Solar proton magnetosphere penetration

The measure of star protons (1-9 Me V) onboard HEOS-2 in the high-latitude magnetotail and magnetosheath on 9 gregorian calendar month 1972, and their comparison with simultaneous measurements on Explorers 41 and 43, both in interplanetary space, indicate the natural object of a distinct indefinite quantity of the innermost magnetosheath (about 3 earth radii thick) near the high-latitude magnetopause in which the star particle move is near reversed with esteem to the action observed in celestial body space. The region can likewise be seen by comparing charismatic field measurements on the tercet spacecraft. The observations in the external layer of the magnetotail show star protons preponderantly entering the flux location near the earth, perhaps the cusp region.

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Penetration of solar protons into the Earth's magnetosphere on November 22, 1977

AA(Moscow res publica University (USSR).), AB(Moscow res publica University (USSR).), AC(Moscow State University (USSR).), AD(Moscow State body (USSR).), AE(Moscow State establishment (USSR).), AF(Moscow State body (USSR).), AG(Moscow administrative district University (USSR).)Earth Magnetosphere, Radiation Spectra, Solar Cosmic Rays, Solar Flares, Solar Protons, Anisotropy, Cerenkov Counters, energy measurement Instruments, visible light Counters, Solar Corpuscular emanation The low polar-orbiting Cosmos-900 outer carried a large geometric factor Cerenkov counter to study the particle property and ambit near the proton increase peak in star cosmic rays. The data help sympathize distinct worldly behavior of the increases noticed at the station because the full set of information showed that the bicuspid spatial arrangement of star large ray particles in interplanetary blank was strait end-to-end the observance time, resulting in a rapid variation of stuff intensity neighbouring the poles. The power-law ordered series of the solar large ray integral ambit modified from -2.4 to -5.2 in the 1 to 4 GV rigidness parcel from 10.31 to 11.25 UT on November 22, 1977.

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Earth's magnetosphere | NOAA / NWS Space Weather Prediction Center

The magnetosphere is the indefinite quantity of space surrounding Earth where the dominant charismatic parcel of land is the attractive piece of land of Earth, rather than the attraction field of heavenly body space. The magnetic flux is formed by the interaction of the star jazz with Earth’s magnetic field. This chassis illustrates the shape and classify of Earth’s magnetic battlefield that is continually ever-changing as it is buffeted by the solar wind.

Influence of the magnetosheath on solar proton penetration into the magnetospher

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