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dc.contributor.authorCravens, Thomas
dc.date.accessioned2023-02-11T20:37:24Z
dc.date.available2023-02-11T20:37:24Z
dc.date.issued2023-02-11
dc.identifier.urihttp://hdl.handle.net/1808/33778
dc.descriptionThe spacecraft magnetometer data and Fourier transforms of this data are contained in the attached Excel files and were used for the J. Geophysical Research paperen_US
dc.description.abstractThe two main sources of magnetic field for the Martian ionosphere are the solar wind magnetic fields (i.e., the interplanetary magnetic field), and, particularly in the southern hemisphere, remnant crustal magnetization. The magnetic fields measured in the ionosphere by the magnetometers onboard the Mars Atmosphere and Volatile EvolutioN (MAVEN) spacecraft and the Mars Global Surveyor (MGS) display a wide range of spatial scales. In this paper we use a Fourier analysis of the magnetic field to quantify the field strength as a function of scale-size. Fourier analysis represents a function of time (or some other variable) as the sum over a wide range of sinusoidal functions of different frequencies. We find that results of the Fourier analysis for the ionospheric magnetic field have much in common with the Fourier analysis of the interplanetary magnetic field. The paper exploits this similarity to probe the sources of the ionosphere’s magnetic structure.en_US
dc.description.sponsorshipNASA MAVENen_US
dc.subjectPlanetary Ionospheresen_US
dc.subjectMarsen_US
dc.subjectmagnetic fielden_US
dc.titleFourier Analysis of Magnetic Fields in the Ionosphere of Marsen_US
dc.typeDataseten_US
kusw.kuauthorCravens, Thomas
kusw.kudepartmentPhysics and Astronomyen_US
dc.rights.accessrightsopenAccessen_US


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