The science case for the EISCAT_3D radar
The EISCAT (European Incoherent SCATer) Scientific Association has provided versatile incoherent scatter (IS) radar facilities on the mainland of northern Scandinavia (the EISCAT UHF and VHF radar systems) and on Svalbard (the electronically scanning radar ESR (EISCAT Svalbard Radar) for studies of...
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ftingv:oai:www.earth-prints.org:2122/10956 2023-05-15T16:04:28+02:00 The science case for the EISCAT_3D radar McCrea, Ian Aikio, Anita Alfonsi, Lucilla Belova, Evgenia Buchert, Stephan Clilverd, Mark Engler, Norbert Gustavsson, Björn Heinselman, Craig Kero, Johan Kosch, Mike Lamy, Hervé Leyser, Thomas Ogawa, Yasunobu Oksavik, Kjellmar Pellinen-Wannberg, Asta Pitout, Frederic Rapp, Markus Stanislawska, Iwona Vierinen, Juha #PLACEHOLDER_PARENT_METADATA_VALUE# Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia 2015 http://hdl.handle.net/2122/10956 https://doi.org/10.1186/s40645-015-0051-8 en eng Progress in Earth and Planetary Science 2 http://hdl.handle.net/2122/10956 doi:10.1186/s40645-015-0051-8 open article 2015 ftingv https://doi.org/10.1186/s40645-015-0051-8 2022-07-29T06:07:16Z The EISCAT (European Incoherent SCATer) Scientific Association has provided versatile incoherent scatter (IS) radar facilities on the mainland of northern Scandinavia (the EISCAT UHF and VHF radar systems) and on Svalbard (the electronically scanning radar ESR (EISCAT Svalbard Radar) for studies of the high-latitude ionised upper atmosphere (the ionosphere). The mainland radars were constructed about 30 years ago, based on technological solutions of that time. The science drivers of today, however, require a more flexible instrument, which allows measurements to be made from the troposphere to the topside ionosphere and gives the measured parameters in three dimensions, not just along a single radar beam. The possibility for continuous operation is also an essential feature. To facilitatefuture science work with a world-leading IS radar facility, planning of a new radar system started first with an EU-funded Design Study (2005–2009) and has continued with a follow-up EU FP7 EISCAT_3D Preparatory Phase project (2010–2014). The radar facility will be realised by using phased arrays, and a key aspect is the use of advanced software and data processing techniques. This type of software radar will act as a pathfinder for other facilities worldwide. The new radar facility will enable the EISCAT_3D science community to address new, significant science questions as well as to serve society, which is increasingly dependent on space-based technology and issues related to space weather. The location of the radar within the auroral oval and at the edge of the stratospheric polar vortex is also ideal for studies of the long-term variability in the atmosphere and global change. This paper is a summary of the EISCAT_3D science case, which was prepared as part of the EU-funded Preparatory Phase project for the new facility. Three science working groups, drawn from the EISCAT user community, participated in preparing this document. In addition to these working group members, who are listed as authors, thanks are due to many ... Article in Journal/Newspaper EISCAT Svalbard Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Svalbard Progress in Earth and Planetary Science 2 1 |
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Open Polar |
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Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
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ftingv |
language |
English |
description |
The EISCAT (European Incoherent SCATer) Scientific Association has provided versatile incoherent scatter (IS) radar facilities on the mainland of northern Scandinavia (the EISCAT UHF and VHF radar systems) and on Svalbard (the electronically scanning radar ESR (EISCAT Svalbard Radar) for studies of the high-latitude ionised upper atmosphere (the ionosphere). The mainland radars were constructed about 30 years ago, based on technological solutions of that time. The science drivers of today, however, require a more flexible instrument, which allows measurements to be made from the troposphere to the topside ionosphere and gives the measured parameters in three dimensions, not just along a single radar beam. The possibility for continuous operation is also an essential feature. To facilitatefuture science work with a world-leading IS radar facility, planning of a new radar system started first with an EU-funded Design Study (2005–2009) and has continued with a follow-up EU FP7 EISCAT_3D Preparatory Phase project (2010–2014). The radar facility will be realised by using phased arrays, and a key aspect is the use of advanced software and data processing techniques. This type of software radar will act as a pathfinder for other facilities worldwide. The new radar facility will enable the EISCAT_3D science community to address new, significant science questions as well as to serve society, which is increasingly dependent on space-based technology and issues related to space weather. The location of the radar within the auroral oval and at the edge of the stratospheric polar vortex is also ideal for studies of the long-term variability in the atmosphere and global change. This paper is a summary of the EISCAT_3D science case, which was prepared as part of the EU-funded Preparatory Phase project for the new facility. Three science working groups, drawn from the EISCAT user community, participated in preparing this document. In addition to these working group members, who are listed as authors, thanks are due to many ... |
author2 |
#PLACEHOLDER_PARENT_METADATA_VALUE# Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia |
format |
Article in Journal/Newspaper |
author |
McCrea, Ian Aikio, Anita Alfonsi, Lucilla Belova, Evgenia Buchert, Stephan Clilverd, Mark Engler, Norbert Gustavsson, Björn Heinselman, Craig Kero, Johan Kosch, Mike Lamy, Hervé Leyser, Thomas Ogawa, Yasunobu Oksavik, Kjellmar Pellinen-Wannberg, Asta Pitout, Frederic Rapp, Markus Stanislawska, Iwona Vierinen, Juha |
spellingShingle |
McCrea, Ian Aikio, Anita Alfonsi, Lucilla Belova, Evgenia Buchert, Stephan Clilverd, Mark Engler, Norbert Gustavsson, Björn Heinselman, Craig Kero, Johan Kosch, Mike Lamy, Hervé Leyser, Thomas Ogawa, Yasunobu Oksavik, Kjellmar Pellinen-Wannberg, Asta Pitout, Frederic Rapp, Markus Stanislawska, Iwona Vierinen, Juha The science case for the EISCAT_3D radar |
author_facet |
McCrea, Ian Aikio, Anita Alfonsi, Lucilla Belova, Evgenia Buchert, Stephan Clilverd, Mark Engler, Norbert Gustavsson, Björn Heinselman, Craig Kero, Johan Kosch, Mike Lamy, Hervé Leyser, Thomas Ogawa, Yasunobu Oksavik, Kjellmar Pellinen-Wannberg, Asta Pitout, Frederic Rapp, Markus Stanislawska, Iwona Vierinen, Juha |
author_sort |
McCrea, Ian |
title |
The science case for the EISCAT_3D radar |
title_short |
The science case for the EISCAT_3D radar |
title_full |
The science case for the EISCAT_3D radar |
title_fullStr |
The science case for the EISCAT_3D radar |
title_full_unstemmed |
The science case for the EISCAT_3D radar |
title_sort |
science case for the eiscat_3d radar |
publishDate |
2015 |
url |
http://hdl.handle.net/2122/10956 https://doi.org/10.1186/s40645-015-0051-8 |
geographic |
Svalbard |
geographic_facet |
Svalbard |
genre |
EISCAT Svalbard |
genre_facet |
EISCAT Svalbard |
op_relation |
Progress in Earth and Planetary Science 2 http://hdl.handle.net/2122/10956 doi:10.1186/s40645-015-0051-8 |
op_rights |
open |
op_doi |
https://doi.org/10.1186/s40645-015-0051-8 |
container_title |
Progress in Earth and Planetary Science |
container_volume |
2 |
container_issue |
1 |
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1766400062648221696 |