Progress on the Study of the Indonesian Seas and Indonesian Throughflow
Received date: 2011-05-06
Revised date: 2011-09-21
Online published: 2011-11-10
This paper reviews the relevant ocean dynamics study of the Indonesian Seas and Indonesian Throughflow in the last 30 years. Centred at the heart of Maritime Contininent, the Indonesian Seas connect the Western Pacific Warm Pool and Indian Ocean Warm Pool, having a direct impact on the large scale atmospheric circulations. The Indonesian Throughflow (ITF), weaving through the mutli-straits and passages in the Indonesian Seas, balances the thermal and saline distribution of the world ocean. In a long time scale, ITF has an influence on the structure of general circulation and climate change. Based on the advance of the in situ observation by international cooperation, the global scientific community has a significant advance in the regional oceanography of the Indonesian Seas and ITF. Those studies include two aspects. In the study of the regional oceanography of the Indonesian Seas, this paper reviews the major advance in ocean circulation, wave dynamics, tide and mixing, ocean vertical stratifications and air-sea interactions. In the study of the ITF, which is the only ocean connection of the global conveyer belt in the tropics, this paper review the advance in the ITF pathway, vertical structure, multiscale variations, water mass origin and their influence, heat and saline transport, ITF relationship with the Pacific circulations and Indian Ocean circulations, and its impact on the large scale ocean-atmosphere interactions, etc. This paper categorizes and discusses the relevant study and proposes prospects.
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 . DOI: 10.11867/j.issn.1001-8166.2011.11.1131
[1]Gordon A L. Oceanography of the Indonesian Seas and their throughflow[J]. Oceanography, 2005, 18(4):14-27.
[2]Broecker W. The great ocean conveyor[J]. Oceanography,1991,4: 79-89.
[3]Gordon A. Interocean exchange of thermocline water[J]. Journal of Geophysical Research, 1986, 91(4): 5 037-5 046.
[4]Yu Yongqiang, Zhou Zuyi, Zhang Xuehong. Impact of the closure of Indonesian seaway on climate: A numerical modeling study[J]. Chinese Science Bulletin, 2003,48(Suppl.II):88-93.[俞永强, 周祖翼, 张学洪.印度尼西亚海道关闭对气候的影响：一个数值模拟研究[J].科学通报, 2003,48(增刊2)：60-64.]
[5]Wu Haiyan, Li Chongyin, Zhang Ming. The preliminary numerical research of effects of ITF on tropical Pacific-Indian Ocean associated temperature anomaly node[J]. Journal of Tropical Meteorology, 2010, doi: 10.3969/j.issn.1004-4965.2010.05.001.[吴海燕，李崇银，张铭.印尼贯穿流对热带太平洋—印度洋海温异常综合模影响的初步模拟研究[J].热带气象学报，2010，26（5）: 513-520.]
[6]Gordon A L, Susanto R D, Vranes K. Cool Indonesian Throughflow as a consequence of restricted surface layer flow[J]. Nature,2003, 425(6 960): 824-828.
[7]Gordon A L, Sprintall J, Van Aken H M, et al.The Indonesian Throughflow during 2004-2006 as observed by the INSTANT program[J]. Dynamics of Atmospheres and Oceans, 2010, doi:10.1016/j.dynatmoce.2009.12.002.
[8]Wang Fan, Hu Dunxin. Introduction to international NPOCE program[J]. Chinese Journal of Oceanology and Limnology, 2010,28(4):953-953.
[9]McPhaden M J, Meyers G, Ando K, et al. RAMA: The research moored array for African-Asian-Australian monsoon analysis and prediction[J]. Bulletin of the American Meteorological Society,2009,90:459-480.
[10]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.
[11]Godfrey J S, Golding T J. The Sverdrup relation in the Indian Ocean and the effect of Pacific-Indian Ocean Throughflow on Indian Ocean circulation and on the East Australian Current[J].Journal of Physical Oceanography,1981, 11: 771-779.
[12]Piola A R, Gordon A L. Pacific and Indian Ocean upper layer salinity budget[J].Journal of Physical Oceanography,1984, 14(4):747-753.
[13]Fine R. Direct evidence using tritium data for Throughflow from the Pacific into the Indian-Ocean[J].Nature,1986, 315(6 019): 478-480.
[14]Wyrtki K. Indonesian Throughflow and the associated pressure gradient[J]. Journal of Geophysical Research,1987, 92(C12): 12 941-12 946.
