Ganachaud A, Wunsch C. Improved estimates of global ocean circulation, heat transport and mixing from hydrographic data. Nature, 2000, 408: 453～457
[2]
Meyers G, Bailey R J, Worby A P. Geostrophic transport of Indonesian throughflow. Deep-Sea Res., Part I, 1995, 42: 1163～1174
[3]
Wijffels S E, Bray N A, Hautala S. The WOCE Indonesian throughflow repeat hydrography sections: I10 and IR6. International WOCE Newsletter, 1996, 24: 25～28
[4]
Wyrtki K. Indonesian throughflow and the assiociated pressure gradient. J. Geophys. Res., 1987, 92: 12941～12946
[5]
Murray S P, Arief D. Throughflow in the Indian Ocean through Lombok Strait (January 1985-January 1986). Nature, 1998, 333: 444～447
[6]
Schneider N, Barnett T. Indonesian throughflow in a coupled general circulation model. J. Geophys. Res., 1997, 102: 12341～12358
[7]
Clarke A J, Liu X. Interannual sea level in the Northern and Eastern Indian Ocean. J. Phys. Oceanogr., 1994, 24: 1224～1235
[8]
Fieux M, Molcard R, Ilahude A G. Geostrophic transport of the Pacific-Indian Oceans throughflow. J. Geophys. Res., 1996, 101: 12421～12432
[9]
Meyers G. Variation of Indonesian throughflow and the El Nio-Southern Oscillation. J. Geophys. Res., 1996, 101: 12255～12263
[10]
Gordon A L, Susanto J S. Makassar transport: Initial estimate based on Arlindo results. Mar. Tech. Soc., 1999, 32: 34～45
[11]
Gordon A L, Susanto J S, Kevin V. Cool Indonesian throughflow as a consequence of restricted surface layer flow. Nature, 2003, 425: 824～828
[12]
王东晓, 刘赟, 刘钦燕, 等. 1997～1998年厄尔尼诺期间印度洋和西太平洋上层海洋的联系. 自然科学进展, 2003, 13(9): 957～963Wang Dongxiao, Liu Yun, Liu Qinyan, et al. The relation between the top layer of Indian Ocean and the top layer of west Pacific Ocean during the 1997-1998 El Nio event. Progress in Natural Science (in Chinese), 2003, 13(9): 957～963
[13]
李薇, 刘海龙, 张学洪. 一个涡相容的海洋环流模式模拟的印度尼亚贯穿流, 科学通报, 2004, 49(19): 2001～2006Li Wei, Liu Hailong, Zhang Xuehong, et al. An ocean model of eddy consistent simulate the Indonesian throughflow. Chinese Science Bulletin (in Chinese), 2004, 49(19): 2001～2006
[14]
Inoue M, Welsh S E. Modeling seasonal variability in the wind driven upper-layer circulation in the Indo-Pacific region. J. Phys. Oceanogr., 1993, 23: 1411～1436
[15]
Godfrey J S . A Sverdrup model of the depth-integrated flow for the world ocean allowing for island circulations. Geophys. Astrophys. Fluid Dyn., 1989 , 45: 89～112
[16]
Clarke A J. On the reflection and transmission of low-frequency energy at the irregular western Pacific Ocean boundary. J. Geophys. Res., 1991, 96: 3289～3305
[17]
Du P Y, Cane M A. Effect of low-latitude western boundary gaps on the reflection of equatorial motions. J. Geophys. Res., 1991, 96: 3307～3322
[18]
Gregory C J, Bernadette M S. Direct mseasurements of upper ocean currents and water properties across the tropical Pacific during the 1990\'s. Progress in Oceanography, 2001, 52: 31～61
[19]
Wester P, Lukas R, Toga C. The coupled ocean atmosphere response experiment. Bull. Amer. Meteor. Soc., 1992, 73: 1377～1416
[20]
Gordon A L. Interocean exchange of thermocline water. J. Geophys. Res., 1986, 91(C4): 5037～5046
[21]
Godfrey J S. The effect of the Indonesian throughflow on ocean circulation and heat exchange with the atmosphere: A review. J. Geophys. Res., 1996, 101(C5): 12217～12237
[22]
Potemra J T, Lukas R. Large-scale estimation of transport from the Pacific to the Indian Ocean. J. Geophys. Res., 1997, 102: 27795～27812
[23]
Masumoto Y. Effects of interannual variability in the eastern Indian Ocean on the Indonesian throughflow. Symposium on the Ocean-Atmosphere Coupled Dynamics in the Indian Ocean, 17-18 December 2001, Tokyo, Prince Hotel, 69 [Frontier Research System for Global Change (FRSGC), International Pacific Research Center (IPRC)]
[24]
Yamagata T, Behera S K, Rao S A, et al. Interannual subsurface variability in the tropical Indian Ocean with a special emphasis on the Indian Ocean dipole. Deep-Sea Res. II, 2002, 49: 1549～1572
[25]
Schneider N . The Indonesian throughflow and the global climate system. J. Climate, 1998, 11: 676～689
[26]
Banks H T. Indonesian Throughflow in a coupled climate model and the sensitivity of the heat budget and deep overturning. J. Geophys. Res., 2000, 105 (C11): 26135～26150
[27]
Wajsowicz R C, Schneider E K. The Indonesian Throughflow\'s effect on global climate determined from the COLA coupled climate system. J. Climate, 2001, 14: 3029～3042
[28]
Yu Yongqiang, Yu Rucong, Zhang Xuehong, et al. A flexible global coupled climate model. Adv. Atmos. Sci., 2002, 19: 169～190
[29]
Yu Yongqiang, Zhang Xuehong, Guo Yufu. Global coupled ocean-atmosphere general circulation models in LASG/IAP. Adv. Atmos. Sci., 2004, 21: 444～455
[30]
刘海龙. 高分辨率海洋环流模式和热带太平洋上层环流的模拟研究. 中国科学院大气物理研究所博士学位论文, 2002Liu Hailong. A ocean circulation model of high resolution and simulated study of top circulation of the tropical Pacific ocean. Ph. D. dissertation (in Chinese), Institute of Atmospheric Physics, Chinese Academy of Sciences, 2002
[31]
Wijffels S E, Meyers G. Fifteen years of XBT measurements in the Indonesian Throughflow. Abstract IUGG General Assembly, Sapporo Japan, 2003
[32]
孟祥风, 吴德星, 胡瑞金, 等. 印度尼西亚贯穿流年代际变化及其分析. 科学通报, 2004, 49(15): 1550～1558Meng Xiangfeng,Wu Dexing, Hu Ruijin, et al. The analyse of the Indonesian throughflow decade change and its reason. Chinese Science Bulletin (in Chinese), 2004, 49(15): 1550～1558
