2019
DOI: 10.1007/s40295-019-00192-1
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A Bi-quintic Latitude/Longitude Spline and Lunar Surface Modeling for Spacecraft Navigation

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Cited by 4 publications
(5 citation statements)
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“…The simulation enables testing of different combinations of ground station arrays, ionosphere error models, and other parameters. Computation for an N e ( r ) electron density truth model utilizes a Chapman profile that is fit to an IRI model for a particular time (Psiaki et al., 2015). A similar procedure is used to generate an a priori estimate of the ionosphere parameter vector for use in the batch filter's cost function.…”
Section: Preliminary Resultsmentioning
confidence: 99%
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“…The simulation enables testing of different combinations of ground station arrays, ionosphere error models, and other parameters. Computation for an N e ( r ) electron density truth model utilizes a Chapman profile that is fit to an IRI model for a particular time (Psiaki et al., 2015). A similar procedure is used to generate an a priori estimate of the ionosphere parameter vector for use in the batch filter's cost function.…”
Section: Preliminary Resultsmentioning
confidence: 99%
“…See Psiaki et al. (2015) on the Chapman parameter fitting procedure. The resulting 365 × 4 = 1,460 parameter vectors were used to compute a covariance matrix for p , i.e., for the natural logarithm and natural logarithm partial derivatives of all three Chapman model parameters at the spline nodes.…”
Section: Earth and Ionosphere Modelsmentioning
confidence: 99%
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“…Spline nodes were placed at predefined latitudes and longitudes along circles of constant latitude. Additional information on spline computations, spline stored data, and nodes placement is provided in Baumgarten et al (2021), Baumgarten (2018), andPsiaki et al (2019).…”
Section: Earth and Ionosphere Modelsmentioning
confidence: 99%
“…The three-dimensional ionosphere model is defined by the three Chapman vertical profile parameter values' natural logarithms at each of the latitude/longitude nodes along with all of their latitude and longitude partial derivatives of up to second order in latitude, longitude, or both. This parameterization and its calculation from the IRI model are described in Psiaki et al (2015Psiaki et al ( , 2019. It should be noted that the Chapman model ignores the possibility of distinct D and E layers, including a sporadic E layer.…”
Section: Truth-model Simulationmentioning
confidence: 99%