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Using a set of 112 magnetopause locations selected from those obtained in recent years with the aid of Imp satellites on the dayside of the magnetosphere over 0600-1800 LT, extended results are presented on the problem of geomagnetic micropulsation periods in relation to magnetospheric parameters. These results include the finding that the two groups represented by micropulsation period ranges from 20 to 40 sec and from 40 to 80 sec, respectively, have a completely different dependence on the radial distance of the magnetopause from satellite experiments.

Explorer 33 observations of sudden impulses propagating in geomagnetic tail and magnetosheath

Diagnostic analysis of magnetosphere based on resonating regions of plasmasphere, outer magnetosphere, and magnetospheric tail

Sudden impulses in geomagnetic field, discussing synchronous equatorial orbit-satellite magnetometer observations

Geomagnetic field boundary observations by Explorer XII

Magnetosheath field, geomagnetic activity index, magnetopause stability and interplanetary magnetic field influence on magnetospheric phenomena

Long period hydromagnetic waves in magnetosphere and coupling to solar wind studied by Explorer XIV

LF hydromagnetic waves in magnetosphere using Explorer XII magnetometer observation

The governing equations for an unsteady turbulent boundary layer on a swept infinite cylinder, composed of a continuity equation, a pair of momentum equations and a pair of turbulent energy equations which include upstream history efforts, are solved numerically. An explicit finite difference analog to the partial differential equations is formulated and developed into a computer program. Calculations were made for a variety of unsteady flows in both two and three dimensions but primarily for two dimensional flow fields in order to first understand some of the fundamental physical aspects of unsteady turbulent boundary layers. Oscillating free stream flows without pressure gradient, oscillating retarded free stream flows and monotonically time-varying flows have all been studied for a wide frequency range. It was found that to the lowest frequency considered, the lower frequency bound being determined by economic considerations (machine time), there were significant unsteady effects on the turbulent boundary layer.

Explorer 33 magnetic field observations have been analyzed to study the propagation of sudden impulses (si) in the geomagnetic tail and the magnetosheath. Average speed of propagation in these regions is 760 km per sec with a range of 550-1230 km per sec. Most of the si's have a propagation speed which is close to that of the shock wave observed in this region. Positive si is shown to have a positive change in the tail or magnetosheath and a negative si has a similar negative change. Nine out of thirteen correlated si's have their origin in the solar wind continuities, while four si's have possible origin in the perturbations of tail or magnetosheath field.