[15]Murray S P, Arief D. Throughflow into the Indian Ocean through the Lombok Strait, January 1985-January 1986[J].Nature,1988, 333: 444-447.
[16]Meyers G, Bailey R J, Worby A P. Geostrophic transport of Indonesian Throughflow[J].Deep-Sea Research, 1995, 42(7): 1 163-1 174.
[17]Fieux M, Andrie C, Delecluse P, et al. Measurements within the Pacific-Indian oceans throughflow region[J].Deep Sea Research Part I: Oceanographic Research Papers,1994, 41(7): 1 091-1 130.
[18]Quadfasel D, Frische A, Cresswell G. The circulation in the source area of the South Equatorial Current in the eastern Indian Ocean[J].Journal of Geophysical Research, 1996, 101(C5): 12 483-12 488.
[19]Gordon A L, Fine R A. Pathways of water between the Pacific and Indian oceans in the Indonesian Seas[J].Nature, 1996, 379: 146-149.
[20]Wajsowicz R C, Gordon A L, Ffield A, et al. Estimating transport in Makassar Strait[C]∥Schott ed. Physical Oceanography of the Indian Ocean during the WOCE period, Deep-Sea Research II, 2003, 50: 2 163-2 181.
[21]Van Aken H M, Punjana J, Saimima S. Physical aspects of the flushing of the east Indonesian basins[J].Netherlands Journal of Sea Research,1988, 22: 15-339.
[22]Van Aken H M, Brodjonegoro I S, Jaya I. The deep water motion through the Lifamatola passage and its contribution to the Indonesian Throughflow[J].Deep Sea Research PartI:Oceanographic Research Papers, 2009, 56(8): 1 203-1 216, doi:10.1016/j.dsr.2009.02.001.
[23]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, C10009, doi:10.1029/2004JC002826.
[24]Fang G, Susanto R D, Wirasantosa S, et al. 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, C12020, doi:10.1029/2010JC006225.
[25]Metzger E J, Hurlburt H E, Xu X, et al. Simulated and observed circulation in the Indonesian Seas: 1/12°global HYCOM and the INSTANT observations[J].Dynamics of Atmosphere and Oceans, 2010, 50: 275-300.
[26]Arief D, Murray S P. Low-frequency fluctuations in the Indonesian Throughflow through Lombok Strait[J].Journal of Geophysical Research,1996, 101(C5):12 455-12 464.
[27]Molcard R, Fieux M, Ilahude A G. The Indo-Pacific Throughflow in the Timor passage[J].Journal of Geophysical Research, 1996, 101:12 411-12 420.[28]Molcard R, Fieux M, Syamsudin F. The throughflow within Ombai Strait[J].Deep Sea Research Part I: Oceanographic Research Papers,2001, 148: 1 237-1 253.
[29]Sprintall J, Wijffels S E, Molcard R, et al. Direct estimates of the Indonesian Throughflow entering the Indian Ocean: 2004-2006[J].Journal of Geophysical Research,2009, 114: C07001.
[30]Wijffels S E, Meyers G, Godfrey J S. A twenty year average of the Indonesian Throughflow: Regional currents and the interbasin exchange[J]. Journal of Physical Oceanography, 2008, doi: 10.1175/JPO2008/3987.1.
[31]Meyers G. Variation of Indonesian Throughflow and El Nio-Southern Oscillation[J].Journal of Geophysical Research,1996, 101: 12 255-12 263.
[32]England M H, Huang F. On the interannual variability of the Indonesian Throughflow and its linkage with ENSO[J]. Journal of Climate, 2005, 18: 1 435-1 444.
[33]Li Wei, Liu Hailong, Zhang Xuehong.Indonesian Throughflow in an eddy-permitting oceanic GCM[J].Chinese Science Bulletin, 2004, doi:1001-6538.0.2004-21-00D. [李薇, 刘海龙, 张学洪,等.一个涡相容的海洋环流模式模拟的印度尼西亚贯穿流[J].科学通报, 2004, 49: 2 001-2 006.]
[34]Li Zhiqiang,Yu Yongqiang,Wang Qianqian,et al. Simulation of the Indonesian Throughflow with a coupled ocean—Atmosphere Model[J]. Chinese Journal of Atmospheric Sciences,2005, 29:697-708.[李志强，俞永强，王谦谦，等.利用海气耦合模式模拟印度尼西亚贯穿流[J].大气科学，2005，29: 697-708.]
[35]Meng X F, Wu D X, Hu R J, et al. The interdecadal variation of Indonesian Throughflow and its mechanism[J].Chinese Science Bulletin,2004, 19: 2 058-2 067.
