Background magnetic spectra: ∼10−5 to ∼105 Hz
The Arrival Heights area of the Hut Point Peninsula on Ross Island has been designated the 2nd Site of Special Scientific Interest (SSSI) on the Antarctic continent. It is the only SSSI in Antarctica designated as a natural electromagnetically ‘quiet site’. As the electromagnetic noise levels of civ...
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Veröffentlicht in: | Geophysical research letters 1990-09, Vol.17 (10), p.1593-1596 |
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creator | Lanzerotti, L. J. Maclennan, C. G. Fraser-Smith, A. C. |
description | The Arrival Heights area of the Hut Point Peninsula on Ross Island has been designated the 2nd Site of Special Scientific Interest (SSSI) on the Antarctic continent. It is the only SSSI in Antarctica designated as a natural electromagnetically ‘quiet site’. As the electromagnetic noise levels of civilization increase world‐wide, such sites around the world, if preserved, will be of increasing scientific importance. We report here the determination of the amplitude and functional form of the geomagnetic fluctuations measured at Arrival Heights in June 1986. The frequency range covered is from ∼10−5 to ∼105 Hz, with a gap between ∼10−1 to ∼10¹ Hz due to instrumentation limitations. Over this frequency range, which is larger than any reported previously from any site on Earth, the magnetic field amplitude spectrum in units of
/
falls with increasing frequency f as ∼f−1 to ∼f−1.5, and has a value of
∼108/
at f∼10−3 Hz. |
doi_str_mv | 10.1029/GL017i010p01593 |
format | Article |
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/
falls with increasing frequency f as ∼f−1 to ∼f−1.5, and has a value of
∼108/
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/
falls with increasing frequency f as ∼f−1 to ∼f−1.5, and has a value of
∼108/
at f∼10−3 Hz.</description><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Magnetic pulsations</subject><subject>Physics of the magnetosphere</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1990</creationdate><recordtype>article</recordtype><recordid>eNpdkM9Kw0AQhxdRsFbPXnPxGJ3Z3WR3vWm1iRAUROlxmSSbEvsvJJFan6Bnn8en6ZMYiSh4mhl-3zeHH2OnCOcI3FxECaAqAaECDIzYYwM0UvoaQO2zAYDpdq7CQ3bUNC8AIEDggIlrymbTevW6zL0FTZeuLTOvqVzW1nTp7bafCLvtR-C1q_4IvPj9mB0UNG_cyc8csufx7dMo9pOH6G50lfglouB-Gha5Q-RC5go0R5eGmhQPuTFaBakSBeUE2qQKU8FJSa0dyA7MpSPKjBiys_5vRU1G86KmZVY2tqrLBdUbi0YIlFx1nOy5dTl3m78c7Hcx9l8xNnpMpDG80_xeK5vWvf1qVM9sqIQK7OQ-svH4ZhKoUWxj8QXiemaW</recordid><startdate>199009</startdate><enddate>199009</enddate><creator>Lanzerotti, L. J.</creator><creator>Maclennan, C. G.</creator><creator>Fraser-Smith, A. C.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope></search><sort><creationdate>199009</creationdate><title>Background magnetic spectra: ∼10−5 to ∼105 Hz</title><author>Lanzerotti, L. J. ; Maclennan, C. G. ; Fraser-Smith, A. C.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-i1132-b6fde11234d70821eb68a726299875b73fada089b71b32a7488e04821d4eaac93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1990</creationdate><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Magnetic pulsations</topic><topic>Physics of the magnetosphere</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lanzerotti, L. J.</creatorcontrib><creatorcontrib>Maclennan, C. G.</creatorcontrib><creatorcontrib>Fraser-Smith, A. C.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lanzerotti, L. J.</au><au>Maclennan, C. G.</au><au>Fraser-Smith, A. C.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Background magnetic spectra: ∼10−5 to ∼105 Hz</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>1990-09</date><risdate>1990</risdate><volume>17</volume><issue>10</issue><spage>1593</spage><epage>1596</epage><pages>1593-1596</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>The Arrival Heights area of the Hut Point Peninsula on Ross Island has been designated the 2nd Site of Special Scientific Interest (SSSI) on the Antarctic continent. It is the only SSSI in Antarctica designated as a natural electromagnetically ‘quiet site’. As the electromagnetic noise levels of civilization increase world‐wide, such sites around the world, if preserved, will be of increasing scientific importance. We report here the determination of the amplitude and functional form of the geomagnetic fluctuations measured at Arrival Heights in June 1986. The frequency range covered is from ∼10−5 to ∼105 Hz, with a gap between ∼10−1 to ∼10¹ Hz due to instrumentation limitations. Over this frequency range, which is larger than any reported previously from any site on Earth, the magnetic field amplitude spectrum in units of
/
falls with increasing frequency f as ∼f−1 to ∼f−1.5, and has a value of
∼108/
at f∼10−3 Hz.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/GL017i010p01593</doi><tpages>4</tpages></addata></record> |
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source | Wiley Online Library |
subjects | Earth, ocean, space Exact sciences and technology External geophysics Magnetic pulsations Physics of the magnetosphere |
title | Background magnetic spectra: ∼10−5 to ∼105 Hz |
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