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<front>
<journal-meta>
<journal-id journal-id-type="publisher">HGSS</journal-id>
<journal-title-group>
<journal-title>History of Geo- and Space Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">HGSS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Hist. Geo Space. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2190-5029</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/hgss-1-13-2010</article-id>
<title-group>
<article-title>Kristian Birkeland&apos;s pioneering investigations of geomagnetic disturbances</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Egeland</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Burke</surname>
<given-names>W. J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>University of Oslo, Norway</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Air Force Research Laboratory, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>12</day>
<month>04</month>
<year>2010</year>
</pub-date>
<volume>1</volume>
<issue>1</issue>
<fpage>13</fpage>
<lpage>24</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2010 A. Egeland</copyright-statement>
<copyright-year>2010</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://hgss.copernicus.org/articles/1/13/2010/hgss-1-13-2010.html">This article is available from https://hgss.copernicus.org/articles/1/13/2010/hgss-1-13-2010.html</self-uri>
<self-uri xlink:href="https://hgss.copernicus.org/articles/1/13/2010/hgss-1-13-2010.pdf">The full text article is available as a PDF file from https://hgss.copernicus.org/articles/1/13/2010/hgss-1-13-2010.pdf</self-uri>
<abstract>
<p>More than 100 years ago Kristian Birkeland (1967&amp;ndash;1917) addressed questions
that had vexed scientists for centuries. Why do auroras appear overhead
while the Earth&apos;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&apos;s
synthesis of laws governing electricity and magnetism. After analyzing
thousands of magnetograms, he divided disturbances into 3 categories:
&lt;br&gt;&lt;br&gt;
1. &lt;i&gt;Polar elementary storms&lt;/i&gt; are auroral-latitude disturbances now called substorms.&lt;br&gt;
2. &lt;i&gt;Equatorial perturbations&lt;/i&gt; correspond to initial and main phases of magnetic storms.&lt;br&gt;
3. &lt;i&gt;Cyclo-median perturbations&lt;/i&gt; reflect enhanced solar-quiet currents on the dayside.&lt;br&gt;
&lt;br&gt;
He published the first two-cell pattern of electric currents in Earth&apos;s
upper atmosphere, nearly 30 years before the ionosphere was identified as a
separate entity. Birkeland&apos;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&apos;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 &quot;electric corpuscles
from the Sun&quot; and &quot;the auroras are formed by corpuscular rays drawn in
from space, and coming from the Sun&quot;. It can be reasonably argued that the
year 1896 marks the founding of space plasma physics. Many of Birkeland&apos;s
insights were rooted in observations made during his terrella experiments,
the first attempts to simulate cosmic phenomena within a laboratory.
Birkeland&apos;s ideas were often misinterpreted or dismissed, but were verified
when technology advances allowed instrumented spacecraft to fly in space
above the ionosphere.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
<title>References</title>
<ref id="ref1">
<label>1</label><mixed-citation publication-type="other" xlink:type="simple">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.</mixed-citation>
</ref>
<ref id="ref2">
<label>2</label><mixed-citation publication-type="other" xlink:type="simple">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.</mixed-citation>
