Aspects of intraseasonal variability of Antarctic sea ice in austral winter related to ENSO and SAM events

Article We performed an Empirical Orthogonal Function (EOF) analysis to assess the intraseasonal variability of 5–60 day band-pass filtered Antarctic sea-ice concentration in austral winter using a 20-year daily dataset from 1995 to 2014. Zonal wave number 3 dominated in the Antarctic, especially so...

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Published in:Journal of Glaciology
Main Authors: 馬場, 賢治, RENWICK, JAMES
Format: Other/Unknown Material
Language:English
Published: Cambridge University Press 2017
Subjects:
Online Access:https://rakuno.repo.nii.ac.jp/record/5696/files/R-2018-230_baba.pdf
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spelling ftrakunogakuenun:oai:rakuno.repo.nii.ac.jp:00005696 2023-10-01T03:51:12+02:00 Aspects of intraseasonal variability of Antarctic sea ice in austral winter related to ENSO and SAM events 馬場, 賢治 RENWICK, JAMES 2017-10 application/pdf https://rakuno.repo.nii.ac.jp/record/5696/files/R-2018-230_baba.pdf eng eng Cambridge University Press 0022-1430 http://dx.doi.org/10.1017/jog.2017.49 Journal of Glaciology 241 63 838 846 https://rakuno.repo.nii.ac.jp/record/5696/files/R-2018-230_baba.pdf © The Author(s) 2017 http://creativecommons.org/licenses/by/4.0/ | http://creativecommons.org/licenses/by/4.0/ atmosphere/ice/ocean interactions climate change sea ice VoR 2017 ftrakunogakuenun https://doi.org/10.1017/jog.2017.49 2023-09-02T20:29:54Z Article We performed an Empirical Orthogonal Function (EOF) analysis to assess the intraseasonal variability of 5–60 day band-pass filtered Antarctic sea-ice concentration in austral winter using a 20-year daily dataset from 1995 to 2014. Zonal wave number 3 dominated in the Antarctic, especially so across the west Antarctic. Results showed the coexistence of stationary and propagating wave components. A spectral analysis of the first two principal components (PCs) showed a similar structure for periods up to 15 days but generally more power in PC1 at longer periods. Regression analysis upon atmospheric fields using the first two PCs of sea-ice concentration showed a coherent wave number 3 pattern. The spatial phase delay between the sea-ice and mean sea-level pressure patterns suggests that meridional flow and associated temperature advection are important for modulating the sea-ice field. EOF analyses carried out separately for El Niño, La Niña and neutral years, and for Southern Annular Mode positive, negative and neutral periods, suggest that the spatial patterns of wave number 3 shift between subsets. The results also indicate that El Niño-Southern Oscillation and Southern Annular Mode affect stationary wave interactions between sea-ice and atmospheric fields on intraseasonal timescales. journal article Other/Unknown Material Antarc* Antarctic Journal of Glaciology Sea ice Rakuno Gakuen University: CLOVER Antarctic The Antarctic Austral Journal of Glaciology 63 241 838 846
institution Open Polar
collection Rakuno Gakuen University: CLOVER
op_collection_id ftrakunogakuenun
language English
topic atmosphere/ice/ocean interactions
climate change
sea ice
spellingShingle atmosphere/ice/ocean interactions
climate change
sea ice
馬場, 賢治
RENWICK, JAMES
Aspects of intraseasonal variability of Antarctic sea ice in austral winter related to ENSO and SAM events
topic_facet atmosphere/ice/ocean interactions
climate change
sea ice
description Article We performed an Empirical Orthogonal Function (EOF) analysis to assess the intraseasonal variability of 5–60 day band-pass filtered Antarctic sea-ice concentration in austral winter using a 20-year daily dataset from 1995 to 2014. Zonal wave number 3 dominated in the Antarctic, especially so across the west Antarctic. Results showed the coexistence of stationary and propagating wave components. A spectral analysis of the first two principal components (PCs) showed a similar structure for periods up to 15 days but generally more power in PC1 at longer periods. Regression analysis upon atmospheric fields using the first two PCs of sea-ice concentration showed a coherent wave number 3 pattern. The spatial phase delay between the sea-ice and mean sea-level pressure patterns suggests that meridional flow and associated temperature advection are important for modulating the sea-ice field. EOF analyses carried out separately for El Niño, La Niña and neutral years, and for Southern Annular Mode positive, negative and neutral periods, suggest that the spatial patterns of wave number 3 shift between subsets. The results also indicate that El Niño-Southern Oscillation and Southern Annular Mode affect stationary wave interactions between sea-ice and atmospheric fields on intraseasonal timescales. journal article
format Other/Unknown Material
author 馬場, 賢治
RENWICK, JAMES
author_facet 馬場, 賢治
RENWICK, JAMES
author_sort 馬場, 賢治
title Aspects of intraseasonal variability of Antarctic sea ice in austral winter related to ENSO and SAM events
title_short Aspects of intraseasonal variability of Antarctic sea ice in austral winter related to ENSO and SAM events
title_full Aspects of intraseasonal variability of Antarctic sea ice in austral winter related to ENSO and SAM events
title_fullStr Aspects of intraseasonal variability of Antarctic sea ice in austral winter related to ENSO and SAM events
title_full_unstemmed Aspects of intraseasonal variability of Antarctic sea ice in austral winter related to ENSO and SAM events
title_sort aspects of intraseasonal variability of antarctic sea ice in austral winter related to enso and sam events
publisher Cambridge University Press
publishDate 2017
url https://rakuno.repo.nii.ac.jp/record/5696/files/R-2018-230_baba.pdf
geographic Antarctic
The Antarctic
Austral
geographic_facet Antarctic
The Antarctic
Austral
genre Antarc*
Antarctic
Journal of Glaciology
Sea ice
genre_facet Antarc*
Antarctic
Journal of Glaciology
Sea ice
op_relation 0022-1430
http://dx.doi.org/10.1017/jog.2017.49
Journal of Glaciology
241
63
838
846
https://rakuno.repo.nii.ac.jp/record/5696/files/R-2018-230_baba.pdf
op_rights © The Author(s) 2017
http://creativecommons.org/licenses/by/4.0/ | http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2017.49
container_title Journal of Glaciology
container_volume 63
container_issue 241
container_start_page 838
op_container_end_page 846
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