The boundary region of the geomagnetic field.
Survey of geomagnetic field boundary data obtained from magnetic field, energetic corpuscular radiation and plasma measurements
Engineering topics
Publications and source records attributed to Coleman, P. J., Jr..
Survey of geomagnetic field boundary data obtained from magnetic field, energetic corpuscular radiation and plasma measurements
Data obtained by the magnetometer carried by the mariner ii space probe
Mariner ii space probe - preliminary observation
Mariner ii magnetometer data analysis indicates persistent interplanetary magnetic field
Low-frequency hydromagnetic waves in geomagnetic field - data obtained from magnetometer, aspect indicator and scintillation counter on explorer 6 satellite
Low frequency hydromagnetic waves in distant geomagnetic field - explorer vi satellite
Interplanetary magnetic fields - mariner ii observations
In the adjoining letter, Dessler [1961] argues that the interface between the solar wind and the geomagnetic field is stable and cannot, therefore, generate hydromagnetic waves. According to our interpretation, his argument may be paraphrased as follows: He observes that, for many sudden commencement geomagnetic storms, surface magnetograms show no marked change in the level of disturbances from the period before the sudden commencement until well into the initial phase of the storm. He applies the attenuation factors calculated by Francis and Karplus [1960] to the measurements of the 1 cps component of the magnetic disturbances obtained at the surface. From this calculation, he concludes that, during the initial phase of these geomagnetic storms, the amplitudes of hydromagnetic disturbances above the ionosphere are less than 1. Assuming that the sudden commencement indicates the presence of a solar wind, he further concludes that hydromagnetie disturbances are not generated in the region between the geomagnetic field and the solar wind and that this interface is, therefore, inherently stable. He subsequently accounts for the hydromagnetie disturbances which are frequently observed at the earth as having been produced by fluctuations in the energy density of the impinging solar wind.