Daily to intraseasonal oscillations at Antarctic research station Neumayer

Abstract High temporal resolution (three hours) records of temperature, wind speed and sea level pressure recorded at Antarctic research station Neumayer (70°S, 8°W) during 1982–2011 are analysed to identify oscillations from daily to intraseasonal timescales. The diurnal cycle dominates the three-h...

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Published in:Antarctic Science
Main Authors: Rimbu, N., Lohmann, G., König-Langlo, G., Necula, C., Ionita, M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2013
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102013000540
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102013000540
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spelling crcambridgeupr:10.1017/s0954102013000540 2024-03-03T08:37:07+00:00 Daily to intraseasonal oscillations at Antarctic research station Neumayer Rimbu, N. Lohmann, G. König-Langlo, G. Necula, C. Ionita, M. 2013 http://dx.doi.org/10.1017/s0954102013000540 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102013000540 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by-nc-sa/3.0/ Antarctic Science volume 26, issue 2, page 193-204 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2013 crcambridgeupr https://doi.org/10.1017/s0954102013000540 2024-02-08T08:33:34Z Abstract High temporal resolution (three hours) records of temperature, wind speed and sea level pressure recorded at Antarctic research station Neumayer (70°S, 8°W) during 1982–2011 are analysed to identify oscillations from daily to intraseasonal timescales. The diurnal cycle dominates the three-hourly time series of temperature during the Antarctic summer and is almost absent during winter. In contrast, the three-hourly time series of wind speed and sea level pressure show a weak diurnal cycle. The dominant pattern of the intraseasonal variability of these quantities, which captures the out-of-phase variation of temperature and wind speed with sea level pressure, shows enhanced variability at timescales of ∼ 40 days and ∼ 80 days, respectively. Correlation and composite analysis reveal that these oscillations may be related to tropical intraseasonal oscillations via large-scale eastward propagating atmospheric circulation wave-trains. The second pattern of intraseasonal variability, which captures in-phase variations of temperature, wind and sea level pressure, shows enhanced variability at timescales of ∼ 35, ∼ 60 and ∼ 120 days. These oscillations are attributed to the Southern Annular Mode/Antarctic Oscillation (SAM/AAO) which shows enhanced variability at these timescales. We argue that intraseasonal oscillations of tropical climate and SAM/AAO are related to distinct patterns of climate variables measured at Neumayer. Article in Journal/Newspaper Antarc* Antarctic Antarctic Science Cambridge University Press Antarctic The Antarctic Neumayer Antarctic Science 26 2 193 204
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
spellingShingle Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Rimbu, N.
Lohmann, G.
König-Langlo, G.
Necula, C.
Ionita, M.
Daily to intraseasonal oscillations at Antarctic research station Neumayer
topic_facet Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
description Abstract High temporal resolution (three hours) records of temperature, wind speed and sea level pressure recorded at Antarctic research station Neumayer (70°S, 8°W) during 1982–2011 are analysed to identify oscillations from daily to intraseasonal timescales. The diurnal cycle dominates the three-hourly time series of temperature during the Antarctic summer and is almost absent during winter. In contrast, the three-hourly time series of wind speed and sea level pressure show a weak diurnal cycle. The dominant pattern of the intraseasonal variability of these quantities, which captures the out-of-phase variation of temperature and wind speed with sea level pressure, shows enhanced variability at timescales of ∼ 40 days and ∼ 80 days, respectively. Correlation and composite analysis reveal that these oscillations may be related to tropical intraseasonal oscillations via large-scale eastward propagating atmospheric circulation wave-trains. The second pattern of intraseasonal variability, which captures in-phase variations of temperature, wind and sea level pressure, shows enhanced variability at timescales of ∼ 35, ∼ 60 and ∼ 120 days. These oscillations are attributed to the Southern Annular Mode/Antarctic Oscillation (SAM/AAO) which shows enhanced variability at these timescales. We argue that intraseasonal oscillations of tropical climate and SAM/AAO are related to distinct patterns of climate variables measured at Neumayer.
format Article in Journal/Newspaper
author Rimbu, N.
Lohmann, G.
König-Langlo, G.
Necula, C.
Ionita, M.
author_facet Rimbu, N.
Lohmann, G.
König-Langlo, G.
Necula, C.
Ionita, M.
author_sort Rimbu, N.
title Daily to intraseasonal oscillations at Antarctic research station Neumayer
title_short Daily to intraseasonal oscillations at Antarctic research station Neumayer
title_full Daily to intraseasonal oscillations at Antarctic research station Neumayer
title_fullStr Daily to intraseasonal oscillations at Antarctic research station Neumayer
title_full_unstemmed Daily to intraseasonal oscillations at Antarctic research station Neumayer
title_sort daily to intraseasonal oscillations at antarctic research station neumayer
publisher Cambridge University Press (CUP)
publishDate 2013
url http://dx.doi.org/10.1017/s0954102013000540
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102013000540
geographic Antarctic
The Antarctic
Neumayer
geographic_facet Antarctic
The Antarctic
Neumayer
genre Antarc*
Antarctic
Antarctic Science
genre_facet Antarc*
Antarctic
Antarctic Science
op_source Antarctic Science
volume 26, issue 2, page 193-204
ISSN 0954-1020 1365-2079
op_rights http://creativecommons.org/licenses/by-nc-sa/3.0/
op_doi https://doi.org/10.1017/s0954102013000540
container_title Antarctic Science
container_volume 26
container_issue 2
container_start_page 193
op_container_end_page 204
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