Instrumentation for the surface measurements of atmospheric electrical parameters at Maitri, Antarctica: first results

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dc.contributor.author Panneerselvam, C.
dc.contributor.author Kumar, C.P. Anil
dc.contributor.author Dhar, Ajay
dc.contributor.author Nair, K.U.
dc.contributor.author Selvaraj, C.
dc.contributor.author Gurubaran, S.
dc.contributor.author Pathan, B.M.
dc.date.accessioned 2015-10-14T05:27:25Z
dc.date.accessioned 2021-02-12T09:34:02Z
dc.date.available 2015-10-14T05:27:25Z
dc.date.available 2021-02-12T09:34:02Z
dc.date.issued 2010
dc.identifier.citation Earth Planets Space, v. 62, p. 545–549, 2010, doi: 10.5047/eps.2010.06.001 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/574
dc.description.abstract We are operating atmospheric electrical instruments like long wire antenna, electric field meter, wire antenna and passive antenna for atmospheric Maxwell current, electric field, conduction current and atmospheric potential gradient. This year (December 2008) we have installed Electric Field Meter (EFM-100) and wire antenna for measuring the atmospheric electric field and conduction current. This instrument is deployed at Maitri, Antarctica and will be operated under any weather conditions like snow fall and strong blizzard etc. The study have been carried out during austral summer for the period of 2008 and 2009 at the Indian station, Maitri (70.75◦S, 11.75◦E, 117 m above mean sea level). The present work has been to understand the new instrument system in response to different meteorological conditions and on fairweather days. In this paper we have selected the data of the days during magnetically quiet period to minimize the upper atmospheric contribution. Fairweather’ conditions, i.e., days with absence of high winds, drifting or falling snow and clouds. The diurnal variation curve of electric field during fairweather days is a single periodic with a minimum at 04:00 UT and a maximum at 19:00 UT. But atmospheric current variation has minimum 03:00 UT for Maxwell current and conduction current. The maximum for Maxwell current is at 20:00 UT and 19:00 UT for the conduction current, which is very similar to the Carnegie curve. The measured electric field from the Passive antenna and EFM-100 compared and is behaving similar variation. Using Maxwell current density and conduction current density we have separated the displacement current density. en_US
dc.language.iso en en_US
dc.subject Maitri en_US
dc.subject Antarctica en_US
dc.subject Atmospheric electrical parameters en_US
dc.subject Atmospheric electricity en_US
dc.subject GEC en_US
dc.subject Global electric circuit en_US
dc.subject Displacement current en_US
dc.subject Conduction current en_US
dc.subject Electric field en_US
dc.subject Maxwell current en_US
dc.subject Fairweather day en_US
dc.title Instrumentation for the surface measurements of atmospheric electrical parameters at Maitri, Antarctica: first results en_US
dc.type Article en_US
dc.identifier.accession 091114


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