Kristian Birkeland's pioneering investigations of geomagnetic disturbances

Author:

Egeland A.,Burke W. J.

Abstract

Abstract. More than 100 years ago Kristian Birkeland (1967–1917) addressed questions that had vexed scientists for centuries. Why do auroras appear overhead while the Earth's magnetic field is disturbed? Are magnetic storms on Earth related to disturbances on the Sun? To answer these questions Birkeland devised terrella simulations, led coordinated campaigns in the Arctic wilderness, and then interpreted his results in the light of Maxwell's synthesis of laws governing electricity and magnetism. After analyzing thousands of magnetograms, he divided disturbances into 3 categories: 1. Polar elementary storms are auroral-latitude disturbances now called substorms. 2. Equatorial perturbations correspond to initial and main phases of magnetic storms. 3. Cyclo-median perturbations reflect enhanced solar-quiet currents on the dayside. He published the first two-cell pattern of electric currents in Earth's upper atmosphere, nearly 30 years before the ionosphere was identified as a separate entity. Birkeland's most enduring contribution toward understanding geomagnetic disturbances flowed from his recognition that field-aligned currents must connect the upper atmosphere with generators in distant space. The existence of field-aligned currents was vigorously debated among scientists for more than 50 years. Birkeland's conjecture profoundly affects present-day understanding of auroral phenomena and global electrodynamics. In 1896, four years after Lord Kelvin rejected suggestions that matter passes between the Sun and Earth, and two years before the electron was discovered, Birkeland proposed current carriers are "electric corpuscles from the Sun" and "the auroras are formed by corpuscular rays drawn in from space, and coming from the Sun". It can be reasonably argued that the year 1896 marks the founding of space plasma physics. Many of Birkeland's insights were rooted in observations made during his terrella experiments, the first attempts to simulate cosmic phenomena within a laboratory. Birkeland's ideas were often misinterpreted or dismissed, but were verified when technology advances allowed instrumented spacecraft to fly in space above the ionosphere.

Publisher

Copernicus GmbH

Subject

History and Philosophy of Science,General Earth and Planetary Sciences

Reference28 articles.

1. Alfvèn, H. and Egeland, A.: Auroral Research in Scandinavia, The Birkeland Lecture No. 1, Norwegian Academy of Science and Letters, Oslo, Norway, 1–32, 1987.

2. Anderson, B. J., Takahashi, K., and Toth, B. A.: Sensing global Birkeland currents with Iridium engineering magnetometer data, Geophys. Res. Lett., 27, 4045–4058, 2000.

3. Birkeland, K.: Solution générale des équations de Maxwell pour un milieu absorbant, homogène et isotrope, Comptes Rendus Hebdomadaires des Sèances de l'Acadèmie des Sciences, Paris, T. 12, 1046–1050, 1895.

4. Birkeland, K.: Résultats des rescherches magnéthiques faites par l'expédition Norvégienne de 1899–1900, Sci. Phy. et Nat., 4éme, T. 12, Geneva, 565–586, 1901.

5. Birkeland, K.: The Norwegian Aurora Polaris Expedition 1902–1903, Aschehoug, Christiania, Norway, Vol. I, 1–316, 1908.

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