Multirate sampling and generalized alias as a source of errors in magnetometer experiments.
Multirate sampling and generalized alias as error source in spacecraft magnetometer experiments
Engineering topics
Publications and source records attributed to Sonett, C. P..
Multirate sampling and generalized alias as error source in spacecraft magnetometer experiments
Solar wind induced planetary magnetic field systems supportable by bodies free of electrically insulating atmospheres and dynamo driven intrinsic magnetic fields
Interplanetary magnetic field reconnection at tangential discontinuities, discussing coincidence with proton temperature maxima in solar wind during magnetic storm
Geomagnetic tail configuration and reconnection data from Explorer 33 satellite, noting skewing of field lines
Mathematical model to establish planet properties as unipolar electric generator
Unipolar induction mechanism for electrical field profiles calculation of moon interior
Geomagnetic tail topology, reconnection and interaction with moon from Explorer 33 satellite data
Diamagnetic solar wind cavity behind moon discovered by magnetometer data from lunar orbiter
Magnetometer observations of magnetic field near moon during orbits of Explorer satellite
Impact of solar wind on lunar unipolar generator, investigating generation of two current systems
Explorer 33 data used to assess geometry and lunar interaction of geomagnetic tail
Discontinuities in plasma parameters of solar wind satisfy conditions of Mhd and can be treated as shock waves and stationary contact surfaces
Mariner II interplanetary magnetic field measurements
Evidence for collision-free hydromagnetic shock in interplanetary space
Correction of magnetic measurements made by Mariner II, noting use of second-order approximation for interplanetary magnetic field
Collision-free hydromagnetic shock observed simultaneously in interplanetary space on October 7, 1962 by Mariner II and Explorer XIV
Spacecraft rotation effect on measurement of hydromagnetic radiation in solar wind
Worldwide positive-negative impulse pair observed on geomagnetic records found to be recurrent and associated with M-region disturbances