Corpuscular streams related to solar m-regions
Corpuscular streams related to solar M-regions - recurrent geomagnetic disturbances during decline phase of sunspot cycle
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Corpuscular streams related to solar M-regions - recurrent geomagnetic disturbances during decline phase of sunspot cycle
Solar corpuscular streams identified with solar M-region - geomagnetic storms
Corpuscular streams related to solar M-regions
Worldwide positive-negative impulse pair observed on geomagnetic records found to be recurrent and associated with M-region disturbances
Search for solar M-regions complicated by velocity decrease near active sun, considering corpuscular streams as enhanced solar wind
Kp index and m-region geomagnetic storms
Interpretation of k sub p index and m-region geomagnetic storms - magnetopause-solar wind interaction
Recurrent cosmic-ray modulation phenomena with Forbush decrease characteristics correlated with M-region magnetic storms, concluding that each series results from shock wave solar initiated
Interpretation of the k sub p index as a measure of the flucuations of the sum of plasma plus magnetic pressure acting on the outer boundary of the magnetosphere
Radio and polarization observations of Jupiter, correlation between Jupiter events and solar M-region storms, and observation comparisons with Doppler shifted cyclotron predictions
Recurrent geomagnetic storms and structure of solar wind consisting of fast M-region stream embedded in slower ambient wind
The height of the GEOS-C spacecraft was utilized as measured by the onboard radar altimeter, for an improved determination of the earth's gravitational field and for the determination of the variation of the physical surface of the oceans. Two tracking system approaches to accurately determine the spacecraft height (orbit) are described and their results stated. These are satellite-to-satellite tracking (SST) and ground laser tracking (GLT). Height variations can be observed in the dm-regions using SST and in the m-region using present GLT.
An attempt was made to use GEOS-C spacecraft height, as measured by the onboard radar altimeter, for an improved determination of the earth's gravitational field and for the determination of the variation of the physical surface of the oceans. Two tracking system approaches to accurately determine the spacecraft height (orbit) are described and their results stated. These are satellite-to-satellite tracking (SST) and ground-laser tracking (GLT). Height variations can be observed in the dm-regions using SST and in the m-region using present GLT.
Skylab and ground-based observations in the extreme UV range of the spectrum are used to analyze characteristics of coronal holes, and to correlate their development with variations in the solar cycle. The mergence of bipolar magnetic regions (BMR) during the declining phase of the cycle is held reponsible for the formation of large equatorial holes (M-regions, which cause recurring geomagnetic storms). The BMR mergence model can also be applied to polar cap holes.
It is commonly believed that geomagnetic disturbances are caused by external influences connected with the solar wind. The 27-day recurrence of perturbations seems to be a strong hint for this interaction. But frequently geomagnetic disturbances occur without any relation to sunspot numbers or radiowave fluxes. This was one of the reasons for introducing hypothetical M-regions on the Sun and their relation to solar wind activities. Only one half of the variance of the geomagnetic AL-index could be related to the solar wind. Therefore it is concluded that internal processes of the magnetosphere were responsible for additional geomagnetic activity. Arguments, which might lead to the suggestion of geomagnetic disturbances as being caused by internal atmospheric dynamics are discussed and a rather preliminary scenario of those processes is proposed.