Five-day planetary waves as seen by the Odin satellite and the ground-based Kiruna millimeter wave radiometer in January–March 2005

The signature of five-day planetary waves in ozone and temperature data from the advanced sub-millimeter radiometer aboard the Odin satellite is examined. The period January–March 2005 and heights from 24–56 km are used. We find highest wave amplitudes in both temperature and ozone in the winter hem...

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Published in:Canadian Journal of Physics
Main Authors: Belova, Alla, Kirkwood, Sheila, Raffalski, U, Kopp, Gerhard, Hochschild, Gerd, Urban, Joachim
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2008
Subjects:
Online Access:http://dx.doi.org/10.1139/p07-172
http://www.nrcresearchpress.com/doi/pdf/10.1139/p07-172
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spelling crcansciencepubl:10.1139/p07-172 2023-12-17T10:32:56+01:00 Five-day planetary waves as seen by the Odin satellite and the ground-based Kiruna millimeter wave radiometer in January–March 2005 Belova, Alla Kirkwood, Sheila Raffalski, U Kopp, Gerhard Hochschild, Gerd Urban, Joachim 2008 http://dx.doi.org/10.1139/p07-172 http://www.nrcresearchpress.com/doi/pdf/10.1139/p07-172 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Physics volume 86, issue 3, page 459-466 ISSN 0008-4204 1208-6045 General Physics and Astronomy journal-article 2008 crcansciencepubl https://doi.org/10.1139/p07-172 2023-11-19T13:39:06Z The signature of five-day planetary waves in ozone and temperature data from the advanced sub-millimeter radiometer aboard the Odin satellite is examined. The period January–March 2005 and heights from 24–56 km are used. We find highest wave amplitudes in both temperature and ozone in the winter hemisphere at 60°N-70°N. The relative phases between ozone and temperature perturbations show the expected antiphase behaviour in the photochemistry-dominated region at about 40 km altitude. We compare the global planetary wave properties from Odin with five-day perturbations in ozone measured by the millimeter wave radiometer in Kiruna (KIMRA, 67°N, 20°E). In the early part of the comparison interval (January–February) at 40 km, we find good correlation between the two in terms of both phase and amplitude of the perturbations. In the latter part of the comparison interval (March) where mean ozone levels are higher, the amplitudes of the ozone five-day perturbations over Kiruna are much higher than the wave amplitudes found using Odin. We conclude that five-day variations in ozone due to planetary waves can be detected by KIMRA in some circumstances, but that other sources of variability dominate at other heights and times. PACS No.: 94.10.Jd Article in Journal/Newspaper Kiruna Canadian Science Publishing (via Crossref) Kiruna Canadian Journal of Physics 86 3 459 466
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic General Physics and Astronomy
spellingShingle General Physics and Astronomy
Belova, Alla
Kirkwood, Sheila
Raffalski, U
Kopp, Gerhard
Hochschild, Gerd
Urban, Joachim
Five-day planetary waves as seen by the Odin satellite and the ground-based Kiruna millimeter wave radiometer in January–March 2005
topic_facet General Physics and Astronomy
description The signature of five-day planetary waves in ozone and temperature data from the advanced sub-millimeter radiometer aboard the Odin satellite is examined. The period January–March 2005 and heights from 24–56 km are used. We find highest wave amplitudes in both temperature and ozone in the winter hemisphere at 60°N-70°N. The relative phases between ozone and temperature perturbations show the expected antiphase behaviour in the photochemistry-dominated region at about 40 km altitude. We compare the global planetary wave properties from Odin with five-day perturbations in ozone measured by the millimeter wave radiometer in Kiruna (KIMRA, 67°N, 20°E). In the early part of the comparison interval (January–February) at 40 km, we find good correlation between the two in terms of both phase and amplitude of the perturbations. In the latter part of the comparison interval (March) where mean ozone levels are higher, the amplitudes of the ozone five-day perturbations over Kiruna are much higher than the wave amplitudes found using Odin. We conclude that five-day variations in ozone due to planetary waves can be detected by KIMRA in some circumstances, but that other sources of variability dominate at other heights and times. PACS No.: 94.10.Jd
format Article in Journal/Newspaper
author Belova, Alla
Kirkwood, Sheila
Raffalski, U
Kopp, Gerhard
Hochschild, Gerd
Urban, Joachim
author_facet Belova, Alla
Kirkwood, Sheila
Raffalski, U
Kopp, Gerhard
Hochschild, Gerd
Urban, Joachim
author_sort Belova, Alla
title Five-day planetary waves as seen by the Odin satellite and the ground-based Kiruna millimeter wave radiometer in January–March 2005
title_short Five-day planetary waves as seen by the Odin satellite and the ground-based Kiruna millimeter wave radiometer in January–March 2005
title_full Five-day planetary waves as seen by the Odin satellite and the ground-based Kiruna millimeter wave radiometer in January–March 2005
title_fullStr Five-day planetary waves as seen by the Odin satellite and the ground-based Kiruna millimeter wave radiometer in January–March 2005
title_full_unstemmed Five-day planetary waves as seen by the Odin satellite and the ground-based Kiruna millimeter wave radiometer in January–March 2005
title_sort five-day planetary waves as seen by the odin satellite and the ground-based kiruna millimeter wave radiometer in january–march 2005
publisher Canadian Science Publishing
publishDate 2008
url http://dx.doi.org/10.1139/p07-172
http://www.nrcresearchpress.com/doi/pdf/10.1139/p07-172
geographic Kiruna
geographic_facet Kiruna
genre Kiruna
genre_facet Kiruna
op_source Canadian Journal of Physics
volume 86, issue 3, page 459-466
ISSN 0008-4204 1208-6045
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/p07-172
container_title Canadian Journal of Physics
container_volume 86
container_issue 3
container_start_page 459
op_container_end_page 466
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