基于历史资料和Argo资料的印尼贯通流次表层和中层水起源与路径探讨

张艳慧; 于晓林; 王凡

基于历史资料和Argo资料的印尼贯通流次表层和中层水起源与路径探讨

1.
中国科学院海洋研究所海洋环流与波动重点实验室, 山东青岛 266071;中国科学院研究生院, 北京 100049
2.
中国科学院海洋研究所海洋环流与波动重点实验室, 山东青岛 266071

基金项目: 国家基础研究重点规划项目课题(2006CB403601);国家自然科学基金项目(40576016)

计量
- 文章访问数: 838
- HTML全文浏览量: 11
- PDF下载量: 1178
- 被引次数: 0
出版历程
- 收稿日期: 2007-06-05
- 修回日期: 2007-10-21

Origins and pathways of the subsurface and intermediate waters of Indonesian throughflow derived from historical and Argo data

1.
Key Laboratory of Ocean Circulation and Waves, Institute of Oceanography, Chinese Academy of Science, Qingdao 266071, China;Graduate University of Chinese Academy of Science, Beijing 100049, China
2.
Key Laboratory of Ocean Circulation and Waves, Institute of Oceanography, Chinese Academy of Science, Qingdao 266071, China

摘要

摘要: 利用Argo资料和《世界海洋数据集2001版》(WOD01)温盐历史资料,通过对代表性等位势面上盐度分布的分析,探讨了次表层和中层等不同层次上印尼贯通流(ITF)的起源与路径问题.分析结果表明,ITF的次表层水源主要来自北太平洋,中层水源地既包括北太平洋、南太平洋,同时也不能排除有印度洋的可能性.在印度尼西亚海域西部,ITF的次表层和中层水源分别为北太平洋热带水(NPTW)和中层水(NPIW),经苏拉威西海、望加锡海峡到达弗洛勒斯海,层次越深特征越明显.在印度尼西亚海域东部,发现哈马黑拉-新几内亚水道附近存在次表层强盐度锋面,阻隔了南太平洋热带水(SPTW)由此进入ITF海域;中层水具有高于NPIW和来自南太平洋的南极中层水(AAIW)的盐度值,既可能是AAIW和SPTW在当地发生剧烈垂直混合而形成,也可能是来自印度洋的AAIW向北延伸进入ITF的结果.
- 印度尼西亚贯通流 /
- 次表层水 /
- 中层水 /
- 起源 /
- 路径
Abstract: Based on Argo data and historic temperature/salinity data from the World Ocean Database 2001 (WOD01),origins and spreading pathways of the subsurface and interm ediate water masses in the Indonesian Throughflow(ITF) region were discussed by analyzing distributions of salinity on representative isopycnal layers.Results were shown that,subsurface water mostly comes from the North Pacific while the intermediate water originates from both the North and South Pacific Ocean,even possibly from the Indian Ocean.Spreading through Sulawesi Sea,Makassar Strait,reach Flores Sea,the North Pacific Subsur face Water and North Pacific Intermediate Water dominate the western part of the Indonesian Archipelago.Furthermore as the depth increases,the features of the North Pacific sourced water masses become more obvious.In the eastern part of the waters,high salinity South Pacific Subsurface Water is blocked by a strong salinity front between Halmahera and New Guinea.Int er mediate watert here owns salinity higher than North Pacific Intermediate Water and Antarctica Intermediate Water(AAIW),possibly coming from thevertical mixing between subsurface water and the AAIW from the South Pacific,and possibly coming from the northward extending of the AAIW in the Indian Ocean as well.
- Indonesian Throughflow /
- subsurface water /
- inter mediate water /
- origin /
- pathway

HTML全文

参考文献(21)

HIRST A C,GODFREY J S.The role of Indonesian throughflow in a global ocean gem[J].Journal of Physical Oceanography,1993,23(6):1057-1086.