[36]Bray N A, Wijffels S E, Chong J C, et al. Characteristics of the Indo-Pacific Throughflow in the eastern Indian Ocean[J].Geophysical Research Letters, 1997, 24: 2 569-2 572.
[37]Schiller A,Wijffels S E, Sprintall J, et al. Pathways of intraseasonal variability in the Indonesian Throughflow region[J]. Dynamics of Atmospheres and Oceans,2010, doi:10.1016/j.dynatmoce.2010.02.003.
[38]Zhou L, Murtugudde R. Influences of Madden-Julian Oscillations on the eastern Indian Ocean and the maritime continent[J]. Dynamics of Atmospheres and Oceans, 2010, doi:10.1016/j.dynatmoce.2009.12.003.
[39]Ffield A, Gordon A L. Vertical mixing in the Indonesian thermocline[J]. Journal of Physical Oceanography, 1992, 22: 184-195.
[40]Godfrey J S, Hirst A C, Wilkin J L. Why does the Indonesian Throughflow appear to originate from the North Pacific?[J]. Journal of Physical Oceanography,1993, 23: 1 088-1 098.
[41]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: 1 560-1 567.
[42]Wajsowicz R C. The circulation of the depth-integrated flow around an island with application to the Indonesian Throughflow[J]. Journal of Physical Oceanography,1993, 23: 1 470-1 484.
[43]Wajsowicz R C.A simple model of the Indonesian Throughflow and its composition[J]. Journal of Physical Oceanography,1993, 2: 2 683-2 703.
[44]Wajsowicz R C. A relationship between Interannual variations in the South Pacific wind stress curl, the Indonesian Throughflow, and the western Pacific warm pool[J]. Journal of Physical Oceanography,1994, 24: 2 180-2 187.
[45]Nof D. Choked flows from the Pacific to the Indian Ocean[J]. Journal of Physical Oceanography,1995, 25: 1 369-1 383.
[46]Nof D. What controls the origin of the Indonesian Throughflow?[J]. Journal of Geophysical Research, 1996, 12 301-12 314, doi:10.1029/95JC03440.
[47]Gordon A L, Ffield A, Ilahude A G. Thermocline of the Flores and Banda Seas[J].Journal of Geophysical Research,1994,99:18 235-18 242.
[48]Ilahude A G, Gordon A L. Thermocline stratification within the Indonesian Seas[J].Journal of Geophysical Research, 1996, 101: 12 401-12 409.
[49]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,1996, 101: 12 375-12 389.
[50]Jean-Baptiste P, Fieux M, Ilahude A G. An eastern Indian Ocean 3He section from Australia to Bali: Evidence for a deep Pacific-Indian throughflow[J].Geophysical Research Letters, 1997, 24: 2 577-2 580.
[51]Wijffels S, Sprintall J, Fieux M, et al. The JADE and WOCE I10/IR6 Throughflow Sections in the Southeast Indian Ocean. Part 1: Water mass distribution and variability[J].Deep-Sea Research II,2002,49: 1 341-1 362.
[52]Murtugudde R, Busalacchi A J, Beauchamp J. Seasonal-to-interannual effects of the Indonesian Throughflow on the tropical Indo-Pacific Basin[J].Journal of Geophysical Research, 1998, 103: 21 425-21 441.
[53]Vranes K, Gordon A L, Ffield A. The heat transport of the Indonesian Throughflow and implications for the Indian Ocean Heat Budget[C]∥Schott F ed. Physical Oceanography of the Indian Ocean during the WOCE Period. Deep-Sea Research, 2002, 49(7/8):1 391-1 410.
[54]Hirst A C,Godfrey J S. The role of Indonesian Throughflow in a global ocean GCM[J].Journal of Physical Oceanography,1993, 3: 1 057-1 086.
[55]Wunsch C. Variability of the Indo-Pacific Ocean exchanges[J].Dynamics of Atmospheres and Oceans,2010, doi:10.1016/j.dynatmoce.2009.12.001.
[56]Hirst A C, Godfrey J S. The response to a sudden change in Indonesian Throughow in a global ocean GCM[J].Journal of Physical Oceanogrphy, 1994, 24: 1 895-1 910.
[57]Song Q, Gordon A L, Visbeck M. Spreading of the Indonesian Throughflow in the Indian Ocean[J].Journal of Physical Oceanogrphy,2004, 34: 772-792.[58]Susanto R D, Gorden A L. Velocity and transport of the Makassar Strait throughflow[J].Journal of Geophysical Research, 2005, 110, C01005, doi: 10.1029/2004JC002425.
