[1] RAMANATHAN V, COLLINS W. Thermodynamic regulation of ocean warming by cirrus clouds deduced from observations of the 1987 El Niño[J]. Nature, 1991, 351: 27–32.
[2] WALISER D E, GRAHAM N E. Convective cloud systems and warm-pool sea-surface temperatures—Coupled interactions and self-regulation[J]. J Geophys Res, 1993, 98D: 12881–12893.
[3] Fu R, DELGENIO A D, ROSSOW W B, et al. Cirrus cloud thermostat for tropical sea surface temperatures tested using satellite data[J]. Nature, 1992, 358: 394–397.
[4] DELGENIOA D, KOVARI W. Climatic properties of tropical precipitating convection under varying environmental conditions[J]. J Climate, 2002,15: 2597–2615.
[5] HARTMANN D L, MICHELSEN M L. Large-scale effects on the regulation of tropical sea surface temperature [J]. J Climate, 1993, 6: 2049–2062.
[6] ZHANG G J, RAMANATHAN V, MCPHADEN M J. Convection-evaporation feedback in the equatorial Pacific[J]. J Climate, 1995, 8: 3040–3051.
[7] PIERRHUMBERT R T. Thermostats, radiator fins, and the runaway greenhouse[J]. J Atmos Sci, 1995, 52: 1784–1806.
[8] LARSON K, HARTMANN D L, KLEIN S A. On the role of clouds, water vapor, circulation, and boundary layer structure on the sensitivity of the tropical climate[J]. J Climate, 1999, 12: 2359–2374.
[9] MILLER R L. Tropical thermostats and low cloud cover[J]. J Climate, 1997, 10: 409–440.
[10] SUN D-Z, LIU Z. Dynamic ocean–atmosphere coupling: A thermostat for the tropics[J]. Science, 1996, 272: 1148–1150.
[11] CLEMENT A C, SEAGER R, CANE M A, et al. An ocean dynamical thermostat[J]. J Climate, 1996, 9: 2190–2196.
[12] CLEMENT A C, SEAGER R. Climate and the tropical oceans[J]. J Climate, 1999, 12: 3384–3401.
[13] VINAYACHANDRAN P N, SHETYE S R. The warm pool in the Indian Ocean[J]. Proc Indian Acad Sci:Earth & Planetary Sci., 1991,100: 165-175.
[14] 周天军, 张学洪.印度洋海气热通量交换研究[J].大气科学, 2002, 26(2): 161-170.
[15] RAO R R, MOLINARI R L, FIESTA J F. Evolution of the climatological near-surface thermal structure of the tropical Indian Ocean: 1. Description of mean monthly mixed layer depth, and sea surface temperature, surface current, and surface meteorological fields[J]. Journal of Geophysical Research, 1989, 105: 985–1015.
[16] UNNIKRISHNANA S, KUMAR S P, NAVELKAR G S. Large-scale processes in the upper layers of the Indian Ocean inferred from temperature climatology[J]. J Mar Res, 1997, 55: 93-115.
[17] CLEMENT A C, SEAGER R, MURTUGUDDE R. Why are there tropical warm pools? [J] J Climate, 2005, 18: 5294-5311.
[18] 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[D]. 北京:中国科学院大气物理研究所, 2002.
[19] 刘海龙, 俞永强, 李薇, 等. LASG/IAP气候系统海洋模式(LICOM1.0)参考手册[R]//大气科学和地球流体力学数值模拟国家重点实验室(LASG)技术报告特刊. 北京: 科学出版社, 2004: 1-108.
[20] 张学洪, 俞永强, 宇如聪, 等. 一个大洋环流模式和相应的海气耦合模式的评估 I. 热带太平洋的年平均状态[J]. 大气科学, 1003, 27: 949-970.
[21] LIU HAILONG, ZHANG XUEHONG, LI WEI, et al. An eddy-permitting oceanic general circulation model and its preliminary evaluation[J]. Adv Atmos Sci, 2004, 21: 675-690.
