2010
DOI: 10.1029/2010gc003026
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An ellipsoidal harmonic representation of Earth's lithospheric magnetic field to degree and order 720

Abstract: [1] While high-degree models of the Earth's gravity potential have been inferred from measurements for more than a decade, corresponding geomagnetic models are difficult to produce. The primary challenge lies in the estimation of the magnetic potential, which is not completely determined by available field intensity measurements and cannot be computed by direct integration. Described here is the methodology behind the third generation of the National Geophysical Data Center's degree 720 magnetic model. Key iss… Show more

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Cited by 108 publications
(85 citation statements)
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“…The main field at PALA was estimated by using the global Enhanced Magnetic Model (EMM) up to degree and order 15. This geomagnetic model up to degree of 720 is derived from ground, satellite, marine and aeromagnetic data (Maus, 2010), and the lithospheric field in this model is described by degrees and orders of 16-720.…”
Section: Methods Of Analysismentioning
confidence: 99%
“…The main field at PALA was estimated by using the global Enhanced Magnetic Model (EMM) up to degree and order 15. This geomagnetic model up to degree of 720 is derived from ground, satellite, marine and aeromagnetic data (Maus, 2010), and the lithospheric field in this model is described by degrees and orders of 16-720.…”
Section: Methods Of Analysismentioning
confidence: 99%
“…where B m is the Earth's magnetic field strength, andα and γ are the values of magnetic declination and inclination, respectively, obtained from the EMM2010 Earth magnetic model [12]. Because they are otherwise not observable, updating of the corresponding biases, b α and b γ , is only allowed when a vision-aiding measurement is available.…”
Section: A Pose Estimation Processmentioning
confidence: 99%
“…Unfortunately, it is also one of the weakest detectable sources at satellite altitudes and is masked by all other constituents of the total Earth's magnetic field (e.g., Hulot et al, 2007). For instance, it represents about 0.01% of the total Earth's magnetic field strength at 400 km height (with a root mean square of about 3.8 nT using the NGDC-720 model; Maus, 2010) and its magnitude rarely exceeds 20 nT.…”
Section: Introductionmentioning
confidence: 99%