• 한국항공운항학회지
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• 제19권4호
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• pp.30-36
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• 2011

Inertial navigation systems requires gravity model to compute gravity acceleration and its trajectory accuracy depends on the gravity model accuracy especially for a long range flight. The gravity model accuracy is important for satellite orbit prediction as well. The precision gravity model requires a precision coordinate transformation between inertial and Earth fixed coordinates. Precision gravity acceleration algorithms with a coordinate transform are studied and a computer program is developed. The effects of individual model components on trajectory error are analyzed.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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• pp.1236-1238
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• 2003

The Earth's total magnetic field was extracted from on board TAM (Three Axis Magnetometer) observations of KOMPSAT-1 satellite between June 19th and 21st, 2000. In the pre-processing, the TAM's telemetry data were transformed from ECI (Earth Centered Inertial frame) to ECEF (Earth Centered Earth Fixed frame) and then to spherical coordination, and self-induced magnetic field by satellite bus itself were removed by using an on-orbit magnetometer data correction method. The 2-D wavenumber correlation filtering and quadrant-swapping method were applied to the pre-processed data in order to eliminate dynamic components and track-line noise, respectively. Then, the spherical harmonic coefficients are calculated from KOMPSAT-1 data. To test the validity of the TAM's geomagnetic field, Danish/NASA/French ${\phi}$rsted satellite's magnetic model and IGRF2000 model were used for statistical comparison. The correlation coefficient between ${\phi}$rsted and TAM is 0.97 and IGRF and TAM is 0.96. It was found that the data from on board magnetometer observations for attitude control of Earth-observing satellites can be used to determinate the Earth's total magnetic field and that they can be efficiently used to upgrade the global geomagnetic field coefficients, such as IGRF by providing new information at various altitudes with better temporal and spatial coverage.

• Journal of Positioning, Navigation, and Timing
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• 제13권2호
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• pp.189-197
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• 2024

Galileo is a European Global Navigation Satellite System (GNSS) that has offered the Galileo Open Service since 2016. Consequently, the standardization of GNSS augmentation systems, such as Satellite Based Augmentation System (SBAS), Ground Based Augmentation System (GBAS), and Aircraft Based Augmentation System (ABAS) for Galileo signals, is ongoing. In 2023, the European Union Space Programme Agency (EUSPA) released prior probabilities of a satellite fault and a constellation fault for Galileo, which are 3×10^-5 and 2×10^-4 per hour, respectively. In particular, the prior probability of a Galileo constellation fault is significantly higher than that for the GPS constellation fault, which is defined as 1×10^-8 per hour. This raised concerns about its potential impact on GBAS integrity monitoring. According to the Global Positioning System (GPS) Standard Positioning Service Performance Standard (SPS PS), a constellation fault is classified as a wide fault. A wide fault refers to a fault that affects more than two satellites due to a common cause. Such a fault can be caused by a failure in the Earth Orientation Parameter (EOP). The EOP is used when transforming the inertial axis, on which the orbit determination is based, to Earth Centered Earth Fixed (ECEF) axis, accounting for the irregularities in the rotation of the Earth. Therefore, a faulty EOP can introduce errors when computing a satellite position with respect to the ECEF axis. In GNSS, the ephemeris parameters are estimated based on the positions of satellites and are transmitted to navigation satellites. Subsequently, these ephemeris parameters are broadcasted via the navigation message to users. Therefore, a faulty EOP results in erroneous broadcast ephemeris data. In this paper, we assess the conventional ephemeris fault detection monitor currently employed in GBAS for wide faults, as current GBAS considers only single failure cases. In addition to the existing requirements defined in the standards on the Probability of Missed Detection (PMD), we derive a new PMD requirement tailored for a wide fault. The compliance of the current ephemeris monitor to the derived requirement is evaluated through a simulation. Our findings confirm that the conventional monitor meets the requirement even for wide fault scenarios.

• 자원환경지질
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• 제37권4호
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• pp.401-411
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• 2004

다목적위성 아리랑 1호(KOMPSAT-1)에 장착된 본체 자세제어용 삼축자력계(TAM) 자료로부터 2000년 6월 19일에서 21일 사이의 지구자기장을 추출하였다 전처리과정으로 관측자료를 지구관성좌표계에서 지구고정좌표계로 변환시킨 후, 이를 다시 구면좌표계로 변환하였고, 지구자기장의 영향이 아닌 위성체 내의 전류에 의한 유도자기장은 자기장의 대칭성을 이용하여 제거하였다. 지구 외적 요인에 의한 자기장의 영향을 제거하기 위해 위성 궤도를 상향 및 하향 두 그룹으로 분류한 후, 2차원 파동수대비법을 이용해 두 그룹 사이에 서로 역으로 대비되는 성분을 제거하였다. 측선 잡음을 제거를 위하여 파동수영역에서 사분면교환법을 도입하였고, 이로부터 삼축자력계 관측값으로부터 최증적인 지구자기장을 추출하였다. TAM 자기장의 검증을 위해 다목적위성과 비슷한 시기에 유사한 고도에서 지구자기장을 전문적으로 측정한 ${\phi}$rsted로부터 유도된 지구자기장 및 IGRF2000모델과 비교한 결과 이들 사이의 상관계수는 각각 0.97과 0.96으로 매우 높게 나타났다. 끝으로 이 연구에서 추출한 지구자기장으로부터 구면조화계수를 degree & order 19까지 계산한 후 이를 IGRF ${\phi}$rsted와 Champ 모델과 비교하였다. 이 연구에 의해 일반적인 지구관측위성의 자세보정용 자력계로부터 degree & order 5까지 신뢰성있는 지구자기장의 추출이 가능함은 밝혀졌고, 이로부터 이 연구의 자료처리과정을 도입하면 지구자기장 전문관측위성이 존재하지 않는 기간은 물론 관측이 존재하지 않는 고도에 대한 지구자기장의 추출이 가능하게 되었고 이로부터 전지구 자기장 모델의 저주파 성분을 향상시킬 수 있음이 밝혀졌다.