Kristian
                                                    Birkeland 
                  (1867-1917) 
                                                   
                                                  The
                                                      Norwegian scientist Kristian
                                                      Birkeland pioneered the first serious
                                                      scientific study of the aurora.
                                                      He was first to suggest (in
                                                      1896) that the northern lights
                                                      were a result of the interaction
                                                      between particles emanating
                                                      from the Sun and Earth’s
                                                      magnetic field. He organized
                                                      several expeditions to the
                                                      far north of Norway and set
                                                      up observing stations there
                                                      to collect data on the aurora
                                                      and Earth’s magnetic
                                                      field. In his laboratory,
                                                      he was able to recreate the
                                                      aurora by bombarding a magnetized
                                                      metal ball (which represented
                                                      Earth) with electrons (representing
                                                      the solar wind). 
                                                   Confirmation
                                                      of his theories had to wait
                                                      for the advent of the Space
                                                      Age and satellites that could
                                                      explore Earth’s magnetosphere.
                                                      In 1973, a polar satellite
                                                      detected electric currents
                                                      that flow along the magnetic
                                                      field from Earth’s
                                                      magnetotail region,  through
                                                      the upper atmosphere and
                                                      back into space. They were
                                                      named “Birkeland currents” after
                                                      the scientist who had suggested
                                                  their existence decades earlier. 
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