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Gravity Field and Steady-State Ocean Circulation Explorer (GOCE) satellite was designed and operated by the European Space Agency with the aim of mapping the Earth’s gravity field with high accuracy and spatial resolution. This report is focused on the modeling, simulation and syntesis of the Drag-Free and Attitude Control System (DFACs), system to counteract the atmospheric drag to delete the non gravitational components from the gradiometer measurement. Co-Authors: Bassissi Enrico Colombo Alessandro De Luca Maria Alessandra
The Gravity Field and Steady-State Ocean Circulation Explorer (GOCE) of the European Space Agency was launched on 17th March 2009, with the purpose of providing an accurate model of Earth’s gravity field through gravity gradiometry and precise orbit determination techniques. To obtain a sufficiently strong gravity field signal, GOCE was set on a near-polar sun-synchronous orbit at a very low altitude of about 260 km, at which atmospheric drag perturbation is significant. For this reason the spacecraft is specifically designed to minimise air drag impact and possesses the capability to counteract it, in order to maintain the nominal orbit and cancel out non-gravitational forces. GOCE is equipped with a Drag Free Attitude and Orbit Control System (DFACS) that provides 3 axis stabilized attitude. The problem requires the modeling of the simplified orbital mechanics, accelerometer, flow control valve and ion thruster subsystem dynamics. Control loop dynamics is simulated. System response is studied in nominal and off-nominal conditions. Finally, some parameters are optimised through a genetic algorithm minimization process.
Proceedings of the 41st IEEE Conference on Decision and Control, 2002., 2002
The paper gives an overview of the attitude and drag-free control (in short DFC) of the European Gravity Field and Ocean Circulation Explorer (GOCE) satellite. The DFC has been designed and tested in view of the Preliminary Design Review (PDR). The DFC is intended to enable the operations of a gravity gradiometer for the Earth gravity field recovery. The DFC has been fully designed on a simplified discrete-time model derived from the 'fine' dynamics of the spacecraft and its environment, as outlined in a companion paper. The DFC has been tested against severe uncertainties and its code has been integrated into GOCE end-to-end simulator.
Proceedings of the 18th IFAC World Congress, 2011
The Gravity and steady state Ocean Circulation Explorer (GOCE) is the first Earth Explorer Core Mission of ESA's Living Planet Program. The scientific objectives of GOCE are the determination of the Earth's steady state gravity field anomalies with an accuracy of 1x10-5 m/s 2 , and the determination of geoid heights with accuracy between 1 to 2 cm, at length scales down to 100 km. To meet the scientific objectives, GOCE flies in a Sun-synchronous orbit with altitude in the range 250÷280km, and it carries out two measurements: gravity gradients by the Electrostatic Gravity Gradiometer, and Precise Orbit Determination based on Global Positioning System data. An essential element for meeting the mission requirements is the Drag Free and Attitude Control (DFAC) using an ion engine for compensating the along track non-gravitational forces and a set of magnetic torquers for attitude control. The drag-free control has the task of realizing a virtual environment reducing the non-gravitational linear accelerations (from that the name drag-free) below a threshold compatible with the accelerometer dynamic range and with the gradiometric performance. For the same reason, the attitude control must constrain the angular accelerations and the angular rates. The mission induces requirements not only on the magnitude of the residual linear and angular accelerations, angular rate and attitude errors, but also on their spectral density in the science measurement bandwidth of [5,100] mHz. GOCE is the first European drag-free mission and the first pure magnetic attitude control system for a medium-sized Low Earth Orbit scientific satellite (about 1 ton mass). The control design has been done following already well known approaches with the introduction of customizations to cope with specific performance requirements, design simplicity and programmatic constraints. After a short presentation of the GOCE mission architecture, of the satellite and of the payload, the paper presents the main aspects of the DFAC scientific mode and its in-flight performances.
