Variability of Antarctic Intermediate Water south of Australia and its relationship with frontal waves
A streamfunction EOF method is applied to a time series of hydrographic sections in the Southern Ocean south of Australia to study water mass variations. Results show that there are large thermohaline variations north of the Subantarctic Front ( SAF) at 300-1500 dbar level, indicating upwelling and...
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ftchinacasciocas:oai:ir.qdio.ac.cn:337002/135875 2023-05-15T13:40:37+02:00 Variability of Antarctic Intermediate Water south of Australia and its relationship with frontal waves Zhang LinLin Yan XiaoMei Sun Che Hu DunXin 2016-08-01 http://ir.qdio.ac.cn/handle/337002/135875 https://doi.org/10.1007/s11430-015-0179-5 英语 eng SCIENCE CHINA-EARTH SCIENCES Zhang LinLin,Yan XiaoMei,Sun Che,et al. Variability of Antarctic Intermediate Water south of Australia and its relationship with frontal waves[J]. SCIENCE CHINA-EARTH SCIENCES,2016,59(8):1674-1682. http://ir.qdio.ac.cn/handle/337002/135875 doi:10.1007/s11430-015-0179-5 Antarctic Intermediate Water (Aaiw) Stream-coordinates Frontal Wave Eof Article 期刊论文 2016 ftchinacasciocas https://doi.org/10.1007/s11430-015-0179-5 2022-06-27T05:37:45Z A streamfunction EOF method is applied to a time series of hydrographic sections in the Southern Ocean south of Australia to study water mass variations. Results show that there are large thermohaline variations north of the Subantarctic Front ( SAF) at 300-1500 dbar level, indicating upwelling and downwelling of the Antarctic Intermediate Water ( AAIW) along isopycnal surfaces. Based on the latest altimeter product, Absolute Dynamic Topography, a mechanism due to frontal wave propagation is proposed to explain this phenomenon, and an index for frontal waves is defined. When the frontal wave is in positive ( negative) phase, the SAF flows northeastward ( southeastward) with the fresh AAIW downwelling ( upwelling). Such mesoscale processes greatly enhance cross-frontal exchanges of water masses. Spectral analysis shows that frontal waves in the Southern Ocean south of Australia are dominated by a period of about 130 days with a phase speed of 4 cm/s and a wavelength of 450 km. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Antarctic Southern Ocean The Antarctic Science China Earth Sciences 59 8 1674 1682 |
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Open Polar |
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Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR |
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ftchinacasciocas |
language |
English |
topic |
Antarctic Intermediate Water (Aaiw) Stream-coordinates Frontal Wave Eof |
spellingShingle |
Antarctic Intermediate Water (Aaiw) Stream-coordinates Frontal Wave Eof Zhang LinLin Yan XiaoMei Sun Che Hu DunXin Variability of Antarctic Intermediate Water south of Australia and its relationship with frontal waves |
topic_facet |
Antarctic Intermediate Water (Aaiw) Stream-coordinates Frontal Wave Eof |
description |
A streamfunction EOF method is applied to a time series of hydrographic sections in the Southern Ocean south of Australia to study water mass variations. Results show that there are large thermohaline variations north of the Subantarctic Front ( SAF) at 300-1500 dbar level, indicating upwelling and downwelling of the Antarctic Intermediate Water ( AAIW) along isopycnal surfaces. Based on the latest altimeter product, Absolute Dynamic Topography, a mechanism due to frontal wave propagation is proposed to explain this phenomenon, and an index for frontal waves is defined. When the frontal wave is in positive ( negative) phase, the SAF flows northeastward ( southeastward) with the fresh AAIW downwelling ( upwelling). Such mesoscale processes greatly enhance cross-frontal exchanges of water masses. Spectral analysis shows that frontal waves in the Southern Ocean south of Australia are dominated by a period of about 130 days with a phase speed of 4 cm/s and a wavelength of 450 km. |
format |
Article in Journal/Newspaper |
author |
Zhang LinLin Yan XiaoMei Sun Che Hu DunXin |
author_facet |
Zhang LinLin Yan XiaoMei Sun Che Hu DunXin |
author_sort |
Zhang LinLin |
title |
Variability of Antarctic Intermediate Water south of Australia and its relationship with frontal waves |
title_short |
Variability of Antarctic Intermediate Water south of Australia and its relationship with frontal waves |
title_full |
Variability of Antarctic Intermediate Water south of Australia and its relationship with frontal waves |
title_fullStr |
Variability of Antarctic Intermediate Water south of Australia and its relationship with frontal waves |
title_full_unstemmed |
Variability of Antarctic Intermediate Water south of Australia and its relationship with frontal waves |
title_sort |
variability of antarctic intermediate water south of australia and its relationship with frontal waves |
publishDate |
2016 |
url |
http://ir.qdio.ac.cn/handle/337002/135875 https://doi.org/10.1007/s11430-015-0179-5 |
geographic |
Antarctic Southern Ocean The Antarctic |
geographic_facet |
Antarctic Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Southern Ocean |
genre_facet |
Antarc* Antarctic Southern Ocean |
op_relation |
SCIENCE CHINA-EARTH SCIENCES Zhang LinLin,Yan XiaoMei,Sun Che,et al. Variability of Antarctic Intermediate Water south of Australia and its relationship with frontal waves[J]. SCIENCE CHINA-EARTH SCIENCES,2016,59(8):1674-1682. http://ir.qdio.ac.cn/handle/337002/135875 doi:10.1007/s11430-015-0179-5 |
op_doi |
https://doi.org/10.1007/s11430-015-0179-5 |
container_title |
Science China Earth Sciences |
container_volume |
59 |
container_issue |
8 |
container_start_page |
1674 |
op_container_end_page |
1682 |
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1766137559185883136 |