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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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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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) |
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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. |
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The Pennsylvania State University CiteSeerX Archives |
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Tavolk GeoMag1304014SmirnovIILO.fm |
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geomag1304014smirnoviilo.fm |
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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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ENVELOPE(158.257,158.257,52.962,52.962) |
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Paratunka |
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Kamchatka |
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Kamchatka |
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http://www.ikir.ru/en/Departments/Paratunka/lfg/GMA515.pdf |
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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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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766051141955616768 |