</ref>
<ref id="ref3">
<label>3</label><mixed-citation publication-type="other" xlink:type="simple">Birkeland, K.: Solution générale des équations de Maxwell pour un milieu absorbant, homogène et isotrope, Comptes Rendus Hebdomadaires des Sèances de l&apos;Acadèmie des Sciences, Paris, T.&amp;nbsp;12, 1046–1050, 1895.</mixed-citation>
</ref>
<ref id="ref4">
<label>4</label><mixed-citation publication-type="other" xlink:type="simple">Birkeland, K.: Résultats des rescherches magnéthiques faites par l&apos;expédition Norvégienne de 1899–1900, Sci. Phy. et Nat., 4éme, T.&amp;nbsp;12, Geneva, 565–586, 1901.</mixed-citation>
</ref>
<ref id="ref5">
<label>5</label><mixed-citation publication-type="other" xlink:type="simple">Birkeland, K.: The Norwegian Aurora Polaris Expedition 1902–1903, Aschehoug, Christiania, Norway, Vol.&amp;nbsp;I, 1–316, 1908.</mixed-citation>
</ref>
<ref id="ref6">
<label>6</label><mixed-citation publication-type="other" xlink:type="simple">Birkeland, K.: The Norwegian Aurora Polaris Expedition 1902–1903, Aschehoug, Christiania, Norway, Vol.&amp;nbsp;II, 317–801, 1913.</mixed-citation>
</ref>
<ref id="ref7">
<label>7</label><mixed-citation publication-type="other" xlink:type="simple">Birkeland, K.: Les rayons corpuscularies du soleil qui pénètrent dans l&apos;athmosphére terrestre sont-ils négatifs ou positives?, Arch. Des Sciences Physiques et Naturelles, 4éme période, T.&amp;nbsp;41,  22–37 and 108–124, 1916.</mixed-citation>
</ref>
<ref id="ref8">
<label>8</label><mixed-citation publication-type="other" xlink:type="simple">Borovsky, J. E. and Denton, M. H.: Differences between CME-driven storms and CIR driven storms, J. Geophys. Res., 111, A07S08, https://doi.org/1029/2005JA011447, 2006.</mixed-citation>
</ref>
<ref id="ref9">
<label>9</label><mixed-citation publication-type="other" xlink:type="simple">Bostrøm, R.: Currents in the ionosphere and magnetosphere, in: The Birkeland Symposium on Aurora and Magnetic Storms, edited by: Egeland, A. and Holtet, J. Centre National de la Recherche Scientifique, Paris, 445–459, 1968.</mixed-citation>
</ref>
<ref id="ref10">
<label>10</label><mixed-citation publication-type="other" xlink:type="simple">Chapman, S.: Historical introduction to aurora and magnetic storms, in: The Birkeland Symposium on Aurora and Magnetic Storms, edited by: Egeland, A. and Holtet, J., Centre National de la Recherche Scientifique, Paris, 21–29, 1968.</mixed-citation>
</ref>
<ref id="ref11">
<label>11</label><mixed-citation publication-type="other" xlink:type="simple">Chapman, S. and Bartels, J.: Geomagnetism, Clarendon Press, Oxford, Vol.&amp;nbsp;I &amp; II,  1940.</mixed-citation>
</ref>
<ref id="ref12">
<label>12</label><mixed-citation publication-type="other" xlink:type="simple">Dessler, A. J.: The evolution of arguments regarding the existence of field-aligned currents, in: Magnetospheric Currents, AGU Geophys. Monograph 28, edited by: Potemra, T., 22–28, 1983.</mixed-citation>
</ref>
<ref id="ref13">
<label>13</label><mixed-citation publication-type="other" xlink:type="simple">Dungey, J. W.: Interplanetary magnetic field and the auroral zones, Phys. Rev. Lett., 6, 47–48, 1961.</mixed-citation>
</ref>
<ref id="ref14">
<label>14</label><mixed-citation publication-type="other" xlink:type="simple">Egeland, A.: Birkeland&apos;s electromagnetic gun, IEEE Trans. Plasma Science, 17, 3–82, 1989.</mixed-citation>
</ref>
<ref id="ref15">
<label>15</label><mixed-citation publication-type="other" xlink:type="simple">Egeland, A. and Burke, W. J.: Kristian Birkeland, The First Space Scientist, 1–221, Springer Verlag,  2005.</mixed-citation>
</ref>
<ref id="ref16">
