印尼贯穿流源区马鲁古海和哈马黑拉海水团来源的气候态分析

王露; 谢玲玲; 周磊; 李强; 石雨鑫; 李明明

doi:10.3969/j.issn.0253-4193.2018.03.001

印尼贯穿流源区马鲁古海和哈马黑拉海水团来源的气候态分析

doi: 10.3969/j.issn.0253-4193.2018.03.001

1.
广东省近海海洋变化与灾害预警重点实验室, 广东湛江 524088;广东海洋大学海洋与气象学院, 广东湛江 524088
2.
上海交通大学海洋研究院, 上海 200240;青岛海洋科学与技术国家实验室区域海洋动力学与数值模拟功能实验室, 山东青岛 266003;国家海洋局第二海洋研究所卫星海洋环境动力学国家重点实验室, 浙江杭州 310012

基金项目: “全球变化与海气相互作用”专项资助（GASI-IPOVAI-01-02，GASI-02-SCS-YGST2-02）；国家自然科学基金项目（41476009）。

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出版历程
- 收稿日期: 2017-03-10

Climatological analysis of water mass sources of Indonesia Throughflow in the Molukka Sea and Halmahera Sea

1.
Guangdong Key Laboratory of Coastal Ocean Variation and Disaster Prediction, Zhanjiang 524088, China;College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China
2.
Marine Research Institute of Shanghai Jiaotong University, Shanghai 200240, China;Regional Marine Dynamics and Numerical Simulation Functional Laboratory, Qingdao National Laboratory for Ocean Science and Technology, Qingdao 266003, China;State Key Laboratory of Marine Environmental Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China

摘要

摘要: 本文利用World Ocean Atlas 2013（WOA2013）气候态的温盐资料和the Simple Ocean Data Assimilation （SODA v3.3.1）流场数据，分析印尼贯穿流东部源区马鲁古海和哈马黑拉海的水团垂向分布特征及其来源，特别是次表层、中层及深层水的来源和路径。结果表明，气候态下，马鲁古海次表层的高温高盐水来自于北太平洋，与北太平洋热带水性质接近，哈马黑拉海次表层主要是来自南太平洋热带水；中层水以低温低盐为特征，马鲁古海的中层水来自南太平洋，受南极中层水控制，哈马黑拉海的中层水可能是从马鲁古海而来的南太平洋水；对于次表层和中层之间的过渡层，马鲁古海与哈马黑拉海的水源为南、北太平洋的混合水，且两个海域之间也存在着水团交换；在深层，马鲁古海的水源更倾向于班达海北部及塞兰海，而与太平洋水无关，哈马黑拉海由于地形阻挡也难以与太平洋直接发生水团交换。
- 印尼贯穿流 /
- 水团来源 /
- 哈马黑拉海 /
- 马鲁古海 /
- 垂向变化
Abstract: Using the climatology data of temperature and salinity from the World Ocean Atlas 2013 (WOA2013) and the ocean current data of the Simple Ocean Data Assimilation version 3.3.1 (SODA v3.3.1), the vertical distribution and water mass sources of the Indonesian Throughflow (ITF) in its east pathway are analyzed, especially the sub-surface, intermediate and deep waters in the Molukka Sea and Halmahera Sea. The results show that the warmer and saltier subsurface waters around 24.5σ_θ(about 150 m) in the Molukka Sea come from the North Pacific (NP), with characteristics close to those of the NP Tropic Water (NPTW), while the subsurface water in the Halmahera Sea is closely related to the South Pacific Tropical Water (SPTW). For the intermediate water around 26.8σ_θ (about 480 m), which is characterized by low temperature and low salinity, the South Pacific (SP) water intrudes into the Molukka Sea, and further enters the Halmahera Sea from the southwest straits. In the transition layer between the subsurface and intermediate waters, the waters in the Molukka Sea and Halmahera Sea are mixed waters from the NP and the SP. There is water exchange between the two seas. In the deep layer around 27.2σ_θ (about 850 m), the water in the Molukka Sea is inclined to being from the northern Banda Sea and the Selan Sea. The deep water in the Halmahera Sea is isolated without direct exchange with the Pacific water due to topographic barrier.
- Indonesian Throughflow /
- watermass sources /
- Halmahera Sea /
- Molukka Sea /
- vertical variability

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参考文献(39)

杜岩,方国洪.印度尼西亚海与印度尼西亚贯穿流研究概述[J].地球科学进展, 2011, 26(11):1131-1142. Du Yan, Fang Guohong. Progress on the study of the Indonesian Seas and Indonesian Throughflow[J]. Advances in Earth Science, 2011, 26(11):1131-1142.