[59]Wijffels S E, Schmitt R W, Bryden H L, et al. Transport of freshwater by the ocean[J].Journal of Physical Oceanogrphy,1992, 22: 155-162.
[60]Liu Xiangcui,Liu Hailong,Li Wei,et al. Geostrophic transport of the Indonesian Throughflow estimated by using the Argo data[J].Journal of Tropical Meteorology,2009,28(5):75-82.[刘祥翠，刘海龙，李薇，等.用Argo温盐资料估计印度尼西亚贯穿流多年平均地转输送[J].热带海洋学报，2009，28(5): 75-82.]
[61]Gordon A L, Ma S, Olson D B, et al. Advection and diffusion of Indonesian Throughflow water within the Indian Ocean South Equatorial Current[J]. Geophysical Research Letters, 1997, 24: 2 573-2 576.
[62]Clarke R A, Liu X. Observations and dynamics of semiannual and annual sea levels near the eastern equatorial Indian Ocean boundary[J].Journal of Physical Oceanography,1993, 23: 386-399.
[63]Clarke A J, Liu X. Interannual sea level in the northern and eastern Indian Ocean[J].Journal of Physical Oceanography,1994, 24: 1 224-1 235.
[64]Yamagata T, Mizuno K,Masumoto Y. Seasonal variations in the equatorial Indian Ocean and their impact on the Lombok throughflow[J].Journal of Geophysical Research,1996, 101: 12 465-12 473.
[65]Wijffels S, Meyers G. An intersection of oceanic waveguides: Variability in the Indonesian Throughflow region[J].Journal of Physical Oceanography,2004, 34: 1 232-1 253.
[66]Sprintall J, Wijffels S, Molcard R, et al. Direct evidence of the South Java Current system in Ombai Strait[J]. Dynamics of Atmospheres and Oceans,2010, doi:10.1016/j.dynatmoce.2010.02.006.
[67]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,1996,101:12 217-12 237.
[68]Wajsowicz R C, Schneider E K. The Indonesian Throughflow′s effect on global climate determined from the COLA coupled climate[J].Jourtnal Climate,2001,14:3 029-3 042.
[69]Yuan D, Liu H. Long wave dynamics of sea level variations during Indian Ocean dipole events[J].Journal of Physical Oceanography,2009,39:1 115-1 132.
[70]Yuan Dongliang, Wang Jing, Xu Tengfei, et al. Forcing of the Indian Ocean Dipole on the interannual variations of the tropical Pacific Ocean: Roles of the Indonesian Throughflow[J].Journal of Climate, 2011,24:3 593-3 607.
[71]Santoso A, Cai W, England M H, et al. The role of the Indonesian Throughflow on ENSO dynamics in a coupled climate model[J].Journal of Climate,2011,24:585-601.
[72]Cai W, Cowan T. La Nia Modoki impacts Australia autumn rainfall variability[J].Geophysical Research Letters,2009, 36, L12805, doi:10.1029/2009GL037885.
[73]Qiu B, Lukus R. Seasonal and interannual variability of the North Equatorial Current, the Mindanao Current and the Kuroshio along the Pacific western boundary[J].Journal of Geophysical Research,1996, 101: 12 315-12 330.
[74]Qu T, Mitsudera H, Yamagata T. Intrusion of the North Pacific waters into the South China Sea[J].Journal of Geophysical Research,2000, 105: 6 415-6 424.
[75]Metzger E J, Hurlburt H E. Coupled dynamics of the South China Sea, the Sulu Sea, and the Pacific Ocean[J].Journal of Geophysical Research,1996, 101: 12 331-12 352.
[76]Fang Guohong, Wei Zexun, Wang Kai, et al.Interbasin freshwater, heat and salt transport through the boundaries of the East and South China Seas from a variable-grid global ocean circulation model[J].Science in China (Series D),2003,doi: 10.1360/03yd9014.[方国洪，魏泽勋，王凯，等.中国近海域际水、热、盐输运：全球变网格模式结果[J].中国科学：D辑,2002,32(12) : 969-977.]
[77]Fang Guohong, Wei Zexun, Huang Qizhou,et al. Volume,heat and salt transports between the southern South China Sea and its adjacent waters,and their contribution to the Idionesian Throughflow[J].Oceanologia et Limnologia Sinica,2002, 33（3）:296-302[方国洪，魏泽勋，黄企洲，等.南海南部与外海间的体积和热、盐输运及其对印尼贯穿流的贡献[J].海洋与湖沼，2002，33（3）：296-302.]
