Observation of Kelvin–Helmholtz instabilities and gravity waves in the summer mesopause above Andenes in Northern Norway

We present observations obtained with the Middle Atmosphere Alomar Radar System (MAARSY) to investigate short-period wave-like features using polar mesospheric summer echoes (PMSEs) as a tracer for the neutral dynamics. We conducted a multibeam experiment including 67 different beam directions durin...

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Main Authors: Stober, Gunter, Sommer, Svenja, Schult, Carsten, Latteck, Ralph, Chau, Jorge L.
Format: Article in Journal/Newspaper
Language:English
Published: München : European Geopyhsical Union 2018
Subjects:
550
Online Access:https://doi.org/10.34657/1136
https://oa.tib.eu/renate/handle/123456789/879
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spelling ftleibnizopen:oai:oai.leibnizopen.de:ziePVYsBBwLIz6xGsgp6 2023-11-12T04:01:03+01:00 Observation of Kelvin–Helmholtz instabilities and gravity waves in the summer mesopause above Andenes in Northern Norway Stober, Gunter Sommer, Svenja Schult, Carsten Latteck, Ralph Chau, Jorge L. 2018 application/pdf https://doi.org/10.34657/1136 https://oa.tib.eu/renate/handle/123456789/879 eng eng München : European Geopyhsical Union CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ Atmospheric Chemistry and Physics, Volume 18, Issue 9, Page 6721-6732 550 article Text 2018 ftleibnizopen https://doi.org/10.34657/1136 2023-10-22T23:36:05Z We present observations obtained with the Middle Atmosphere Alomar Radar System (MAARSY) to investigate short-period wave-like features using polar mesospheric summer echoes (PMSEs) as a tracer for the neutral dynamics. We conducted a multibeam experiment including 67 different beam directions during a 9-day campaign in June 2013. We identified two Kelvin–Helmholtz instability (KHI) events from the signal morphology of PMSE. The MAARSY observations are complemented by collocated meteor radar wind data to determine the mesoscale gravity wave activity and the vertical structure of the wind field above the PMSE. The KHIs occurred in a strong shear flow with Richardson numbers Ri <0.25. In addition, we observed 15 wave-like events in our MAARSY multibeam observations applying a sophisticated decomposition of the radial velocity measurements using volume velocity processing. We retrieved the horizontal wavelength, intrinsic frequency, propagation direction, and phase speed from the horizontally resolved wind variability for 15 events. These events showed horizontal wavelengths between 20 and 40km, vertical wavelengths between 5 and 10km, and rather high intrinsic phase speeds between 45 and 85ms−1 with intrinsic periods of 5–10min. Leibniz_Fonds publishedVersion Article in Journal/Newspaper Andenes Northern Norway Unknown Alomar ENVELOPE(-67.083,-67.083,-68.133,-68.133) Norway
institution Open Polar
collection Unknown
op_collection_id ftleibnizopen
language English
topic 550
spellingShingle 550
Stober, Gunter
Sommer, Svenja
Schult, Carsten
Latteck, Ralph
Chau, Jorge L.
Observation of Kelvin–Helmholtz instabilities and gravity waves in the summer mesopause above Andenes in Northern Norway
topic_facet 550
description We present observations obtained with the Middle Atmosphere Alomar Radar System (MAARSY) to investigate short-period wave-like features using polar mesospheric summer echoes (PMSEs) as a tracer for the neutral dynamics. We conducted a multibeam experiment including 67 different beam directions during a 9-day campaign in June 2013. We identified two Kelvin–Helmholtz instability (KHI) events from the signal morphology of PMSE. The MAARSY observations are complemented by collocated meteor radar wind data to determine the mesoscale gravity wave activity and the vertical structure of the wind field above the PMSE. The KHIs occurred in a strong shear flow with Richardson numbers Ri <0.25. In addition, we observed 15 wave-like events in our MAARSY multibeam observations applying a sophisticated decomposition of the radial velocity measurements using volume velocity processing. We retrieved the horizontal wavelength, intrinsic frequency, propagation direction, and phase speed from the horizontally resolved wind variability for 15 events. These events showed horizontal wavelengths between 20 and 40km, vertical wavelengths between 5 and 10km, and rather high intrinsic phase speeds between 45 and 85ms−1 with intrinsic periods of 5–10min. Leibniz_Fonds publishedVersion
format Article in Journal/Newspaper
author Stober, Gunter
Sommer, Svenja
Schult, Carsten
Latteck, Ralph
Chau, Jorge L.
author_facet Stober, Gunter
Sommer, Svenja
Schult, Carsten
Latteck, Ralph
Chau, Jorge L.
author_sort Stober, Gunter
title Observation of Kelvin–Helmholtz instabilities and gravity waves in the summer mesopause above Andenes in Northern Norway
title_short Observation of Kelvin–Helmholtz instabilities and gravity waves in the summer mesopause above Andenes in Northern Norway
title_full Observation of Kelvin–Helmholtz instabilities and gravity waves in the summer mesopause above Andenes in Northern Norway
title_fullStr Observation of Kelvin–Helmholtz instabilities and gravity waves in the summer mesopause above Andenes in Northern Norway
title_full_unstemmed Observation of Kelvin–Helmholtz instabilities and gravity waves in the summer mesopause above Andenes in Northern Norway
title_sort observation of kelvin–helmholtz instabilities and gravity waves in the summer mesopause above andenes in northern norway
publisher München : European Geopyhsical Union
publishDate 2018
url https://doi.org/10.34657/1136
https://oa.tib.eu/renate/handle/123456789/879
long_lat ENVELOPE(-67.083,-67.083,-68.133,-68.133)
geographic Alomar
Norway
geographic_facet Alomar
Norway
genre Andenes
Northern Norway
genre_facet Andenes
Northern Norway
op_source Atmospheric Chemistry and Physics, Volume 18, Issue 9, Page 6721-6732
op_rights CC BY 4.0 Unported
https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.34657/1136
_version_ 1782329483894718464