Vertical mixing in the lower troposphere by mountain waves over Arctic Scandinavia
Document identifier: oai:DiVA.org:ltu-7641
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10.5194/acpd-11-31475-2011Keyword: Engineering and Technology,
Mechanical Engineering,
Aerospace Engineering,
Teknik och teknologier,
Maskinteknik,
Rymd- och flygteknik,
Rymdteknik,
Space TechnologyPublication year: 2011Relevant Sustainable Development Goals (SDGs):

The SDG label(s) above have been assigned by OSDG.aiAbstract: Measurements made by ozonesondes and by a 52 MHz wind-profiling radar during February and March 1997 are studied. The radar is located at Esrange, near Kiruna in Arctic Sweden, on the eastern flank of the Scandinavian mountains. Daily ozonesondes were launched from the same site. The radar vertical and horizontal wind measurements are used to identify times when mountain waves were present. Mean vertical gradients in ozone mixing ratio in the lower troposphere are determined in conditions with mountain waves present and when they were absent. Back-trajectories were calculated so that only air-masses with their origin to the west of the mountains were included in the final averages. The vertical gradient in ozone mixing ratio is found to be about twice as steep outside wave conditions as it is during mountain waves. This suggests a very high rate of vertical mixing, with an average eddy diffusivity of order 5000 m2 s−1. This is consistent with an earlier estimate of the occurrence rate of complete mixing by wave breaking over the mountain range.
Authors
Maria Mihalikova
Luleå tekniska universitet; Institutionen för system- och rymdteknik
Other publications
>>
Sheila Kirkwood
Luleå tekniska universitet; Rymdteknik
Other publications
>>
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identifier: oai:DiVA.org:ltu-7641
datestamp: 2021-04-19T11:02:37Z
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recordCreationDate: 2016-09-29
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http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-7641
10.5194/acpd-11-31475-2011
60afce1f-3308-4015-b07e-33194ac6904d
titleInfo:
@attributes:
lang: eng
title: Vertical mixing in the lower troposphere by mountain waves over Arctic Scandinavia
abstract: Measurements made by ozonesondes and by a 52 MHz wind-profiling radar during February and March 1997 are studied. The radar is located at Esrange near Kiruna in Arctic Sweden on the eastern flank of the Scandinavian mountains. Daily ozonesondes were launched from the same site. The radar vertical and horizontal wind measurements are used to identify times when mountain waves were present. Mean vertical gradients in ozone mixing ratio in the lower troposphere are determined in conditions with mountain waves present and when they were absent. Back-trajectories were calculated so that only air-masses with their origin to the west of the mountains were included in the final averages. The vertical gradient in ozone mixing ratio is found to be about twice as steep outside wave conditions as it is during mountain waves. This suggests a very high rate of vertical mixing with an average eddy diffusivity of order 5000 m2 s−1. This is consistent with an earlier estimate of the occurrence rate of complete mixing by wave breaking over the mountain range.
subject:
@attributes:
lang: eng
authority: uka.se
topic:
Engineering and Technology
Mechanical Engineering
Aerospace Engineering
@attributes:
lang: swe
authority: uka.se
topic:
Teknik och teknologier
Maskinteknik
Rymd- och flygteknik
@attributes:
lang: swe
authority: ltu
topic: Rymdteknik
genre: Research subject
@attributes:
lang: eng
authority: ltu
topic: Space Technology
genre: Research subject
language:
languageTerm: eng
genre:
publication/journal-article
ref
note:
Published
2
Validerad; 2011; 20160610 (andbra)
name:
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type: personal
authority: ltu
namePart:
Mihalikova
Maria
role:
roleTerm: aut
affiliation:
Luleå tekniska universitet
Institutionen för system- och rymdteknik
nameIdentifier: marmih
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type: personal
authority: ltu
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Kirkwood
Sheila
role:
roleTerm: aut
affiliation:
Luleå tekniska universitet
Rymdteknik
nameIdentifier: shekir
originInfo:
dateIssued: 2011
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type: host
titleInfo:
title: Atmospheric Chemistry And Physics
identifier:
1680-7316
1680-7324
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detail:
@attributes:
type: volume
number: 11
extent:
start: 31475
end: 31493
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form: print
typeOfResource: text