[78]Qu T, Kim Y Y, Yaremchuk M,et al. Can Luzon Strait transport play a role in conveying the impact of ENSO to the South China Sea?[J]. Journal of Climate, 2004, 17: 3 643-3 656.
[79]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, L24609, doi:10.1029/2005GL024698.
[80]Qu T, Du Y, Sasaki H. South China Sea throughflow: A heat and freshwater conveyor[J].Geophysical Research Letters,2006, 33, L23617, doi:10.1029/2006GL028350.
[81]Wang D, Liu Q, Huang R X, et al. Interannual variability of the South China Sea throughflow inferred from wind data and an ocean data assimilation product[J].Geophysical Research Letters, 2006, 33, L14605, doi:10.1029/2006GL026316.
[82]Fang G H, Wang Y G, Wei Z X, et al. Interocean circulation and heat and freshwater budgets of the South China Sea based on a numerical model[J].Dynamics of Atmosphere and Oceans, 2009, 47: 55-72.
[83]Fang G, Susanto D, Soesilo I, et al. A note on the South China Sea shallow interocean circulation[J].Advances in Atmospheric Sciences, 2005, 22(6): 946-954.
[84]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 Atmosphere and Oceans,2009, 47: 73-85.
[85]Tozuka T, Qu T,Yamagata T. Dramatic impact of the South China Sea on the Indonesian Throughflow[J].Geophysical Research Letters, 2007, 34, L12612, doi:10.1029/2007GL030420.
[86]Lukas R, Yamagata T,McCreary J P. Pacific low-latitude western boundary currents and the Indonesian Throughflow[J].Journal of Geophysical Research,1996, 101(C5): 12 209-12 216.
[87]Kashino Y, Aoyama M, Kawano T, et al. The water masses between Mindanao and New Guinea[J].Journal of Geophysical Research,1996, 101(C5):12 391-12 400.
[88]Hatayama T, Awaji T, Akitomo K. Tidal currents in the Indonesian Seas and their effect on transport and mixing[J].Journal of Geophysical Research,1996, 101(C5):12 353-12 373.
[89]Sprintall J, Wijffels S, Chereskin T, et al. The JADE and WOCE I10/IR6 throughflow sections in the Southeast Indian Ocean. Part 2: Velocity and transports[J].Deep-sea Research II, 2002, 49: 1 363-1 389.
[90]Potemra J T, Hautala S L, Sprintall J. Vertical structure of the Indonesian Throughflow in a large-scale model[J].Deep Sea Research, 2003, 50: 2 143-2 161.
[91]Gordon A L, Giulivi C F, Ilahude A G. Deep topographic barriers within the Indonesian Seas[J].Deep-Sea Research II, 2003, 50: 2 205-2 228.
[92]Syamsudin F, Van Aken H M, Kaneko A. Annual variation of the southern boundary current in the Banda Sea[J].Dynamics of Atmosphere and Oceans,2010, doi:10.1016/j.dynatmoce.2009.12.005.
[93]Schiller A,Wijffels S E, Sprintall J, et al. Pathways of Intraseasonal variability in the Indonesian Throughflow region[J]. Dynamics of Atmospheres and Oceans, 2008, doi:10.1016/j.dynatmoce.2010.02.003.
[94]Tillinger D, Gordon A L. Transport weighted temperature and internal energy transport of the Indonesian Throughflow[J].Dynamics of Atmosphere and Ocean, 2010, doi:10.1016/j.dynatmoce.2010.01.002.
[95]Du Y, Qu T. Three inflow pathways of the Indonesian Throughflow as seen from the simple ocean data assimilation[J]. Dynamics of Atmospheres and Oceans,2010, doi:10.1016/j.dynatmoce.2010.04.001.
[96]Bernhard Mayer, Damm P E. Thomas Pohlmann, et al. What is driving the ITF? An illumination of the Indonesian Throughflow with a numerical nested model system[J].Dynamics of Atmospheres and Oceans,2010, doi:10.1016/j.dynatmoce.2010.03.002.
[97]Rosenfield D, Kamenkovich V,O’Driscoll K, et al. Validation of a regional Indonesian Seas model based on a comparison between model and INSTANT transports[J].Dynamics of Atmospheres and Oceans,2010, doi:10.1016/j.dynatmoce.2010.02.005.
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