Abstract. A recurring pattern with a period of 267/8 days observed in the polar geomagnetic field during the interval from 1926 to 1941 appears to persist in the interplanetary magnetic field polarity observed with spacecraft during the interval from 1963 to 1968. This observation suggests the exist...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.696.718 http://www.leif.org/EOS/Science-1971-Wilcox-Dipole.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.696.718 2023-05-15T16:28:05+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.696.718 http://www.leif.org/EOS/Science-1971-Wilcox-Dipole.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.696.718 http://www.leif.org/EOS/Science-1971-Wilcox-Dipole.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.leif.org/EOS/Science-1971-Wilcox-Dipole.pdf text ftciteseerx 2016-01-08T18:40:34Z Abstract. A recurring pattern with a period of 267/8 days observed in the polar geomagnetic field during the interval from 1926 to 1941 appears to persist in the interplanetary magnetic field polarity observed with spacecraft during the interval from 1963 to 1968. This observation suggests the existence of a rotating solar magnetic "dipole " with a period of 267/8 + 0.003 days. Olsen (1) has discovered a recur-rent pattern with a period of 267/8 days in the horizontal component of the geomagnetic field observed at God-havn, Greenland (corrected geomagnet-ic latitude, 77.5°N), during the years Text Greenland Unknown Greenland |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
| description |
Abstract. A recurring pattern with a period of 267/8 days observed in the polar geomagnetic field during the interval from 1926 to 1941 appears to persist in the interplanetary magnetic field polarity observed with spacecraft during the interval from 1963 to 1968. This observation suggests the existence of a rotating solar magnetic "dipole " with a period of 267/8 + 0.003 days. Olsen (1) has discovered a recur-rent pattern with a period of 267/8 days in the horizontal component of the geomagnetic field observed at God-havn, Greenland (corrected geomagnet-ic latitude, 77.5°N), during the years |
| author2 |
The Pennsylvania State University CiteSeerX Archives |
| format |
Text |
| url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.696.718 http://www.leif.org/EOS/Science-1971-Wilcox-Dipole.pdf |
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Greenland |
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Greenland |
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Greenland |
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Greenland |
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http://www.leif.org/EOS/Science-1971-Wilcox-Dipole.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.696.718 http://www.leif.org/EOS/Science-1971-Wilcox-Dipole.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766017699566059520 |