 1 Institute for Astronomy, Astrophysics, Space Applications and Remote Sensing, National.
Karla Vega University of California, Berkeley Attitude Determination and Control 6/9/2015.
4 th Swarm QWG Meeting 2 – 5 December 2014GFZ Potsdam/D On Calibrating the Magnetometry Package Data Nils Olsen, DTU Space.
J. Ebbing & N. Holzrichter – University of Kiel Johannes Bouman – DGFI Munich Ronny Stolz – IPHT Jena SPP Dynamic EarthPotsdam, 03/04 July 2014 Swarm &
Physical Approach to the ASM-VFM residual investigation National Space Institute, DTU 3. December 2014.
ESA Presentation | P. Vogel | Potsdam | 02/12/2014 | Slide 1 ESA UNCLASSIFIED – For Official Use SWARM QWG Overview of ASM, VFM and STR instruments status.
Swarm Data Processing and First Scientific Results
Study of an Improved Comprehensive Magnetic Field Inversion Analysis for Swarm PM1, E2Eplus Study Work performed by Nils Olsen, Terence J. Sabaka, Luis.
4 th Swarm QWG Meeting 2 – 5 December 2014GFZ Potsdam/D Data Selection Model Parameterization Results: Statistics, Lithospheric Field, Core Field Perspective.
Attitude Determination and Control System
T SPP1788 “DynamicEarth“ Workshop, GFZ Potsdam, 3 July 2014 No. 1 Calibration/Validation of Swarm Data Products: German activities Hermann Lühr and Cal/Val.
Van Allen Probes Spacecraft Operations July 29, 2015 Kristin Fretz
Outline  Construction of gravity and magnetic models  Principle of superposition (mentioned on week 1 )  Anomalies  Reference models  Geoid  Figure.
Secular variation in Germany from repeat station data and a recent global field model Monika Korte and Vincent Lesur Helmholtz Centre Potsdam, German Research.
Chapter 1 Predicting the Motions of the Stars, Sun, and Moon.
Introducing POMME Potsdam Magnetic Model of the Earth Star camera calibration Ring current field Static and annually varying external fields Internal field.
Swarm ASM-VFM meeting 9-10 Apr 2015ESTEC (NL) Ideas for improving the disturbance model or Welcome to the Null-Space! Nils Olsen, Lars Tøffner-Clausen,
1) Magnetic total field (T) obtained from airborne survey (see R.J.Blakely, 1995) (ΔT) Total field anomaly (IGRF removal), which satisfy potential theory,
Survey of the Universe Tom Burbine
The Seasons Seasonality: the variation of the sun’s position over the horizon; the changing daylength during the year Seasons result from: variations in.
Study on the Impact of Combined Magnetic and Electric Field Analysis and of Ocean Circulation Effects on Swarm Mission Performance by S. Vennerstrom, E.
Study of an Improved Comprehensive Magnetic Field Inversion Analysis for Swarm MTR, E2Eplus Study Work performed by Nils Olsen, Terence J. Sabaka, Luis.
The earths energy balance MR ASKEW. The unequal heating of the atmosphere  Short wave radiation heats the earths surface.  The heated earth radiates.
AstroLab-2 Locating Stars in the Sky Merav Opher-Fall 2004.
Introduction to On-Orbit Thermal Environments
Observational Astronomy Mapping the Heavens Coordinate Systems We have two different ways to locate objects in the sky: Celestial equatorial system -Right.
Cross-Calibration Meeting, ESTEC, February Comparison of the EDI and FGM Measurements of the Magnetic Field Magnitude Plot shown.
X axis y axis Points on a coordinate plane are written like this: (-8, 9) Move the dot.
TRIO-CINEMA 1 UCB, 2/08/2010 ACS Dave Auslander, Dave Pankow, Han Chen, Yao-Ting Mao, UC Berkeley Space Sciences Laboratory University of California, Berkeley.
Lab 3: Earth Sun-Geometry
Temperature dependency of ACC data TUD provides all available GPS-derived linear accelerations to VZLU End of January – end of May To be used for validation.
Magnetic Measurement Expert Group10-11 March 2016Warsaw / PL MAGNETOMETER – STAR-IMAGER ALIGNMENT: APPARENT EULER ANGLE VARIATION DUE TO MAGNETOSPHERIC.
Summary of Session 2M Swarm 5th Data Quality Workshop
ACC/GPSR Splinter Summary
Solar Energy to Earth and the Seasons
The 3rd Swarm Science Meeting, June 2014, Copenhagen, Denmark
The Instruments Faraday Cup CfA/U of Mich & MIT
Adjustment of Trilateration
The Swarm Advanced stellar Compass
Rapid core field variations just before Swarm
Summary of part of L2 session
Optical Bench Anomaly Investigation and Modelling
Winter Sky – Facing North
you thought of going into teaching?”
swarm End-To-End Mission Performance Study Working meeting on Task 2
Earth’s Seasons.
Mac Keiser and Alex Silbergleit
Image Stabilization System (ISS)
RELATIVE MOTION OF EARTH IN SOLAR SYSTEM
Earth in Space Seasons.
New "quite time" concept: application to Champ lithospheric field modelling Nils Olsen, Jesper Gjerløv & Co.
Swarm Magnetic Package Calibrations Way Forward
Orbit in Space Coordinate Frames and Time
Mac Keiser and Alex Silbergleit
Sun-Earth System.
Launch and On-orbit Checkout
Tilt of the Earth’s Rotational Axis
The Sky (Celestial Sphere)
Chapter 6 Less 2 Earth in Space
In flight calibration of the experimental ASM vector mode on board the Swarm satellites Thomas Jager, François Bertrand, Viviane Cattin & Jean-Michel.
Thermodynamics Atmosphere
Outline Construction of gravity and magnetic models Reference models
I. Earth’s Place in Space
Presentation transcript:

Magnetic Splinter Meeting

ASM inter-satellite comparison

VFM calibration: Swarm A residual analysis in-flight determination of 18 VFM parameters, including temperature dependencies

Model of VFM perturbation field (responsible for ASM-VFM residuals) Determining the Sun vector Ecliptic Plane Earth Spin (23.5˚) Summer Solstice X Z Spacecraft Quaternion Inertial Space Ecliptic Plane Sun Aligned 𝑣 𝑠𝑢𝑛 = 𝑞 𝑠/𝑐 −1 𝑡 ∙ 𝑀 𝐶𝐼𝑆 −1 𝑡 ∙ 𝑀 𝐸𝑂 −1 ∙ 𝑀 𝑆𝐴 −1 𝑡 ∙ 𝑛 𝑥 Sun vector in baffle Max sun absorption angle 𝑣 𝑏𝑎𝑓 = 𝑟 𝜃 𝜑 = 𝑠𝑖𝑛 𝛼 0 𝑐𝑜𝑠 𝛼 0 1 0 𝑐𝑜𝑠 𝛼 0 −𝑠𝑖𝑛 𝛼 ∙ 𝑣 𝑠𝑢𝑛 𝛼=70° Flight direction Baffle Heat model 𝐵𝑎𝑓 𝑚𝑜𝑑𝑒𝑙 = 0 𝑒𝑐𝑙𝑖𝑝𝑠𝑒 0 𝜃<0 𝑠𝑖𝑛 4 𝜑 ∙ 𝑠𝑖𝑛 4 𝜃 𝑒𝑙𝑠𝑒

Comparing Model predictions with observations Measurements Simulation

Kursk anomaly against MF7 100 90 MF7 degree 60

Kursk anomaly against MF7: gradients } 100 0.2 nT 90 MF7 degree 60

NGDC Main field model (based on NEC data) Swarm B residuals with MF7 subtracted X Y Z rms = 6.4 nT rms = 12.7 nT rms = 3.2 nT

BGS Field Modelling (based on NEC data) Swarm Z misfits Misfit statistics Satellite mean std dev X -0.42 30.47 Y -0.04 21.48 Z 0.75 19.92 Observatory X -0.07 5.96 Y -0.07 3.77 Z -0.06 3.73

Euler angle determination, 3 day, adjusted offsets X axis looks fine Y axis: Swarm A drifting off at about 1 arcsec/10 days Z axis Swarm B: 25 arcsec shift. Does toroidal magnetic field change by 8 nT with altitude?

Field Modeling and Euler angle estimation (based on VFM + STR data) sun lower than +10 above horizon

Variation of inter-boresight angle, Swarm C

Summary ASM-VFM perturbation VFM calibration “empirical model” (GFZ) “engineering model” (DTU) Provide perturbation model predictions Merging of the two models ASM vector data: Provision of more data for Cal/Val activities VFM calibration Estimate VFM parameters using night/corrected data (ESA) … after applying empirical correction from GFZ … after applying “engineering model” prediction from DTU Co-estimation of perturbation model and VFM calibration parameters Updated L1b data with new Euler angles Replace pre-flight values with in-flight determined (which?) ones IGRF team needs updated L1b data by 1 August 2014 for IGRF determination Need for more information (e.g on flags, “ASM-VFM perturbation” tasks, …) data rejection based on which flags / thresholds Sharing of information, coordination, documentation of data sets

Estimation of static Euler angles (DTU) “dark regions”, but including “twilight data”: sun lower than +10 above horizon SW-A SW-B SW-C a 11.8042 -8.8847 1.8130 b -76.1903 -76.4266 -76.8269 g -12.5736 9.1141 -1.9789 In-flight (degrees): SW-A SW-B SW-C a 11.8294 -8.9132 1.7931 b -76.1904 -76.4241 -76.8270 g -12.5941 9.1525 -1.9536 Pre-flight (degrees): SW-A SW-B SW-C Da 23.2 -25.1 -16.3 Db 4.6 4.9 0.2 Dg 14.6 38.8 21.1 Difference (arcsecs)

Estimation of static Euler angles (GFZ) SW-A SW-B SW-C a 11.8237 -8.8947 1.7727 b -76.1848 -76.4171 -76.8229 g -12.5827 9.1799 -1.9386 In-flight (degrees): SW-A SW-B SW-C a 11.8294 -8.9132 1.7931 b -76.1904 -76.4241 -76.8270 g -12.5941 9.1525 -1.9536 Pre-flight (degrees):