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[J].海洋学报, 2008, 30(3):1-8. Zhang Yanhui, Yu Xiaolin, Wang Fan. Origins and pathways of the subsurface and intermediate waters of Indonesian throughflow derived from historical and Argo data[J].Haiyang Xuebao, 2008, 30(3):1-8.

刘钦燕,王东晓,谢强,等.印尼贯穿流与南海贯穿流的年代际变化特征及机制[J].热带海洋学报, 2007, 26(2):1-6. Liu Qinyan, Wang Dongxiao, Xie Qiang, et al. Decadel variability of Indonesian throughflow and South China Sea throughflow and its mechanism[J]. Journal of Tropical Oceanography, 2007, 26(2):1-6.

Zhou L, Murtugudde R, Jochum M, et al. Seasonal influence of Indonesian Throughflow in the southwestern Indian Ocean[J]. Journal of Physical Oceanography, 2008, 38(7):1529-1541.

Wajsowicz R C. Flow of a western boundary current through multiple straits:An electrical circuit analogy for the Indonesian throughflow and archipelago[J]. Journal of Geophysical Research, 1996, 101(C5):12295-12300.

Susanto R D, Gordon A L. Velocity and transport of the Makassar Strait throughflow[J]. Journal of Geophysical Research, 2005, 110(C1):287-294.

Gordon A L, Sprintall J, Van Aken H, et al. The Indonesian throughflow during 2004-2006 as observed by the INSTANT program[J]. Dynamics of Atmospheres and Oceans, 2010, 50(2):115-128.

Susanto R D, Ffield A, Gordon A L, et al. Variability of Indonesian throughflow within Makassar Strait, 2004-2009[J]. Journal of Geophysical Research, 2012, 117(C9):26-33.

Qu T, Du Y, Meyers G, et al. Connecting the tropical Pacific with Indian Ocean through South China Sea[J]. Geophysical Research Letters, 2005, 32(24):348-362.

Qu T, Du Y, Sasaki H, et al. South China Sea throughflow:A heat and freshwater conveyor[J]. Geophysical Research Letters, 2006, 332(23):430-452.

Tozuka T, Qu T, Masumoto Y, et al. Impacts of the South China Sea Throughflow on seasonal and interannual variations of the Indonesian Throughflow[J]. Dynamics of Atmospheres and Oceans, 2009, 47(1):73-85.

Fang G, Susanto R D, Wirasantosa S, et al. Volume, heat, and freshwater transports from the South China Sea to Indonesian seas in the boreal winter of 2007-2008[J]. Journal of Geophysical Research, 2010, 115(C12):93-102.

Susanto R D, Fang G, Soesilo I, et al. New surveys of a branch of the Indonesian Throughflow[J]. Eos, Transactions American Geophysical Union, 2010, 91(30):261-263.

Susanto R D, Wei Z, Adi R T, et al. Observations of the Karimata Strait througflow from December 2007 to November 2008[J]. Acta Oceanologica Sinica, 2013, 32(5):1-6.

Luick J L, Cresswell G R. Current measurements in the Molukka Sea[J]. Journal of Geophysical Research, 2001,106(C7):13953-13958.

Talley L D, Sprintall J. Deep expression of the Indonesian Throughflow:Indonesian Intermediate Water in the South Equatorial Current[J]. Journal of Geophysical Research, 2005, 110(C10):205-213.

Van Aken H M, Brodjonegoro I S, Jaya I, et al. The deep-water motion through the Lifamatola Passage and its contribution to the Indonesian throughflow[J]. Deep-Sea Research Part Ⅰ:Oceanographic Research Papers, 2009, 56(8):1203-1216.

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.

Lukas R, Firing E, Hacker P, et al. Observations of the Mindanao Current during the western equatorial Pacific Ocean circulation study[J]. Journal of Geophysical Research, 1991, 96(4):7089-7104.

Miyama T, Awaji T, Akitomo K, et al. Study of seasonal transport variations in the Indonesian seas[J]. Journal of Geophysical Research, 1995, 100(C10):20517-20541.