<label>16</label><mixed-citation publication-type="other" xlink:type="simple">Fukushima, N.: Equivalence in ground geomagnetic effects of Chapman-Vestine&apos;s and Birkeland–Alfvén&apos;s electric current systems for polar magnetic storms, Rep. Ionos. Space Res. Japan, 23, 219–228, 1969.</mixed-citation>
</ref>
<ref id="ref17">
<label>17</label><mixed-citation publication-type="other" xlink:type="simple">Fukushima, N.: Birkeland&apos;s work with geomagnetic disturbances in relation to modern research, The Birkeland Lecture No. 3, Norwegian Academy of Science and Letters, Oslo, 1989.</mixed-citation>
</ref>
<ref id="ref18">
<label>18</label><mixed-citation publication-type="other" xlink:type="simple">Gauss, C. F.: Resultate aus den Beobachtungen des magnetischen Vereins Jahre 1836–1841, Werke, 5, 1841.</mixed-citation>
</ref>
<ref id="ref19">
<label>19</label><mixed-citation publication-type="other" xlink:type="simple">Iijima, T. and Potemra, T. A.: The amplitude distribution of field-aligned currents at northern high latitudes observed by TRIAD, J. Geophys. Res., 81, 2165–2174, 1976.</mixed-citation>
</ref>
<ref id="ref20">
<label>20</label><mixed-citation publication-type="other" xlink:type="simple">Iijima, T. and Potemra, T. A.: Large-scale characteristics of field-aligned currents associated with substorms, J. Geophys. Res., 83, 599–615, 1978.</mixed-citation>
</ref>
<ref id="ref21">
<label>21</label><mixed-citation publication-type="other" xlink:type="simple">Lundin, R.: The universal importance of auroral research, in: Egeland Symposium on Auroral and Atmospheric Research, edited by: Moen, J. and Holtet, J., Department of Physics, University of Oslo, 55–75, 2002.</mixed-citation>
</ref>
<ref id="ref22">
<label>22</label><mixed-citation publication-type="other" xlink:type="simple">Peratt, A. L.: The legacy of Birkeland&apos;s plasma torch, The Birkeland Lecture No. 9, Norwegian Academy of Science and Letters, Oslo, 1996.</mixed-citation>
</ref>
<ref id="ref23">
<label>23</label><mixed-citation publication-type="other" xlink:type="simple">Potemra, T. A.: Satellite measurements of the Birkeland currents, The Birkeland Lecture No. 3, Norwegian Academy of Science and Letters, Oslo, 1989.</mixed-citation>
</ref>
<ref id="ref24">
<label>24</label><mixed-citation publication-type="other" xlink:type="simple">Schuster, A.: On the origin of magnetic storms, Proc. Roy. Soc. London, 85, 44–50, 1911.</mixed-citation>
</ref>
<ref id="ref25">
<label>25</label><mixed-citation publication-type="other" xlink:type="simple">Thomson, J. J.: Cathode rays, Phil. Mag., 44, p.&amp;nbsp;293, 1897.</mixed-citation>
</ref>
<ref id="ref26">
<label>26</label><mixed-citation publication-type="other" xlink:type="simple">Tsurutani, B. T., Gonzalez, W. D., Gonzalez, A. L. C., Guarnieri, F. L., Gopalswamy, N., Grande, M., Kamide, Y., Kasahara, Y., Lu, G., Mann, I., McPherron, R., Soraas, F., and Vasyliunas, V. M.: Corotating solar wind streams and recurrent geomagnetic activity: A review, J. Geophys. Res., 111, A07S01, https://doi.org/10.1029/2005JA011273, 2006.</mixed-citation>
</ref>
<ref id="ref27">
<label>27</label><mixed-citation publication-type="other" xlink:type="simple">Vasyliunas, V. M.: Mathematical models of magnetospheric convection and coupling to the ionosphere, in: Particles and Fields in the Magnetosphere, edited by: McCormac, B., Reidel, 60–72,  1970.</mixed-citation>
</ref>
<ref id="ref28">
<label>28</label><mixed-citation publication-type="other" xlink:type="simple">Vestine, E. H. and Chapman, S.: The electric current-system of geomagnetic disturbances, J. Geophys. Res., 43, 351–382,  1938.</mixed-citation>
</ref>
</ref-list>
</back>
</article>