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: S. Wilhelm, G. Stober, J. L. Chau
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2017
Subjects:
Online Access:https://doi.org/10.5194/angeo-35-893-2017
https://doaj.org/article/c55682d701164d39b82398ccf49f4fad
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author S. Wilhelm
G. Stober
J. L. Chau
author_facet S. Wilhelm
G. Stober
J. L. Chau
author_sort S. Wilhelm
collection Directory of Open Access Journals: DOAJ Articles
container_issue 4
container_start_page 893
container_title Annales Geophysicae
container_volume 35
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.
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Northern Norway
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op_doi https://doi.org/10.5194/angeo-35-893-2017
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doi:10.5194/angeo-35-893-2017
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https://doaj.org/article/c55682d701164d39b82398ccf49f4fad
op_source Annales Geophysicae, Vol 35, Pp 893-906 (2017)
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spelling ftdoajarticles:oai:doaj.org/article:c55682d701164d39b82398ccf49f4fad 2025-01-16T18:55:48+00:00 A comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and MF radar at 69 ° N S. Wilhelm G. Stober J. L. Chau 2017-07-01T00:00:00Z https://doi.org/10.5194/angeo-35-893-2017 https://doaj.org/article/c55682d701164d39b82398ccf49f4fad EN eng Copernicus Publications https://www.ann-geophys.net/35/893/2017/angeo-35-893-2017.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-35-893-2017 0992-7689 1432-0576 https://doaj.org/article/c55682d701164d39b82398ccf49f4fad Annales Geophysicae, Vol 35, Pp 893-906 (2017) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2017 ftdoajarticles https://doi.org/10.5194/angeo-35-893-2017 2022-12-31T13:54:19Z 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. Article in Journal/Newspaper Andenes Northern Norway Directory of Open Access Journals: DOAJ Articles Norway Saura ENVELOPE(12.989,12.989,66.233,66.233) Annales Geophysicae 35 4 893 906
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
S. Wilhelm
G. Stober
J. L. Chau
A comparison of 11-year mesospheric and lower thermospheric winds determined by meteor and MF radar at 69 ° N
title 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_short 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
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
url https://doi.org/10.5194/angeo-35-893-2017
https://doaj.org/article/c55682d701164d39b82398ccf49f4fad