Millstone Hill Thomson Scatter Results for 1972

During 1972, the vertically directed incoherent scatter radar at Millstone Hill (42.6°N, 71.5°W) was employed to measure electron density, electron and ion temperatures, and vertical ion velocity in the F-region over periods of 24 hours, one or two times per month. The observations spanned the heigh...

Full description

Bibliographic Details
Main Authors: Evans, J. V., Holt, J. M.
Format: Technical Report
Language:en_US
Published: Haystack Observatory 2015
Online Access:http://hdl.handle.net/1721.1/97674
_version_ 1811083398352994304
author Evans, J. V.
Holt, J. M.
author_facet Evans, J. V.
Holt, J. M.
author_sort Evans, J. V.
collection MIT
description During 1972, the vertically directed incoherent scatter radar at Millstone Hill (42.6°N, 71.5°W) was employed to measure electron density, electron and ion temperatures, and vertical ion velocity in the F-region over periods of 24 hours, one or two times per month. The observations spanned the height interval 200 to 900 km, approximately, and achieved a time resolution of about 30 minutes. This report presents the results of these measurements in a set of contour diagrams. For a number of the days, the spectra of the signals gathered at altitudes between 450 and 1125 km have been the subject of further analysis in an effort to determine the percentage of H[superscript +] ions present over Millstone. The results suggest that H[superscript +] ions are escaping from the F-region to the magnetosphere at a value close to the theoretical limiting flux during the daytime in all seasons. At night the flux becomes downward commencing near midnight in winter, but may remain upward throughout the night in summer.
first_indexed 2024-09-23T12:32:26Z
format Technical Report
id mit-1721.1/97674
institution Massachusetts Institute of Technology
language en_US
last_indexed 2024-09-23T12:32:26Z
publishDate 2015
publisher Haystack Observatory
record_format dspace
spelling mit-1721.1/976742019-04-12T13:25:09Z Millstone Hill Thomson Scatter Results for 1972 Evans, J. V. Holt, J. M. During 1972, the vertically directed incoherent scatter radar at Millstone Hill (42.6°N, 71.5°W) was employed to measure electron density, electron and ion temperatures, and vertical ion velocity in the F-region over periods of 24 hours, one or two times per month. The observations spanned the height interval 200 to 900 km, approximately, and achieved a time resolution of about 30 minutes. This report presents the results of these measurements in a set of contour diagrams. For a number of the days, the spectra of the signals gathered at altitudes between 450 and 1125 km have been the subject of further analysis in an effort to determine the percentage of H[superscript +] ions present over Millstone. The results suggest that H[superscript +] ions are escaping from the F-region to the magnetosphere at a value close to the theoretical limiting flux during the daytime in all seasons. At night the flux becomes downward commencing near midnight in winter, but may remain upward throughout the night in summer. 2015-07-06T13:56:06Z 2015-07-06T13:56:06Z 1978-09-18 Technical Report http://hdl.handle.net/1721.1/97674 en_US Millstone Technical Reports;530 application/pdf Haystack Observatory
spellingShingle Evans, J. V.
Holt, J. M.
Millstone Hill Thomson Scatter Results for 1972
title Millstone Hill Thomson Scatter Results for 1972
title_full Millstone Hill Thomson Scatter Results for 1972
title_fullStr Millstone Hill Thomson Scatter Results for 1972
title_full_unstemmed Millstone Hill Thomson Scatter Results for 1972
title_short Millstone Hill Thomson Scatter Results for 1972
title_sort millstone hill thomson scatter results for 1972
url http://hdl.handle.net/1721.1/97674
work_keys_str_mv AT evansjv millstonehillthomsonscatterresultsfor1972
AT holtjm millstonehillthomsonscatterresultsfor1972