LEE T,FUKUMORI L,MENEMENLIS D,et al.Effects of the Indonesian throughflow on the Pacific and Indian oceans[J].Journal of Physical Oceanography,2002,32(5):1404-1429.

MURTUGUDDC R,BUSALACCHI A J.Interannual variability of the dynamics and thermodynamics of the tropical Indian Ocean[J].Journal of Climate,1999,12(8):2300-2326.

MURTUGUDDE R,BUSALACCHI A J,BEAUCHAMP J.Seasonal-to-interannual effects of the Indonesian throughflow on the tropical Indo——Pacific Basin.Journal of Geophysical Research——Oceans,1998,103(C10):21425-21441.

VRANES K,GORDON A L,FFIELD A.The heat transport of the Indonesian throughflow and implications for the Indian Ocean heat budget[J].Deep-Sea Research Part Ⅱ -Topical Studies in Oceanography,2002,49(7/8):1391-1410.

WAJSOWJCZ R C,SCHNEIDER E K.The Indonesian throughflow's effect on global climate determined from the COLA coupled climate system[J].Journal of Climate,2001,14(13):3029-3042.

WAJSOWICZ R C.Air-sea interaction over the Indian Ocean due to variations in the Indonesian throughflow[J].Climate Dynamics,2002,18(5):437-453.

WEBSTER P J,MAGANA V O,PALMERTN,et al.Monsoons:processes,predictability,and the prospects for prediction[J].Journal of Geophysical Research-Oceans,1998,103(C7):14451-14510.

GODFREY J S.The effect of the Indonesian throughflow on ocean circulation and heat exchange with the atmosphere..A review[J].Journal of Geophysical Research——Oceans,1996,101(C5):12217-12237.

FFIELD A,GORDON A L.Tidal mixing signatures in the Indonesian Seas[J].Journal of Physical Oceanography,1996,26(9):1924-1937.

HAUTALA S L,REID J L,BRAY N.The distribution and mixing of Pacific water masses in the Indonesian Seas[J].Journal of Geophysical Research——Oceans,1996,101(C5):12375-12389.

GORDON A L,SUSANTO R D.Banda Sea surface-layer divergence[J].Ocean Dynamics,2001,52:2-10.

GORDON A L,GIULIVI C E,HAHUDE A G.Deep topographic barriers within the Indonesian Seas[J].Deep-Sea Research Part Ⅱ ——Topical Studies in Oceanography,2003,50(12/13):2205-2228.

GORDON A L.When is appearance reality——A comment on why does the Indonesian throughflow appear to originate from the North Pacific[J].Journal of Physical Oceanography,1995,25(6):1660-1567.

GODFREY J S,HIRST A C,WILKIN J.Why does the Indonesian throughflow appear to originate from the North Pacific[J].Journal of Physical Oceanography,1993,23(6):1087-1098.

Van RIEHL P M.The Bottom Configuration in Relation to the Flow of Bottom Water[R]//BRILL E J.Snellius Expedition 1929-1930,Vol.2,Part 2,Chap 2.Leiden,Netherlands,1934:1-63.

GORDON A L,FINE R A.Pathways of water between the Pacific and Indian Oceans in the Indonesian Seas[J].Nature,1996,379(6561):146-149.

ILAHUDE A G,GORDON A L.Thermocline stratification within the Indonesian Seas[J].Journal of Geophysical Research——Oceans,1996,101(C5):12401-12409.

GORDON A L,SUSANTORD,VRANES K.Cool Indonesian throughflow as a consequence of restricted surface layer flow[J].Nature,2003,425(6960):824-828.

FFIELD A,GORDON A L.Vertical mixing in the Indonesian thermocline[J].Journal of Physical Oceanography,1992,22(2):184-195.

WYRTKI K,KILONSKY B.Mean water and current structure during the Hawaii-to-Tahiti Shuttle Experiment[J].Journal of Physical Oceanography,1984,14:242-254.

施引文献

资源附件(0)

访问统计