Conference on Decision and Control, 2002
The paper gives an overview of the attitude and drag-free control (in short DFC) of the European Gravity Field and Ocean Circulation Explorer (GOCE) satellite. The DFC has been designed and tested in view of the Preliminary Design Review (PDR). The DFC is intended to enable the operations of a gravity gradiometer for the Earth gravity field recovery. The DFC
2008
The paper concerns Drag-Free and Attitude Control of the European satellite Gravity field and steady-state Ocean Circulation Explorer (GOCE) during the science phase. Design has followed Embedded Model Control, where a spacecraft/environment discrete-time model becomes the realtime control core and is interfaced to actuators and sensors via tuneable feedback laws. Drag-free control implies cancelling non-gravitational forces and all torques, leaving the satellite to free fall subject only to gravity. In addition, for reasons of science, the spacecraft must be carefully aligned to the local orbital frame, retrieved from range and rate of a Global Positioning System receiver. Accurate drag-free and attitude control requires proportional and low-noise thrusting, which in turn raises the problem of propellant saving. Six-axis drag-free control is driven by accurate acceleration measurements provided by the mission payload. Their angular components must be combined with the star-tracker attitude so as to compensate accelerometer drift. Simulated results are presented and discussed. he contributed to data reduction of the European astrometric mission Hipparcos. Technological studies in view of scientific and drag-free space missions, like Gaia and GOCE provided the opportunity of applying Embedded Model Control to drag-free satellites and to electro-optics. He contributed to the conception, design and implementation of the interferometric thrust-stand Nanobalance, capable of sub-micro-Newton accuracy. His research interests cover the entire field of control problems that are challenging because of complexity, uncertainty and precision.
Acta Astronautica, 2009
This paper concerns the drag-free and attitude control (DFAC) of the European Gravity field and steady-state Ocean Circulation Explorer satellite (GOCE), during the science phase. GOCE aims to determine the Earth's gravity field with high accuracy and spatial resolution, through complementary space techniques such as gravity gradiometry and precise orbit determination. Both techniques rely on accurate attitude and drag-free control, especially in the gradiometer measurement bandwidth (5mHz to 100mHz), where non-gravitational forces must be counteracted down to micronewton, and spacecraft attitude must track the local orbital reference frame with micro-radian accuracy. DFAC aims to enable the gravity gradiometer to operate so as to determine the Earth's gravity field especially in the so-called measurement bandwidth (5mHz to 100mHz), making use of ion and micro-thruster actuators. The DFAC unit has been designed entirely on a simplified discrete-time model (Embedded Model) derived from the fine dynamics of the spacecraft and its environment; the relevant control algorithms are implemented and tuned around the Embedded Model, which is the core of the control unit. The DFAC has been tested against uncertainties in spacecraft and environment and its code has been the preliminary model for final code development. The DFAC assumes an allpropulsion command authority, partly abandoned by the actual GOCE control system because of electric micropropulsion not being fully developed. Since all-propulsion authority is expected to be imperative for future scientific and observation missions, design and simulated results are believed to be of interest to the space community.
… of the 2002 International Conference on, 2002
High precision mapping of the geoid and the Earth's gravity field are of importance to a wide range of ongoing studies in areas like ocean circulation, solid Earth physics and ice sheet dynamics. Using a satellite in orbit around the Earth gives the opportunity to map the Earth's gravity field in 3 dimensions with much better accuracy and spatial resolution than ever accomplished. To reach the desired quality of measurements, the satellite must fly in a low Earth orbit where disturbances from atmospheric drag and the Earth's magnetic field will perturb the satellite's motion. These effects will compromise measurement accuracy, unless they are accurately compensated by onboard thrusters. The paper concerns the design of a control system to performing such delicate drag compensation. A six degrees-of-freedom model for the satellite is developed with the model including dynamics of the satellite, sensors, actuators and environmental disturbances to the required micro-Newton accuracy. A control system is designed to compensate the non-gravitational disturbances on the satellite in three axes using an H ∞ design. Performance is validated against mission requirements.
