Equatorial longitude and local time variations of topside magnetic field‐aligned ion drifts at solar minimum
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Diurnal and latitude variations in zenith nightglow intensity
Jupiter Red Spot coordinate measurement from recent plates
Diurnal and latitudinal variations in 6300 angstrom nightglow intensity determined along Pacific coast of South America, noting relation between location of antisolar point and equatorial midnight enhancement
Diurnal and latitudinal variations in 5577 angstrom zenith nightglow intensity compared with 6300 angstrom calibrations
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Computer approach to first order planetary theory using perturbation calculation in rectangular coordinates
Low degree earth gravity harmonics effect on 12 and 24 hour orbits of high altitude communications satellites
Jupiter Red Spot semiregular oscillations from photographic measurements, determining mean period and amplitude
Tracking data reduction to geopotential accelerations for satellites
Radar scattering law derivation method for small regions of Venus surface, synthesizing CW spectra
The data obtained indicate that the formaldehyde is concentrated in distinct clouds to a much greater extent than atomic hydrogen. The findings suggest that most of the mass in these clouds is in the form of molecular hydrogen. The locations of four dominant clouds are reported. The strongest formaldehyde features are apparently associated with the galactic nucleus. Estimates of the hydrogen density in the clouds, based on the assumption of stability and also on a comparison with local dark clouds, indicate a number density in the range from 1000 to 10,000 per cc, and a mass of approximately 500,000 solar masses.
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Detailed particle observations from various Pioneer spacecraft located at different heliolongitudes during the complex solar flare events of Mar. 30 to Apr. 10, 1969, have been utilized to investigate the energy dependence of azimuthal gradients of cosmic ray particles and its effect on the decay of the flare intensity. For an observer located to the east of the centroid of the population, the azimuthal corotation term and the convection term will be additive, resulting in a short decay time constant. An observer located to the west of the centroid of the population will experience a much longer decay time constant, the corotation term partially or completely compensating the loss of particles due to convection. At very low energies, the azimuthal corotation term may even be more than the convection term, thus resulting in a rise in intensity instead of decay during the later part of the event.
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