Atmospheric influence on a laser beam observed on the OICETS – ARTEMIS communication demonstration link

In 2006 bi-directional optical inter-satellite communication experiments were conducted between the Japan Aerospace Exploration Agency (JAXA) Optical Inter-orbit Communications Engineering Test Satellite (OICETS) and the European Space Agency (ESA) multi-purpose telecommunications and technology dem...

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Main Author: A. Löscher
Format: Article
Language:English
Published: Copernicus Publications 2010-09-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/3/1233/2010/amt-3-1233-2010.pdf
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spelling doaj-356dbe8ee3a5462c83ec872301b593ec2020-11-24T22:37:57ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482010-09-01351233123910.5194/amt-3-1233-2010Atmospheric influence on a laser beam observed on the OICETS – ARTEMIS communication demonstration linkA. LöscherIn 2006 bi-directional optical inter-satellite communication experiments were conducted between the Japan Aerospace Exploration Agency (JAXA) Optical Inter-orbit Communications Engineering Test Satellite (OICETS) and the European Space Agency (ESA) multi-purpose telecommunications and technology demonstration satellite (Advanced Relay and Technology MISsion) ARTEMIS. On 5 April 2006, an experiment was successfully carried out by maintaining the inter-satellite link during OICETS's setting behind the Earth limb until the signal was lost. This setup resembles an occultation observation where the influence of Earth's atmosphere is evident in the power fluctuations recorded at ARTEMIS's (and OICETS's) receiver. These fluctuations do not exist or are at a low level at a link path above the atmosphere and steadily increase as OICETS sets behind the horizon until the tracking of the signal is lost. This specific experiment was performed only once since atmospheric science was not the goal of this demonstration. Nevertheless, this kind of data, if available more frequently in future, can help to study atmospheric turbulence and validate models. The data present here were recorded at ARTEMIS. http://www.atmos-meas-tech.net/3/1233/2010/amt-3-1233-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Löscher
spellingShingle A. Löscher
Atmospheric influence on a laser beam observed on the OICETS – ARTEMIS communication demonstration link
Atmospheric Measurement Techniques
author_facet A. Löscher
author_sort A. Löscher
title Atmospheric influence on a laser beam observed on the OICETS – ARTEMIS communication demonstration link
title_short Atmospheric influence on a laser beam observed on the OICETS – ARTEMIS communication demonstration link
title_full Atmospheric influence on a laser beam observed on the OICETS – ARTEMIS communication demonstration link
title_fullStr Atmospheric influence on a laser beam observed on the OICETS – ARTEMIS communication demonstration link
title_full_unstemmed Atmospheric influence on a laser beam observed on the OICETS – ARTEMIS communication demonstration link
title_sort atmospheric influence on a laser beam observed on the oicets – artemis communication demonstration link
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2010-09-01
description In 2006 bi-directional optical inter-satellite communication experiments were conducted between the Japan Aerospace Exploration Agency (JAXA) Optical Inter-orbit Communications Engineering Test Satellite (OICETS) and the European Space Agency (ESA) multi-purpose telecommunications and technology demonstration satellite (Advanced Relay and Technology MISsion) ARTEMIS. On 5 April 2006, an experiment was successfully carried out by maintaining the inter-satellite link during OICETS's setting behind the Earth limb until the signal was lost. This setup resembles an occultation observation where the influence of Earth's atmosphere is evident in the power fluctuations recorded at ARTEMIS's (and OICETS's) receiver. These fluctuations do not exist or are at a low level at a link path above the atmosphere and steadily increase as OICETS sets behind the horizon until the tracking of the signal is lost. This specific experiment was performed only once since atmospheric science was not the goal of this demonstration. Nevertheless, this kind of data, if available more frequently in future, can help to study atmospheric turbulence and validate models. The data present here were recorded at ARTEMIS.
url http://www.atmos-meas-tech.net/3/1233/2010/amt-3-1233-2010.pdf
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