The Aurora Borealis
There are few sights as mesmerising as an undulating aurora. Although these appear in many forms – pillars, streaks, wisps and haloes of vibrating light – they're most memorable when taking the form of pale curtains wafting on a gentle breeze. Most often, the Arctic aurora appears as a faint green or light rose but, in periods of extreme activity, can change to yellow or crimson.
The visible aurora borealis, or Northern Lights, are caused by streams of charged particles from the sun, called the solar wind, which are directed by the earth's magnetic field towards the polar regions. Because the field curves downward in a halo surrounding the magnetic poles, the charged particles are drawn earthward. Their interaction with electrons in nitrogen and oxygen atoms in the upper atmosphere releases the energy creating the visible aurora. During periods of high activity, a single auroral storm can produce a trillion watts of electricity with a current of 1 million amps.
The Inuit (Eskimos) call the lights arsarnerit ('to play with a ball'), as they were thought to be ancestors playing ball with a walrus skull. The Inuit also attach spiritual significance to the lights, and some believe that they represent the capering of unborn children; some consider them gifts from the dead to light the long polar nights and others see them as a storehouse of events, past and future.
The best time of year to catch the northern lights in Norway is from October to March, although you may also see them as early as August.