Payload charging events in the mesosphere and their impact on Langmuir type electric probes
Three sounding rockets were launched from Andøya Rocket Range in the ECOMA campaign in December 2010. The aim was to study the evolution of meteoric smoke particles during a major meteor shower. Of the various instruments onboard the rocket payload, this paper presents the data from a multi-Needle L...
Published in: | Annales Geophysicae |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2013
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Subjects: | |
Online Access: | https://elib.dlr.de/81628/ http://www.ann-geophys.net/31/187/2013/ |
_version_ | 1835010617232064512 |
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author | Bekkeng, T.-A. Barjatya, A. Hoppe, U.-P. Pedersen, A. Moen, J. I. Friedrich, M. Rapp, M. |
author_facet | Bekkeng, T.-A. Barjatya, A. Hoppe, U.-P. Pedersen, A. Moen, J. I. Friedrich, M. Rapp, M. |
author_sort | Bekkeng, T.-A. |
collection | Unknown |
container_issue | 2 |
container_start_page | 187 |
container_title | Annales Geophysicae |
container_volume | 31 |
description | Three sounding rockets were launched from Andøya Rocket Range in the ECOMA campaign in December 2010. The aim was to study the evolution of meteoric smoke particles during a major meteor shower. Of the various instruments onboard the rocket payload, this paper presents the data from a multi-Needle Langmuir Probe (m-NLP) and a charged dust detector. The payload floating potential, as observed using the m-NLP instrument, shows charging events on two of the three flights. These charging events cannot be explained using a simple charging model, and have implications towards the use of fixed bias Langmuir probes on sounding rockets investigating mesospheric altitudes. We show that for a reliable use of a single fixed bias Langmuir probe as a high spatial resolution relative density measurement, each payload should also carry an additional instrument to measure payload floating potential, and an instrument that is immune to spacecraft charging and measures absolute plasma density. |
format | Article in Journal/Newspaper |
genre | Andøya |
genre_facet | Andøya |
geographic | Andøya Langmuir |
geographic_facet | Andøya Langmuir |
id | ftdlr:oai:elib.dlr.de:81628 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(13.982,13.982,68.185,68.185) ENVELOPE(-67.150,-67.150,-66.967,-66.967) |
op_collection_id | ftdlr |
op_container_end_page | 196 |
op_doi | https://doi.org/10.5194/angeo-31-187-2013 |
op_relation | https://elib.dlr.de/81628/1/angeo-31-187-2013.pdf Bekkeng, T.-A. und Barjatya, A. und Hoppe, U.-P. und Pedersen, A. und Moen, J. I. und Friedrich, M. und Rapp, M. (2013) Payload charging events in the mesosphere and their impact on Langmuir type electric probes. Annales Geophysicae, 31, Seiten 187-196. Copernicus Publications. doi:10.5194/angeo-31-187-2013 <https://doi.org/10.5194/angeo-31-187-2013>. ISSN 0992-7689. |
publishDate | 2013 |
publisher | Copernicus Publications |
record_format | openpolar |
spelling | ftdlr:oai:elib.dlr.de:81628 2025-06-15T14:07:09+00:00 Payload charging events in the mesosphere and their impact on Langmuir type electric probes Bekkeng, T.-A. Barjatya, A. Hoppe, U.-P. Pedersen, A. Moen, J. I. Friedrich, M. Rapp, M. 2013 application/pdf https://elib.dlr.de/81628/ http://www.ann-geophys.net/31/187/2013/ en eng Copernicus Publications https://elib.dlr.de/81628/1/angeo-31-187-2013.pdf Bekkeng, T.-A. und Barjatya, A. und Hoppe, U.-P. und Pedersen, A. und Moen, J. I. und Friedrich, M. und Rapp, M. (2013) Payload charging events in the mesosphere and their impact on Langmuir type electric probes. Annales Geophysicae, 31, Seiten 187-196. Copernicus Publications. doi:10.5194/angeo-31-187-2013 <https://doi.org/10.5194/angeo-31-187-2013>. ISSN 0992-7689. Institut für Physik der Atmosphäre Zeitschriftenbeitrag PeerReviewed 2013 ftdlr https://doi.org/10.5194/angeo-31-187-2013 2025-06-04T04:58:07Z Three sounding rockets were launched from Andøya Rocket Range in the ECOMA campaign in December 2010. The aim was to study the evolution of meteoric smoke particles during a major meteor shower. Of the various instruments onboard the rocket payload, this paper presents the data from a multi-Needle Langmuir Probe (m-NLP) and a charged dust detector. The payload floating potential, as observed using the m-NLP instrument, shows charging events on two of the three flights. These charging events cannot be explained using a simple charging model, and have implications towards the use of fixed bias Langmuir probes on sounding rockets investigating mesospheric altitudes. We show that for a reliable use of a single fixed bias Langmuir probe as a high spatial resolution relative density measurement, each payload should also carry an additional instrument to measure payload floating potential, and an instrument that is immune to spacecraft charging and measures absolute plasma density. Article in Journal/Newspaper Andøya Unknown Andøya ENVELOPE(13.982,13.982,68.185,68.185) Langmuir ENVELOPE(-67.150,-67.150,-66.967,-66.967) Annales Geophysicae 31 2 187 196 |
spellingShingle | Institut für Physik der Atmosphäre Bekkeng, T.-A. Barjatya, A. Hoppe, U.-P. Pedersen, A. Moen, J. I. Friedrich, M. Rapp, M. Payload charging events in the mesosphere and their impact on Langmuir type electric probes |
title | Payload charging events in the mesosphere and their impact on Langmuir type electric probes |
title_full | Payload charging events in the mesosphere and their impact on Langmuir type electric probes |
title_fullStr | Payload charging events in the mesosphere and their impact on Langmuir type electric probes |
title_full_unstemmed | Payload charging events in the mesosphere and their impact on Langmuir type electric probes |
title_short | Payload charging events in the mesosphere and their impact on Langmuir type electric probes |
title_sort | payload charging events in the mesosphere and their impact on langmuir type electric probes |
topic | Institut für Physik der Atmosphäre |
topic_facet | Institut für Physik der Atmosphäre |
url | https://elib.dlr.de/81628/ http://www.ann-geophys.net/31/187/2013/ |