International Association of Geodesy Symposia, 2001
GOCE (Gravity Field and Steady-State Ocean Circulation Explorer) is one of the four selected ESA Earth Explorer Missions. The main objective of GOCE is the determination of the Earth's gravity field with high spatial resolution and with high homogeneous accuracy. For this purpose, two observation concepts will be realised. Satellite-to-Satellite Tracking (SST) in high-low mode will be used for the orbit determination and for the retrieval of the long-wavelength part of the gravity field. Satellite Gravity Gradiometry (SGG) will be employed for the derivation of the medium/short-wavelength parts of the gravity field.. For the realisation, a GPS receiver, a 3-axis gradiometer and auxiliary instruments are needed; e.g. star trackers to control the orientation of the spacecraft or thrusters for attitude and drag-free control. Each instrument exhibits, its own error behaviour which affects the measurements and the final products in some typical way. The SID consortium consists of three organisations: the Institut für Astronomische und Physikalische Geodäsie (IAPG), Delft Institute for Earth-Oriented Space Research (DEOS) and the Space Research Organization Netherlands (SRON). They have the goal to provide a reliable error budget for the GOCE system, identify it's weaknesses and limitations and make a complete error analysis of the whole mission. A complete simulator of the gradiometer has been developed. The simulator describes the test mass motion as a mass-spring system. The output are gravity gradients (V ij out) as if they were measured, based on input gravity accelerations, S/C position, orientation and disturbing forces. The corresponding error PSD's (Power Spectral Densities) representing the effect of different error sources are computed. The PSD's are propagated to spherical harmonic error spectra, geoid heights and gravity anomaly accuracies to assess effects of instrument and measurement errors on gravity field determination. The different tasks within the consortium are described by means of a flow chart.
SpaceOps 2012 Conference, 2012
ESA's Gravity Field and Steady-State Ocean Circulation Explorer (GOCE) is operated in an extremely low Earth orbit at 260 km altitude. The spacecraft has an aerodynamic shape and employs drag-free control with an ion propulsion system to counteract the atmospheric drag. GOCE's extraordinary mission profile and spacecraft design led to many peculiarities for flight operations. The experience gained after launch has resulted in a significant evolution of the flight operations approach. Changes include a revised approach for orbit control manoeuvres, a new altitude selection owing to the low level of solar activity, and the decision to not interrupt science operations in eclipse season. Flight operations in 2010 were particularly challenging due to severe anomalies in the on-board data handling subsystem. Most notably, the spacecraft had to be operated "in the blind" with little to no status information for a period of about 1.5 months. This paper presents the experience gained when operating GOCE, describing the evolution of the flight operations approach and ground segment. I. The GOCE Mission he Gravity Field and Steady-state Ocean Circulation Explorer (GOCE) was selected in 1999 as the first Earth Explorer Core Mission of ESA's Living Planet Programme. After nearly a decade of development, GOCE was launched on 17 th March 2009. A. Mission Overview GOCE's scientific objective is to measure the Earth's gravity field and to provide a model of the geoid with unprecedented accuracy, determining gravity field anomalies with an accuracy of 1 mGal (or 10 −5 m/s 2), and the geoid to an accuracy of 1 to 2 cm at a spatial resolution of 100 km. The high accuracy expected for GOCE's gravity field model is in particular essential for precise determination of ocean circulation. GOCE data will also be useful for leveling by GPS, navigation, continental lithosphere studies and for global unification of height systems, e.g. to establish a global sea-level monitoring system. GOCE is the first spacecraft employing the concept of gradiometry, i.e. the measurement of acceleration differences over short baselines between proof masses of a set of accelerometers of the Electrostatic Gravity Gradio
Remote Sensing
The Next Generation Gravity Mission (NGGM), currently in a feasibility study phase as a candidate Mission of Opportunity for ESA-NASA cooperation in the frame of the Mass Change and Geo-Sciences International Constellation (MAGIC), is designed to monitor mass transport in the Earth system by its variable gravity signature with increased spatial and temporal resolution. The NGGM will be composed by a constellation of two pairs of satellites, each providing the measurement of two quantities from which the map of Earth’s gravity field will be obtained: the variation of the distance between two satellites of each pair, measured by a laser interferometer with nanometer precision; and the relative non-gravitational acceleration between the centers of mass of each satellite pair, measured by ultra-sensitive accelerometers. This article highlights the importance of the second “observable” in the reconstruction of the lower harmonics of Earth’s gravity field, by highlighting the tight contro...
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