INTERACTION BETWEEN ANTARCTIC SEA ICE AND ENSO EVENTS
In this paper, the theory of the cross-coupled correlation-resonance of two wave spectra is used to study the interaction between Antarctic sea ice and ENSO events. It is found that : (1) The principal period of the correlation time series oscillation is usually coincident with the principal period...
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National Research Center for Marine Environment Forecasts
1994
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ftnipr:oai:nipr.repo.nii.ac.jp:00003828 2023-05-15T13:49:01+02:00 INTERACTION BETWEEN ANTARCTIC SEA ICE AND ENSO EVENTS / / Simei XIE Chenglan BAO Zhenhe XUE Lin ZHANG Chunjiang HAO 1994-11 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3828 http://id.nii.ac.jp/1291/00003828/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3828&item_no=1&attribute_id=18&file_no=1 en eng National Research Center for Marine Environment Forecasts National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3828 http://id.nii.ac.jp/1291/00003828/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 8, 95-110(1994-11) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3828&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1994 ftnipr 2022-12-17T19:45:54Z In this paper, the theory of the cross-coupled correlation-resonance of two wave spectra is used to study the interaction between Antarctic sea ice and ENSO events. It is found that : (1) The principal period of the correlation time series oscillation is usually coincident with the principal period of sea ice itself. If the same periods of two elements were in resonance, the correlation oscillation period would be more significant. (2) The sea ice of the Ross Sea area with its principal period of quasi-11 years has a strong cross correlation oscillation with SSTA of Nino 4. Their common period produces a resonance from 96 months leading to 36 months lagging causing a sine-shaped correlation variation with a strong positive SSTA from 87 to 50 months leading and a strong negative one from 20 months leading to 24 months lagging. (3) The same is true for the Weddell Sea ice and SSTA of the central-eastern equatorial Pacific but with a common period of quasi-5 years. ENSO events have a good correlation with sea ice in the eastern Antarctic in their later stage. The feedback of sea ice to SSTA in the western equatorial Pacific is also significant with a quasi-5 year period, but it is very weak to SSTA of the central-eastern equatorial Pacific. SST of the central equatorial Pacific has a quasi-contemporary oscillation relationship with Ross Sea ice and a 1.5 years lag oscillation relationship with Weddell Sea ice. We call this oscillation relationship between Antarctic sea ice and ENSO events, the Southern Oceanic Oscillation (SOO). Report Antarc* Antarctic Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology Ross Sea Sea ice Weddell Sea National Institute of Polar Research Repository, Japan Antarctic Weddell Sea Ross Sea Pacific Weddell |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
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ftnipr |
language |
English |
description |
In this paper, the theory of the cross-coupled correlation-resonance of two wave spectra is used to study the interaction between Antarctic sea ice and ENSO events. It is found that : (1) The principal period of the correlation time series oscillation is usually coincident with the principal period of sea ice itself. If the same periods of two elements were in resonance, the correlation oscillation period would be more significant. (2) The sea ice of the Ross Sea area with its principal period of quasi-11 years has a strong cross correlation oscillation with SSTA of Nino 4. Their common period produces a resonance from 96 months leading to 36 months lagging causing a sine-shaped correlation variation with a strong positive SSTA from 87 to 50 months leading and a strong negative one from 20 months leading to 24 months lagging. (3) The same is true for the Weddell Sea ice and SSTA of the central-eastern equatorial Pacific but with a common period of quasi-5 years. ENSO events have a good correlation with sea ice in the eastern Antarctic in their later stage. The feedback of sea ice to SSTA in the western equatorial Pacific is also significant with a quasi-5 year period, but it is very weak to SSTA of the central-eastern equatorial Pacific. SST of the central equatorial Pacific has a quasi-contemporary oscillation relationship with Ross Sea ice and a 1.5 years lag oscillation relationship with Weddell Sea ice. We call this oscillation relationship between Antarctic sea ice and ENSO events, the Southern Oceanic Oscillation (SOO). |
format |
Report |
author |
/ / Simei XIE Chenglan BAO Zhenhe XUE Lin ZHANG Chunjiang HAO |
spellingShingle |
/ / Simei XIE Chenglan BAO Zhenhe XUE Lin ZHANG Chunjiang HAO INTERACTION BETWEEN ANTARCTIC SEA ICE AND ENSO EVENTS |
author_facet |
/ / Simei XIE Chenglan BAO Zhenhe XUE Lin ZHANG Chunjiang HAO |
author_sort |
/ / |
title |
INTERACTION BETWEEN ANTARCTIC SEA ICE AND ENSO EVENTS |
title_short |
INTERACTION BETWEEN ANTARCTIC SEA ICE AND ENSO EVENTS |
title_full |
INTERACTION BETWEEN ANTARCTIC SEA ICE AND ENSO EVENTS |
title_fullStr |
INTERACTION BETWEEN ANTARCTIC SEA ICE AND ENSO EVENTS |
title_full_unstemmed |
INTERACTION BETWEEN ANTARCTIC SEA ICE AND ENSO EVENTS |
title_sort |
interaction between antarctic sea ice and enso events |
publisher |
National Research Center for Marine Environment Forecasts |
publishDate |
1994 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3828 http://id.nii.ac.jp/1291/00003828/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3828&item_no=1&attribute_id=18&file_no=1 |
geographic |
Antarctic Weddell Sea Ross Sea Pacific Weddell |
geographic_facet |
Antarctic Weddell Sea Ross Sea Pacific Weddell |
genre |
Antarc* Antarctic Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology Ross Sea Sea ice Weddell Sea |
genre_facet |
Antarc* Antarctic Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology Ross Sea Sea ice Weddell Sea |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3828 http://id.nii.ac.jp/1291/00003828/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 8, 95-110(1994-11) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3828&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250437411864576 |