Planetary Wave Spectrum in the Stratosphere–Mesosphere during Sudden Stratospheric Warming 2018

The planetary wave activity in the stratosphere–mesosphere during the Arctic major Sudden Stratospheric Warming (SSW) in February 2018 is discussed on the basis of microwave radiometer (MWR) measurements of carbon monoxide (CO) above Kharkiv, Ukraine (50.0° N, 36.3° E) and the Aura Microwave Limb So...

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Published in:Remote Sensing
Main Authors: Yuke Wang, Gennadi Milinevsky, Oleksandr Evtushevsky, Andrew Klekociuk, Wei Han, Asen Grytsai, Oleksandr Antyufeyev, Yu Shi, Oksana Ivaniha, Valerii Shulga
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
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Online Access:https://doi.org/10.3390/rs13061190
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author Yuke Wang
Gennadi Milinevsky
Oleksandr Evtushevsky
Andrew Klekociuk
Wei Han
Asen Grytsai
Oleksandr Antyufeyev
Yu Shi
Oksana Ivaniha
Valerii Shulga
author_facet Yuke Wang
Gennadi Milinevsky
Oleksandr Evtushevsky
Andrew Klekociuk
Wei Han
Asen Grytsai
Oleksandr Antyufeyev
Yu Shi
Oksana Ivaniha
Valerii Shulga
author_sort Yuke Wang
collection MDPI Open Access Publishing
container_issue 6
container_start_page 1190
container_title Remote Sensing
container_volume 13
description The planetary wave activity in the stratosphere–mesosphere during the Arctic major Sudden Stratospheric Warming (SSW) in February 2018 is discussed on the basis of microwave radiometer (MWR) measurements of carbon monoxide (CO) above Kharkiv, Ukraine (50.0° N, 36.3° E) and the Aura Microwave Limb Sounder (MLS) measurements of CO, temperature and geopotential heights. From the MLS data, eastward and westward migrations of wave 1/wave 2 spectral components were differentiated, to which less attention was paid in previous studies. Abrupt changes in zonal wave spectra occurred with the zonal wind reversal near 10 February 2018. Eastward wave 1 and wave 2 were observed before the SSW onset and disappeared during the SSW event, when westward wave 1 became dominant. Wavelet power spectra of mesospheric CO variations showed statistically significant periods of 20–30 days using both MWR and MLS data. Although westward wave 1 in the mesosphere dominated with the onset of the SSW 2018, it developed independently of stratospheric dynamics. Since the propagation of upward planetary waves was limited in the easterly zonal flow in the stratosphere during SSW, forced planetary waves in the mid-latitude mesosphere may exist due to the instability of the zonal flow.
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op_doi https://doi.org/10.3390/rs13061190
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op_rights https://creativecommons.org/licenses/by/4.0/
op_source Remote Sensing; Volume 13; Issue 6; Pages: 1190
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spelling ftmdpi:oai:mdpi.com:/2072-4292/13/6/1190/ 2025-01-16T20:39:25+00:00 Planetary Wave Spectrum in the Stratosphere–Mesosphere during Sudden Stratospheric Warming 2018 Yuke Wang Gennadi Milinevsky Oleksandr Evtushevsky Andrew Klekociuk Wei Han Asen Grytsai Oleksandr Antyufeyev Yu Shi Oksana Ivaniha Valerii Shulga agris 2021-03-20 application/pdf https://doi.org/10.3390/rs13061190 EN eng Multidisciplinary Digital Publishing Institute Atmospheric Remote Sensing https://dx.doi.org/10.3390/rs13061190 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 13; Issue 6; Pages: 1190 planetary wave mesosphere stratosphere major sudden stratospheric warming microwave radiometer carbon monoxide wavelet power spectra Text 2021 ftmdpi https://doi.org/10.3390/rs13061190 2023-08-01T01:19:49Z The planetary wave activity in the stratosphere–mesosphere during the Arctic major Sudden Stratospheric Warming (SSW) in February 2018 is discussed on the basis of microwave radiometer (MWR) measurements of carbon monoxide (CO) above Kharkiv, Ukraine (50.0° N, 36.3° E) and the Aura Microwave Limb Sounder (MLS) measurements of CO, temperature and geopotential heights. From the MLS data, eastward and westward migrations of wave 1/wave 2 spectral components were differentiated, to which less attention was paid in previous studies. Abrupt changes in zonal wave spectra occurred with the zonal wind reversal near 10 February 2018. Eastward wave 1 and wave 2 were observed before the SSW onset and disappeared during the SSW event, when westward wave 1 became dominant. Wavelet power spectra of mesospheric CO variations showed statistically significant periods of 20–30 days using both MWR and MLS data. Although westward wave 1 in the mesosphere dominated with the onset of the SSW 2018, it developed independently of stratospheric dynamics. Since the propagation of upward planetary waves was limited in the easterly zonal flow in the stratosphere during SSW, forced planetary waves in the mid-latitude mesosphere may exist due to the instability of the zonal flow. Text Arctic MDPI Open Access Publishing Arctic Remote Sensing 13 6 1190
spellingShingle planetary wave
mesosphere
stratosphere
major sudden stratospheric warming
microwave radiometer
carbon monoxide
wavelet power spectra
Yuke Wang
Gennadi Milinevsky
Oleksandr Evtushevsky
Andrew Klekociuk
Wei Han
Asen Grytsai
Oleksandr Antyufeyev
Yu Shi
Oksana Ivaniha
Valerii Shulga
Planetary Wave Spectrum in the Stratosphere–Mesosphere during Sudden Stratospheric Warming 2018
title Planetary Wave Spectrum in the Stratosphere–Mesosphere during Sudden Stratospheric Warming 2018
title_full Planetary Wave Spectrum in the Stratosphere–Mesosphere during Sudden Stratospheric Warming 2018
title_fullStr Planetary Wave Spectrum in the Stratosphere–Mesosphere during Sudden Stratospheric Warming 2018
title_full_unstemmed Planetary Wave Spectrum in the Stratosphere–Mesosphere during Sudden Stratospheric Warming 2018
title_short Planetary Wave Spectrum in the Stratosphere–Mesosphere during Sudden Stratospheric Warming 2018
title_sort planetary wave spectrum in the stratosphere–mesosphere during sudden stratospheric warming 2018
topic planetary wave
mesosphere
stratosphere
major sudden stratospheric warming
microwave radiometer
carbon monoxide
wavelet power spectra
topic_facet planetary wave
mesosphere
stratosphere
major sudden stratospheric warming
microwave radiometer
carbon monoxide
wavelet power spectra
url https://doi.org/10.3390/rs13061190