1971
DOI: 10.1029/jb076i032p07844
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A second-order Markov Gravity Anomaly Model

Abstract: A second‐order Markov process is proposed as a statistical model for gravity anomalies in a local region. The method is applied to the analysis of errors in an inertial navigation system caused by unknown gravity phenomena. Statistical models of vertical deflection obtained from the anomaly model by means of the Vening Meinesz equations yield predictions of rms position and velocity errors for the navigation system. Actual vertical deflection data are used as simulated inputs to a computer model of an inertial… Show more

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Cited by 49 publications
(15 citation statements)
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“…The distribution of the ice sheet data and the majority of was used to generate the DEM from the data [Kasper, 1971]. This approach has been shown to be effective for elevation modeling as it takes into account variations in data accuracy in the determination of the weighting matrix so that the detail in the DEM reflects the local data quality [Ekholm, 1996].…”
Section: Dem Generationmentioning
confidence: 98%
“…The distribution of the ice sheet data and the majority of was used to generate the DEM from the data [Kasper, 1971]. This approach has been shown to be effective for elevation modeling as it takes into account variations in data accuracy in the determination of the weighting matrix so that the detail in the DEM reflects the local data quality [Ekholm, 1996].…”
Section: Dem Generationmentioning
confidence: 98%
“…Position reference errors are modeled as biases by t,he equations 2 Other more complicated models are often used also [10]- [12].…”
Section: Evaluatim By Covariance Simulationmentioning
confidence: 99%
“…6, , 6, Kort,h, east vertica.1 deflection component,s.The 3. angles are small misalignment angles bet,ween the platform and computer and they obey t.he differential equations $ n = -Q sin L+e + en(12) $, = D sin L#n + Q cos L#2 + e,…”
mentioning
confidence: 99%
“…For local models, the earth is assumed to be flat. The popular models used to represent either gravity or anomalous potential autocovariance function are self‐consistent planar covariance models, namely the familiar class of Markov models (Shaw et al 1969; Kasper 1971; Jordan 1972), Poisson and reciprocal distance covariance models (Nash & Jordan 1978), the planar logarithm covariance model (Forsberg 1987). However, except the planar logarithm covariance model, these models fail to produce the correct asymptotic decay of the power spectral density at high spatial frequencies.…”
Section: Introductionmentioning
confidence: 99%