A comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and MF radar at 69 ° N

The Andenes Meteor Radar (MR) and the Saura Medium Frequency (MF) Radar are located in northern Norway (69° N, 16° E) and operate continuously to provide wind measurements of the mesosphere and lower thermosphere (MLT) region. We compare the two systems to find potential biases between the radars an...

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Published in:Annales Geophysicae
Main Authors: Wilhelm, Sven, Stober, Gunter, Chau, Jorge L.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-35-893-2017
https://angeo.copernicus.org/articles/35/893/2017/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo57351 2023-05-15T13:25:22+02:00 A comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and MF radar at 69 ° N Wilhelm, Sven Stober, Gunter Chau, Jorge L. 2018-09-27 application/pdf https://doi.org/10.5194/angeo-35-893-2017 https://angeo.copernicus.org/articles/35/893/2017/ eng eng doi:10.5194/angeo-35-893-2017 https://angeo.copernicus.org/articles/35/893/2017/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-35-893-2017 2020-07-20T16:23:38Z The Andenes Meteor Radar (MR) and the Saura Medium Frequency (MF) Radar are located in northern Norway (69° N, 16° E) and operate continuously to provide wind measurements of the mesosphere and lower thermosphere (MLT) region. We compare the two systems to find potential biases between the radars and combine the data from both systems to enhance altitudinal coverage between 60 and 110 km. The systems have altitudinal overlap between 78 and 100 km at which we compare winds and tides on the basis of hourly winds with 2 km altitude bins. Our results indicate reasonable agreement for the zonal and meridional wind components between 78 and 92 km. An exception to this is the altitude range below 84 km during the summer, at which the correlation decreases. We also compare semidiurnal and diurnal tides according to their amplitudes and phases with good agreement below 90 km for the diurnal and below 96 km for the semidiurnal tides. Based on these findings we have taken the MR data as a reference. By comparing the MF and MR winds within the overlapping region, we have empirically estimated correction factors to be applied to the MF winds. Existing gaps in that data set will be filled with weighted MF data. This weighting is done due to underestimated wind values of the MF compared to the MR, and the resulting correction factors fit to a polynomial function of second degree within the overlapping area. We are therefore able to construct a consistent and homogenous wind from approximately 60 to 110 km. Text Andenes Northern Norway Copernicus Publications: E-Journals Norway Saura ENVELOPE(12.989,12.989,66.233,66.233) Annales Geophysicae 35 4 893 906
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The Andenes Meteor Radar (MR) and the Saura Medium Frequency (MF) Radar are located in northern Norway (69° N, 16° E) and operate continuously to provide wind measurements of the mesosphere and lower thermosphere (MLT) region. We compare the two systems to find potential biases between the radars and combine the data from both systems to enhance altitudinal coverage between 60 and 110 km. The systems have altitudinal overlap between 78 and 100 km at which we compare winds and tides on the basis of hourly winds with 2 km altitude bins. Our results indicate reasonable agreement for the zonal and meridional wind components between 78 and 92 km. An exception to this is the altitude range below 84 km during the summer, at which the correlation decreases. We also compare semidiurnal and diurnal tides according to their amplitudes and phases with good agreement below 90 km for the diurnal and below 96 km for the semidiurnal tides. Based on these findings we have taken the MR data as a reference. By comparing the MF and MR winds within the overlapping region, we have empirically estimated correction factors to be applied to the MF winds. Existing gaps in that data set will be filled with weighted MF data. This weighting is done due to underestimated wind values of the MF compared to the MR, and the resulting correction factors fit to a polynomial function of second degree within the overlapping area. We are therefore able to construct a consistent and homogenous wind from approximately 60 to 110 km.
format Text
author Wilhelm, Sven
Stober, Gunter
Chau, Jorge L.
spellingShingle Wilhelm, Sven
Stober, Gunter
Chau, Jorge L.
A comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and MF radar at 69 ° N
author_facet Wilhelm, Sven
Stober, Gunter
Chau, Jorge L.
author_sort Wilhelm, Sven
title A comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and MF radar at 69 ° N
title_short A comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and MF radar at 69 ° N
title_full A comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and MF radar at 69 ° N
title_fullStr A comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and MF radar at 69 ° N
title_full_unstemmed A comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and MF radar at 69 ° N
title_sort comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and mf radar at 69 ° n
publishDate 2018
url https://doi.org/10.5194/angeo-35-893-2017
https://angeo.copernicus.org/articles/35/893/2017/
long_lat ENVELOPE(12.989,12.989,66.233,66.233)
geographic Norway
Saura
geographic_facet Norway
Saura
genre Andenes
Northern Norway
genre_facet Andenes
Northern Norway
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-35-893-2017
https://angeo.copernicus.org/articles/35/893/2017/
op_doi https://doi.org/10.5194/angeo-35-893-2017
container_title Annales Geophysicae
container_volume 35
container_issue 4
container_start_page 893
op_container_end_page 906
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