Magnetic storm associated perturbations of the upper atmosphere: Recent results obtained by satellite‐borne gas analyzers
GW Prölss - Reviews of Geophysics, 1980 - Wiley Online Library
This review summarizes some of the recent results on the disturbed upper atmosphere
obtained by satellite‐borne gas analyzers. According to these measurements …
obtained by satellite‐borne gas analyzers. According to these measurements …
Some properties of upper atmosphere dynamics
HG Mayr, I Harris, NW Spencer - Reviews of Geophysics, 1978 - Wiley Online Library
Composition and temperature data from satellite measurements and from radar backscatter
observations show that dynamics is a major key in our understanding of the upper …
observations show that dynamics is a major key in our understanding of the upper …
Density perturbations in the upper atmosphere caused by the dissipation of solar wind energy
GW Prölss - Surveys in Geophysics, 2011 - Springer
The upper atmosphere constitutes the outer region of the terrestrial gas envelope above
about 100 km altitude. The energy budget of this outer gas layer is partly controlled by the …
about 100 km altitude. The energy budget of this outer gas layer is partly controlled by the …
A theoretical study of thermospheric composition perturbations during an impulsive geomagnetic storm
AG Burns, TL Killeen, RG Roble - Journal of Geophysical …, 1991 - Wiley Online Library
The compositional response of the neutral thermosphere to an impulsive geomagnetic storm
has been investigated using a numerical simulation made with the National Center for …
has been investigated using a numerical simulation made with the National Center for …
Neutral atmospheric composition between 60 and 220 km: A theoretical model for mid-latitudes
A new theoretical model for mid-latitude mesosphere and lower thermosphere at equinox
conditions has been developed by including new values of various characteristic …
conditions has been developed by including new values of various characteristic …
Dissipation of solar wind energy in the Earth's upper atmosphere: The geomagnetic activity effect
GW Prölss, M Roemer, JW Slowey - Advances in space research, 1988 - Elsevier
The dissipation of solar wind energy in the Earth's upper atmosphere remains one of the
most challenging topics in thermospheric physics. Not only does this energy transfer have a …
most challenging topics in thermospheric physics. Not only does this energy transfer have a …
Seasonal variations in the latitudinal structure of atmospheric disturbances
GW Prölss, U Von Zahn - Journal of Geophysical Research, 1977 - Wiley Online Library
The N2/O density ratio as measured by the Esro 4 satellite is used to investigate seasonal
changes in the latitudinal structure of nine disturbance events. A comparison of summer and …
changes in the latitudinal structure of nine disturbance events. A comparison of summer and …
[图书][B] The prediction of ionospheric conditions
GS Ivanov-Kholodny, AV Mikhailov - 2012 - books.google.com
The ionosphere of the Earth has been actively studied since the 1920's, following the
discovery of ground radio-sounding. By means of this method results were ohtained by an …
discovery of ground radio-sounding. By means of this method results were ohtained by an …
On the mechanisms responsible for high‐latitude thermospheric composition variations during the recovery phase of a geomagnetic storm
AG Burns, TL Killeen, G Crowley… - Journal of …, 1989 - Wiley Online Library
A considerable amount of previous work has been carried out to investigate variations in
thermospheric composition that occur in response to the onset and main phase of …
thermospheric composition that occur in response to the onset and main phase of …
Seasonal variations of atmospheric‐ionospheric disturbances
GW Prölss - Journal of Geophysical Research, 1977 - Wiley Online Library
This study investigates seasonal changes in the morphology of atmospheric‐ionospheric
disturbances. They are inferred from variations in the global distribution of negative storm …
disturbances. They are inferred from variations in the global distribution of negative storm …