Validation of the radiation pattern of the Middle Atmosphere Alomar Radar System (MAARSY)

In 2009/2010 the Leibniz-Institute of Atmospheric Physics (IAP) installed a new powerful VHF radar on the island Andøya in Northern Norway (69.30° N, 16.04° E). The Middle Atmosphere Alomar Radar System (MAARSY) allows studies with high spatial and temporal resolution in the troposphere/lower strato...

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Published in:Advances in Radio Science
Main Authors: Renkwitz, T., Singer, W., Latteck, R., Stober, G., Rapp, M.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/ars-10-245-2012
https://ars.copernicus.org/articles/10/245/2012/
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spelling ftcopernicus:oai:publications.copernicus.org:ars38984 2023-05-15T13:25:41+02:00 Validation of the radiation pattern of the Middle Atmosphere Alomar Radar System (MAARSY) Renkwitz, T. Singer, W. Latteck, R. Stober, G. Rapp, M. 2018-01-15 application/pdf https://doi.org/10.5194/ars-10-245-2012 https://ars.copernicus.org/articles/10/245/2012/ eng eng doi:10.5194/ars-10-245-2012 https://ars.copernicus.org/articles/10/245/2012/ eISSN: 1684-9973 Text 2018 ftcopernicus https://doi.org/10.5194/ars-10-245-2012 2020-07-20T16:25:42Z In 2009/2010 the Leibniz-Institute of Atmospheric Physics (IAP) installed a new powerful VHF radar on the island Andøya in Northern Norway (69.30° N, 16.04° E). The Middle Atmosphere Alomar Radar System (MAARSY) allows studies with high spatial and temporal resolution in the troposphere/lower stratosphere and in the mesosphere/lower thermosphere of the Arctic atmosphere. The monostatic radar is operated at 53.5 MHz with an active phased array antenna consisting of 433 Yagi antennas. Each individual antenna is connected to its own transceiver with independent phase control and a scalable power output of up to 2 kW, which implies high flexibility of beam forming and beam steering. During the design phase of MAARSY several model studies have been carried out in order to estimate the radiation pattern for various combinations of beam forming and steering. However, parameters like mutual coupling, active impedance and ground parameters have an impact on the radiation pattern, but can hardly be measured. Hence, experiments need to be designed to verify the model results. For this purpose, the radar has occasionally been used in passive mode, monitoring the noise power received from both distinct cosmic noise sources like e.g. Cassiopeia A and Cygnus A, and the diffuse cosmic background noise. The analysis of the collected dataset enables us to verify beam forming and steering attempts. These results document the current status of the radar during its development and provide valuable information for further improvement. Text Andøya Arctic Northern Norway Copernicus Publications: E-Journals Alomar ENVELOPE(-67.083,-67.083,-68.133,-68.133) Andøya ENVELOPE(13.982,13.982,68.185,68.185) Arctic Norway Advances in Radio Science 10 245 253
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description In 2009/2010 the Leibniz-Institute of Atmospheric Physics (IAP) installed a new powerful VHF radar on the island Andøya in Northern Norway (69.30° N, 16.04° E). The Middle Atmosphere Alomar Radar System (MAARSY) allows studies with high spatial and temporal resolution in the troposphere/lower stratosphere and in the mesosphere/lower thermosphere of the Arctic atmosphere. The monostatic radar is operated at 53.5 MHz with an active phased array antenna consisting of 433 Yagi antennas. Each individual antenna is connected to its own transceiver with independent phase control and a scalable power output of up to 2 kW, which implies high flexibility of beam forming and beam steering. During the design phase of MAARSY several model studies have been carried out in order to estimate the radiation pattern for various combinations of beam forming and steering. However, parameters like mutual coupling, active impedance and ground parameters have an impact on the radiation pattern, but can hardly be measured. Hence, experiments need to be designed to verify the model results. For this purpose, the radar has occasionally been used in passive mode, monitoring the noise power received from both distinct cosmic noise sources like e.g. Cassiopeia A and Cygnus A, and the diffuse cosmic background noise. The analysis of the collected dataset enables us to verify beam forming and steering attempts. These results document the current status of the radar during its development and provide valuable information for further improvement.
format Text
author Renkwitz, T.
Singer, W.
Latteck, R.
Stober, G.
Rapp, M.
spellingShingle Renkwitz, T.
Singer, W.
Latteck, R.
Stober, G.
Rapp, M.
Validation of the radiation pattern of the Middle Atmosphere Alomar Radar System (MAARSY)
author_facet Renkwitz, T.
Singer, W.
Latteck, R.
Stober, G.
Rapp, M.
author_sort Renkwitz, T.
title Validation of the radiation pattern of the Middle Atmosphere Alomar Radar System (MAARSY)
title_short Validation of the radiation pattern of the Middle Atmosphere Alomar Radar System (MAARSY)
title_full Validation of the radiation pattern of the Middle Atmosphere Alomar Radar System (MAARSY)
title_fullStr Validation of the radiation pattern of the Middle Atmosphere Alomar Radar System (MAARSY)
title_full_unstemmed Validation of the radiation pattern of the Middle Atmosphere Alomar Radar System (MAARSY)
title_sort validation of the radiation pattern of the middle atmosphere alomar radar system (maarsy)
publishDate 2018
url https://doi.org/10.5194/ars-10-245-2012
https://ars.copernicus.org/articles/10/245/2012/
long_lat ENVELOPE(-67.083,-67.083,-68.133,-68.133)
ENVELOPE(13.982,13.982,68.185,68.185)
geographic Alomar
Andøya
Arctic
Norway
geographic_facet Alomar
Andøya
Arctic
Norway
genre Andøya
Arctic
Northern Norway
genre_facet Andøya
Arctic
Northern Norway
op_source eISSN: 1684-9973
op_relation doi:10.5194/ars-10-245-2012
https://ars.copernicus.org/articles/10/245/2012/
op_doi https://doi.org/10.5194/ars-10-245-2012
container_title Advances in Radio Science
container_volume 10
container_start_page 245
op_container_end_page 253
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