Aurora Borealis


Luosto and Suomu- Home to the Northern Lights


The aurora borealis (the Northern Lights) has always fascinated mankind, and people enjoy travelling to Lapland to view them in all their magnificence; when visible they provide brilliant light shows in the earth's atmosphere.

The Northern Lights often frequent Luosto and Suomu and our tours and safaris are geared to ensure that you receive the best chances to view them.

Imagine sitting in your log cabin, next to the roaring open fire looking out at the fantastic display of lights. Or perhaps consider a late night skidoo (snowmobile) safari and seeing the lights right in the heart of nature. These are fantastic photogrpahy moments that should be enjoyed by all.






But how does the Aurora Borealis Work?

The aurora, surrounds the north magnetic pole (aurora borealis)  occurs when highly charged electrons from the solar wind interact with elements in the earth's atmosphere. Solar winds stream away from the sun at speeds of about 1 million miles per hour. When they reach the earth, some 40 hours after leaving the sun, they follow the lines of magnetic force generated by the earth's core and flow through the magnetosphere, a teardrop-shaped area of highly charged electrical and magnetic fields.

­As the electrons enter the earth's upper atmosphere, they will encounter atoms of oxygen and nitrogen at altitudes from 20 to 200 miles above the earth's surface. The color of the aurora depends on which atom is struck, and the altitude of the meeting.

    Green - oxygen, up to 150 miles in altitude
    Red - oxygen, above 150 miles in altitude
    Blue - nitrogen, up to 60 miles in altitude
    Purple/violet - nitrogen, above 60 miles in altitude

All of the magnetic and electrical forces react with one another in constantly shifting combinations. These shifts and flows can be seen as the auroras "dance," moving along with the atmospheric currents that can reach 20,000,000 amperes at 50,000 volts. (In contrast, the circuit breakers in your home will disengage when current flow exceeds 15-30 amperes at 120 volts.)

The auroras generally occur along the "auroral ovals," which center on the magnetic poles (not the geographic poles) and roughly correspond with the Arctic and Antarctic circles. There are times, though, when the lights are farther south, usually when there are a lot of sunspots. Sunspot activity follows an 11-year cycle. The next peak will occur in 2011 and 2012, so opportunities to see auroras outside their normal range should be good.