GeoMag1304014SmirnovIILO.fm

Abstract-Diurnal variations in the electric field strength, electrical conductivity, and temperature in the near Earth atmosphere under "fair weather" conditions at the Paratunka observatory (Kamchatka) are con sidered. It is shown that the morning maximum in the electric field diurnal beh...

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Main Author: Tavolk
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1082.898
http://www.ikir.ru/en/Departments/Paratunka/lfg/GMA515.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1082.898 2023-05-15T16:59:00+02:00 GeoMag1304014SmirnovIILO.fm Tavolk The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1082.898 http://www.ikir.ru/en/Departments/Paratunka/lfg/GMA515.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1082.898 http://www.ikir.ru/en/Departments/Paratunka/lfg/GMA515.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ikir.ru/en/Departments/Paratunka/lfg/GMA515.pdf text ftciteseerx 2020-05-03T00:27:47Z Abstract-Diurnal variations in the electric field strength, electrical conductivity, and temperature in the near Earth atmosphere under "fair weather" conditions at the Paratunka observatory (Kamchatka) are con sidered. It is shown that the morning maximum in the electric field diurnal behavior is caused by air convec tion in the near surface layer. The difference in the atmospheric temperatures near the Earth's surface and at an altitude of 25 m is chosen as a measure of the convective air flow. A high correlation of the values of the temperature difference for these altitudes with the diurnal behavior of the electric field strength is obtained. Text Kamchatka Unknown Paratunka ENVELOPE(158.257,158.257,52.962,52.962)
institution Open Polar
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description Abstract-Diurnal variations in the electric field strength, electrical conductivity, and temperature in the near Earth atmosphere under "fair weather" conditions at the Paratunka observatory (Kamchatka) are con sidered. It is shown that the morning maximum in the electric field diurnal behavior is caused by air convec tion in the near surface layer. The difference in the atmospheric temperatures near the Earth's surface and at an altitude of 25 m is chosen as a measure of the convective air flow. A high correlation of the values of the temperature difference for these altitudes with the diurnal behavior of the electric field strength is obtained.
author2 The Pennsylvania State University CiteSeerX Archives
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author Tavolk
spellingShingle Tavolk
GeoMag1304014SmirnovIILO.fm
author_facet Tavolk
author_sort Tavolk
title GeoMag1304014SmirnovIILO.fm
title_short GeoMag1304014SmirnovIILO.fm
title_full GeoMag1304014SmirnovIILO.fm
title_fullStr GeoMag1304014SmirnovIILO.fm
title_full_unstemmed GeoMag1304014SmirnovIILO.fm
title_sort geomag1304014smirnoviilo.fm
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1082.898
http://www.ikir.ru/en/Departments/Paratunka/lfg/GMA515.pdf
long_lat ENVELOPE(158.257,158.257,52.962,52.962)
geographic Paratunka
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genre Kamchatka
genre_facet Kamchatka
op_source http://www.ikir.ru/en/Departments/Paratunka/lfg/GMA515.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1082.898
http://www.ikir.ru/en/Departments/Paratunka/lfg/GMA515.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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