Gordon A L, Susanto R D, Vranes K. Cool Indonesian throughflow as a consequence of restricted surface layer flow[J]. Nature, 2003, 425(6960):824-828.

Zhou L, Murtugudde R. Influence of the Makassar Strait throughflow and winds over the southeastern Indian Ocean on the southwestern Indian Ocean SST variability[J]. Advances in Geosciences, 2009, 9(6):71-86.

Qu T, Mitsudera H, Yamagata T, et al. A climatology of the circulation and water mass distribution near the Philippine coast[J]. Journal of Physical Oceanography, 1999, 29(7):1488-1505.

Xie L L, Tian J W, Hu D X, et al. A quasi-synoptic interpretation of water mass distribution and circulation in the western North Pacific:Ⅰ. Water mass distribution[J]. Chinese Journal of Oceanology and Limnology, 2009, 27(3):630-639.

谢玲玲.西北太平洋环流及其与南海水交换研究[D]. 青岛:中国海洋大学,2009. Xie Lingling. Study on the circulation in western North Pacific and the water exchange between the Pacific and the South China Sea[D]. Qingdao:Ocean University of China, 2009.

谢骏.南海水团分析[D]. 青岛:中国海洋大学,2004. Xie Jun. The analysis of the South China Sea Water Masses[D]. Qingdao:Ocean University of China, 2004.

Fine R A, Lukas R, Bingham F M, et al. The western equatorial Pacific:A water mass crossroads[J]. Journal of Geophysical Research, 1994, 99(C12):25063-25080.

You Y, Suginohara N, Fukasawa M, et al. Roles of the Okhotsk Sea and Gulf of Alaska in forming the North Pacific Intermediate Water[J]. Journal of Geophysical Research, 2000, 105(C2):3253-3280.

You Y. Implications of cabbeling on the formation and transformation mechanism of North Pacific Intermediate Water[J]. Journal of Geophysical Research, 2003, 108(C5):31-34.

Wyrtki K. NAGA Report Volume 2:Scientific results of marine investigations of the South China Sea and the Gulf of Thailand 1959-1961[R]. Technical Report, Scripps Institute of Oceanography, 1961:195.

Nitani H. Beginning of the Kuroshio[M]//Kuroshio, Its Physical Aspects. Tokyo:University of Tokyo Press, 1972:129-163.

Talley L D. Some aspects of ocean heat transport by the shallow, intermediate and deep overturning circulation[M]//Mechanism of Global Climate Change at Millenial Time Scales. Washington DC:American Geophysical Union Geophysical Monograph, 1999, 112:1-22.

杨阳, 周伟东, 董丹鹏. 印尼贯穿流的诊断计算[J]. 热带海洋学报, 2007, 26(2):1-7. Yang Yang, Zhou Weidong, Dong Danpeng. Diagnostic calculation of Indonesian Throughflow[J]. Journal of Tropical Oceanography, 2007, 26(2):1-7.

李丽娟,刘秦玉,刘伟.太平洋北赤道流表层流速及分叉点位置[J]. 中国海洋大学学报, 2005, 35(3):370-374. Li Lijuan, Liu Qinyu, Liu Wei. Surface current speed and bifurcation of the North Equatorial Current in the Pacific Ocean[J]. Periodical of Ocean University of China, 2005, 35(3):370-374.

Du Yan, Qu Tangdong. Three inflow pathways of the Indonesian throughflow as seen from the simple ocean data assimilation[J]. Dynamics of Atmospheres and Oceans, 2010, 50(2):233-256.

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

Qu T D, Girton J B, Whitehead J A, et al. Deepwater overflow through Luzon Strait[J]. Journal of Geophysical Research, 2006, 111(C1):311-330.

Schiller A, Godfrey J S, Mcintosh P C, et al. Seasonal near-surface dynamics and thermodynamics of the Indian Ocean and Indonesian Throughflow in a global Ocean general circulation Model[J]. Journal of Physical Oceanography, 1998, 28(11):2288-2312.

Liu Qinyan, Feng Ming, Wang Dongxiao, et al. Interannual variability of the Indonesian Throughflow transport:A revisit based on 30 year expendable bathythermograph data[J]. Journal of Geophysical Research, 2015, 120(12):8270-8282.

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