[22] GENT P R, MCWILLIAMS J C. Isopycnal mixing in ocean circulation models[J]. J Phys Oecanogr, 1990, 20: 150-155.
[23] PACANOWSKIR C, PHILANDER G. Parameterization of vertical mixing in numerical models of the tropical ocean[J]. J Phys Oceanogr, 1981, 11: 1442-1451.
[24] FRANK R. An atlas of surface fluxes based on the ECMWF re-analysis—a climatological dataset to force global ocean general circulation models[R]//Report No. 323. Hamburg: Max-Planck- Institut für Meteorologie, 2001: 1-31.
[25] STEPHENS C, ANTONOV J I, BOYER T P, et al. World Ocean Atlas 2001, Volume 1: Temperature[C]//LEVITUS S. NOAA Atlas NESDIS 49, U.S. Government Printing Office, Wash, D C, 2002: 1-167. CD-ROMs.
[26] YU YONGQIANG, ZHNEG WEIPENG, WANG BIN, et al. The IAP Flexible Global Ocean-Atmosphere-Land System Model versions g1.0 and g1.1[J]. Adv Atmos Sci, 2010, doi: 10.1007/s00376-010-9112-5.
[27] YU YONGQINAG, SUN DE-ZHENG. Response of ENSO to subtropical cooling: A study using the IAP coupled model[J]. J Climate, 2009, 22: 5902-5917.
[28] YU YONGQIANG, ZHI HAI, WANG BIN, et al. Coupled model simulations of climate changes in the 20th century and beyond[J]. Adv Atmos Sci, 2008, 25: 641-654.
[29] 俞永强, 郑伟鹏, 刘海龙, 等. LASG耦合气候系统模式FGCM-1.0[J]. 地球物理学报, 2007, 50: 1677-1687.
[30] YU YONGQINAG, ZHANG XUEHONG, GUO YUFU. Global coupled ocean- atmosphere general circulation models in LASG/IAP[J]. Adv Atmos Sci, 2004, 21: 444-455.
[31] YU YONGQIANG, YU RUCONG, ZHANG XUEHONG, et al. A flexible global coupled climate model[J]. Adv Atmos Sci, 2002, 19: 169-190.
[32] GIBSON J K, KALLBERG P, UPPALA S, et al. ERA Description, ECMWF Reanalysis Project Report Series 1[R]. European Center for Medium Range Weather Forecast, Reading, UK. 1997: 1-66.
[33] JOSEY S A, KENT E C, TAYLOR P K. The Southampton Oceanography Centre (SOC) ocean-atmosphere heat, momentum and freshwater flux atlas[R]. Southampton Oceanography Centre Report No. 6, 1998: 1-25.
[34] HOFFMAN R N, LEIDNER S M. An introduction to the near-real time QuikSCAT data[J]. Wea Forecasting, 2005, 20: 476–493.
[35] KALNAY E, KANAMITSU M, KISTLER R, et al. The NCEP/NCAR 40-year reanalysis project[J]. Bull Amer Meteor Soc, 1996, 77: 437-471.
[36] YU L, WELLER R A, SUN B. Improving latent and sensible heat flux estimates for the Atlantic Ocean (1988-1999) by a synthesis approach[J]. J Clim, 2004, 17: 373-393.
[37] WU FANGHUA, LIU HAILONG, LI JIANGLONG, et al. Effect of adjusting vertical resolution on the eastern equatorial Pacific cold tongue[J]. Acta Oceanologica Sinica, 2005, 24(3): 1-12.
[38] LIU HAILONG, LIN WUYIN, ZHANG MINGHUA. Heat budget of the upper ocean in the south central Equatorial Pacific[J]. Journal of Climate, 2010, 23 (7): 1779-1792.
[39] 李超. 东半球暖池季节变化与上混合层热收支分析[D]. 广州:中国科学院南海海洋研究所, 2007.