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рддрддреНрд╕рдо рдФрд░ рддрджреНрднрд╡ рд╢рдмреНрдж рдХреА рдкрд░рд┐рднрд╛рд╖рд╛,рдкрд╣рдЪрд╛рдирдиреЗ рдХреЗ рдирд┐рдпрдо рдФрд░ рдЙрджрд╣рд╛рд░рдг - Tatsam Tadbhav

рддрддреНрд╕рдо рд╢рдмреНрдж (Tatsam Shabd) : рддрддреНрд╕рдо рджреЛ рд╢рдмреНрджреЛрдВ рд╕реЗ рдорд┐рд▓рдХрд░ рдмрдирд╛ рд╣реИ тАУ рддрдд +рд╕рдо , рдЬрд┐рд╕рдХрд╛ рдЕрд░реНрде рд╣реЛрддрд╛ рд╣реИ рдЬреНрдпреЛрдВ рдХрд╛ рддреНрдпреЛрдВред рдЬрд┐рди рд╢рдмреНрджреЛрдВ рдХреЛ рд╕рдВрд╕реНрдХреГрдд рд╕реЗ рдмрд┐рдирд╛...

magnetosphere


Our Sun emits a continuous outflowing stream of electrons and protons into the solar system, called the solar wind. The solar wind plasma which has charged particles embedded in the extended magnetic field of the Sun, moves at speeds of a few hundred km per second. It interacts with solar system bodies including Earth and its moon. Since the Earth has a global magnetic field, it obstructs the solar wind plasma and this interaction results in the formation of a magnetic envelope around Earth, called the magnetosphere.

The EarthтАЩs magnetosphere is compressed into a region approximately three to four times the Earth radius (~22000 km above the surface) on the side facing the Sun, but is stretched into a long tail (geotail) on the opposite side that goes beyond the orbit of Moon. Approximately, once every 29 days, Moon traverses the geotail for about 6 days centered around full moon. 
#Geo_Tail
#SOLAR_WIND

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