The intermediate water in the Philippine Sea

The dimensional and temporal distribution of Antarctic Intermediate Water (AAIW) and North Pacific Intermediate Water (NPIW) in the Philippine Sea were explored using Argo profiles and gridded Argo data. As the salinity minimum of intermediate water from mid-high latitude of the southern and norther...

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Published in:Journal of Oceanology and Limnology
Main Authors: Zang Nan, Wang Fan, Sprintall, Janet
Format: Report
Language:English
Published: SCIENCE PRESS 2020
Subjects:
Online Access:http://ir.qdio.ac.cn/handle/337002/168528
http://ir.qdio.ac.cn/handle/337002/168529
https://doi.org/10.1007/s00343-020-0035-4
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spelling ftchinacasciocas:oai:ir.qdio.ac.cn:337002/168529 2023-05-15T13:50:09+02:00 The intermediate water in the Philippine Sea Zang Nan Wang Fan Sprintall, Janet 2020-05-19 http://ir.qdio.ac.cn/handle/337002/168528 http://ir.qdio.ac.cn/handle/337002/168529 https://doi.org/10.1007/s00343-020-0035-4 英语 eng SCIENCE PRESS JOURNAL OF OCEANOLOGY AND LIMNOLOGY http://ir.qdio.ac.cn/handle/337002/168528 http://ir.qdio.ac.cn/handle/337002/168529 doi:10.1007/s00343-020-0035-4 the intermediate water the Antarctic Intermediate Water the North Pacific Intermediate Water seasonal variation Marine & Freshwater Biology Oceanography Limnology 期刊论文 2020 ftchinacasciocas https://doi.org/10.1007/s00343-020-0035-4 2022-06-27T05:43:07Z The dimensional and temporal distribution of Antarctic Intermediate Water (AAIW) and North Pacific Intermediate Water (NPIW) in the Philippine Sea were explored using Argo profiles and gridded Argo data. As the salinity minimum of intermediate water from mid-high latitude of the southern and northern hemisphere of the Pacific Ocean, the properties of AAIW and NPIW merge at about 10 degrees N with different properties in the Philippine Sea. The core of AAIW is located below 600 dbar with potential density of 27 <=sigma(theta)<= 27.3 kg/m(3)and salinity of 34.5 <= S <= 34.55. The core of NPIW is located between 300-700 dbar with potential density of 26.2 <=sigma(theta)<= 27 kg/m(3)and salinity of 34 <= S <= 34.4. The volume of AAIW and NPIW during January 2004 to December 2017 is negatively correlated. The time series of AAIW and NPIW is dominated by significant periods of 6 and 8 months, respectively. The variations of AAIW and NPIW are mainly affected by volume transport through a 130 degrees E section by the North Equatorial Current (NEC) and North Equatorial Undercurrent (NEUC). Report Antarc* Antarctic Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Antarctic Pacific The Antarctic Journal of Oceanology and Limnology 38 5 1343 1353
institution Open Polar
collection Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR
op_collection_id ftchinacasciocas
language English
topic the intermediate water
the Antarctic Intermediate Water
the North Pacific Intermediate Water
seasonal variation
Marine & Freshwater Biology
Oceanography
Limnology
spellingShingle the intermediate water
the Antarctic Intermediate Water
the North Pacific Intermediate Water
seasonal variation
Marine & Freshwater Biology
Oceanography
Limnology
Zang Nan
Wang Fan
Sprintall, Janet
The intermediate water in the Philippine Sea
topic_facet the intermediate water
the Antarctic Intermediate Water
the North Pacific Intermediate Water
seasonal variation
Marine & Freshwater Biology
Oceanography
Limnology
description The dimensional and temporal distribution of Antarctic Intermediate Water (AAIW) and North Pacific Intermediate Water (NPIW) in the Philippine Sea were explored using Argo profiles and gridded Argo data. As the salinity minimum of intermediate water from mid-high latitude of the southern and northern hemisphere of the Pacific Ocean, the properties of AAIW and NPIW merge at about 10 degrees N with different properties in the Philippine Sea. The core of AAIW is located below 600 dbar with potential density of 27 <=sigma(theta)<= 27.3 kg/m(3)and salinity of 34.5 <= S <= 34.55. The core of NPIW is located between 300-700 dbar with potential density of 26.2 <=sigma(theta)<= 27 kg/m(3)and salinity of 34 <= S <= 34.4. The volume of AAIW and NPIW during January 2004 to December 2017 is negatively correlated. The time series of AAIW and NPIW is dominated by significant periods of 6 and 8 months, respectively. The variations of AAIW and NPIW are mainly affected by volume transport through a 130 degrees E section by the North Equatorial Current (NEC) and North Equatorial Undercurrent (NEUC).
format Report
author Zang Nan
Wang Fan
Sprintall, Janet
author_facet Zang Nan
Wang Fan
Sprintall, Janet
author_sort Zang Nan
title The intermediate water in the Philippine Sea
title_short The intermediate water in the Philippine Sea
title_full The intermediate water in the Philippine Sea
title_fullStr The intermediate water in the Philippine Sea
title_full_unstemmed The intermediate water in the Philippine Sea
title_sort intermediate water in the philippine sea
publisher SCIENCE PRESS
publishDate 2020
url http://ir.qdio.ac.cn/handle/337002/168528
http://ir.qdio.ac.cn/handle/337002/168529
https://doi.org/10.1007/s00343-020-0035-4
geographic Antarctic
Pacific
The Antarctic
geographic_facet Antarctic
Pacific
The Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation JOURNAL OF OCEANOLOGY AND LIMNOLOGY
http://ir.qdio.ac.cn/handle/337002/168528
http://ir.qdio.ac.cn/handle/337002/168529
doi:10.1007/s00343-020-0035-4
op_doi https://doi.org/10.1007/s00343-020-0035-4
container_title Journal of Oceanology and Limnology
container_volume 38
container_issue 5
container_start_page 1343
op_container_end_page 1353
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