热带海洋学报    2011 30 (1): 1-10   ISSN: 1009-5470  CN: 44-1500/P  

暖池季节变化的数值模拟及其对海表热力和动力强迫的敏感性
俞永强1, 李超1, 2, 王东晓2, 刘海龙1
1. 中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室, 北京 100029; 2. 中国科学院南海海洋研究所, 广东 广州 510301
收稿日期 2009-07-27  修回日期 2009-10-12  网络版发布日期 2011-03-16
参考文献  

[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 SciEarth & 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): 161170.

[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, . 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, . 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-analysisa 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, . 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.



通讯作者: