First EISCAT measurement of electron-gas temperature in the arti®cially heated D-region ionosphere
Abstract. The ionospheric electron gas can be heated arti®cially by a powerful radio wave. According to our modeling, the maximum e€ect of this heating occurs in the D-region where the electron temperature can increase by a factor of ten. Ionospheric plasma parameters such as Ne; Te and Ti are measu...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.210.431 2023-05-15T16:04:15+02:00 First EISCAT measurement of electron-gas temperature in the arti®cially heated D-region ionosphere A. Kero T. Boè Singer P. Pollari E. Turunen M. Rietveld The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.210.431 http://www.ann-geophys.net/18/1210/2000/angeo-18-1210-2000.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.210.431 http://www.ann-geophys.net/18/1210/2000/angeo-18-1210-2000.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ann-geophys.net/18/1210/2000/angeo-18-1210-2000.pdf text ftciteseerx 2016-01-07T17:49:46Z Abstract. The ionospheric electron gas can be heated arti®cially by a powerful radio wave. According to our modeling, the maximum e€ect of this heating occurs in the D-region where the electron temperature can increase by a factor of ten. Ionospheric plasma parameters such as Ne; Te and Ti are measured by EISCAT incoherent scatter radar on a routine basis. However, in the D-region the incoherent scatter echo is very weak because of the low electron density. Moreover, the incoherent scatter spectrum from the D-region is of Lorentzian shape which gives less information than the spectrum from the E- and F-regions. These make EISCAT measurements in the D-region di cult. A combined EISCAT VHF-radar and heating experiment was carried out in November 1998 with the aim to measure the electron temperature increase due to heating. In the experiment the heater was switched on/o € at 5 minute intervals and the integration time of the radar was chosen synchronously with the heating cycle. A systematic di€erence in the measured autocorrelation functions was found between heated and unheated periods. Key words: Ionosphere �active experiments; plasma temperature and density; wave propagation) 1 Text EISCAT Unknown |
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Open Polar |
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language |
English |
description |
Abstract. The ionospheric electron gas can be heated arti®cially by a powerful radio wave. According to our modeling, the maximum e€ect of this heating occurs in the D-region where the electron temperature can increase by a factor of ten. Ionospheric plasma parameters such as Ne; Te and Ti are measured by EISCAT incoherent scatter radar on a routine basis. However, in the D-region the incoherent scatter echo is very weak because of the low electron density. Moreover, the incoherent scatter spectrum from the D-region is of Lorentzian shape which gives less information than the spectrum from the E- and F-regions. These make EISCAT measurements in the D-region di cult. A combined EISCAT VHF-radar and heating experiment was carried out in November 1998 with the aim to measure the electron temperature increase due to heating. In the experiment the heater was switched on/o € at 5 minute intervals and the integration time of the radar was chosen synchronously with the heating cycle. A systematic di€erence in the measured autocorrelation functions was found between heated and unheated periods. Key words: Ionosphere �active experiments; plasma temperature and density; wave propagation) 1 |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
A. Kero T. Boè Singer P. Pollari E. Turunen M. Rietveld |
spellingShingle |
A. Kero T. Boè Singer P. Pollari E. Turunen M. Rietveld First EISCAT measurement of electron-gas temperature in the arti®cially heated D-region ionosphere |
author_facet |
A. Kero T. Boè Singer P. Pollari E. Turunen M. Rietveld |
author_sort |
A. Kero |
title |
First EISCAT measurement of electron-gas temperature in the arti®cially heated D-region ionosphere |
title_short |
First EISCAT measurement of electron-gas temperature in the arti®cially heated D-region ionosphere |
title_full |
First EISCAT measurement of electron-gas temperature in the arti®cially heated D-region ionosphere |
title_fullStr |
First EISCAT measurement of electron-gas temperature in the arti®cially heated D-region ionosphere |
title_full_unstemmed |
First EISCAT measurement of electron-gas temperature in the arti®cially heated D-region ionosphere |
title_sort |
first eiscat measurement of electron-gas temperature in the arti®cially heated d-region ionosphere |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.210.431 http://www.ann-geophys.net/18/1210/2000/angeo-18-1210-2000.pdf |
genre |
EISCAT |
genre_facet |
EISCAT |
op_source |
http://www.ann-geophys.net/18/1210/2000/angeo-18-1210-2000.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.210.431 http://www.ann-geophys.net/18/1210/2000/angeo-18-1210-2000.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766399953425399808 |