一个重构的 153 年热带太平洋次表层上卷海温资料

doi:10.11978/j.issn.1009-5470.2012.01.001

热带海洋学报 ›› 2012, Vol. 31 ›› Issue (1): 1-9.doi: 10.11978/j.issn.1009-5470.2012.01.001cstr: 32234.14.j.issn.1009-5470.2012.01.001

• 海洋水文学 • 下一篇

一个重构的 153 年热带太平洋次表层上卷海温资料

杜娟 ^1,2 , 郑飞 ¹ , 朱江 ³

1. 中国科学院大气物理研究所国际气候与环境科学中心 , 北京 100029; 2. 中国科学院研究生院 , 北京 100039; 3. 中国科学院大气物理研究所大气边界层物理和大气化学国家重点实验室 , 北京 100029

收稿日期:2012-03-13 修回日期:2010-05-05 出版日期:2012-03-10 发布日期:2012-03-13
通讯作者: 郑飞 E-mail: zhengfei@mail.iap.ac.cn
作者简介: 杜娟 (1982 — ), 女 , 河北省保定市人 , 硕士研究生 , 研究方向 ENSO 年代际可预报性。 E-mail tenni2005@gmail.com
基金资助:
国家自然科学 (40805033, 41075064)

A reconstructed subsurface entrainment temperature data over the tropical Pacific for the past 153y

DU Juan^1,2, ZHENG Fei¹, ZHU Jiang³

1. International Center for Climate and Environment Science ICCES , Institute of Atmospheric Physics , CAS, Beijing 100029, China ; 2. Graduate School of CAS , Beijing 100039, China ; 3. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry LAPC , Institute of Atmospheric Physics , CAS , Beijing 100029, China

Received:2012-03-13 Revised:2010-05-05 Online:2012-03-10 Published:2012-03-13

摘要/Abstract

摘要： 次表层上卷海温对改进ENSO(厄尔尼诺-南方涛动, ElNiñ o-SouthernOscillation)模拟水平及ENSO年代际变化均具有重要作用。利用一个中等复杂程度耦合模式(intermediatecoupledmodel, 简称ICM)和Nudging(张弛逼近)同化方法, 重构了1856—2008年间热带太平洋地区的次表层上卷海温。统计检验表明, 重构的次表层上卷海温与近50年的3种分析资料间具有较高的相关性和较小的均方根误差。此外, 通过此重构的次表层上卷海温资料重新驱动ICM模式, 模拟得到的海表温度距平(seasurfacetemperatureanomaly, 简称SSTA)可以真实地反映出ENSO的年际和年代际变化, 表明此重构的次表层上卷海温资料可用于气候研究, 特别是用于ENSO的大尺度低频变化或年代际气候变化研究。

关键词: 重构的次表层上卷海温, 中等复杂程度耦合模式(ICM), 厄尔尼诺-南方涛动(ENSO)

Abstract: The temperature of subsurface water entrained into the mixed layer ( T _e) is very important to improve El Niño-Southern Oscillation (ENSO ) simulations and modulated ENSO decadal variability. Based on an intermediate coupled model (ICM) and nudging data assimilation method, a long-term monthly-mean T_e dataset is reconstructed over the tropical Pacific for the period of 1856 - 2008. The verification results show that the reconstructed T_e data have high correlations and small root mean square (RMS) errors with three analysis T_e dataset in the last 50 years. Also, the simulated sea surface temperature (SST) anomalies from the ICM, forced by the reconstructed T_e dataset, can simulate realistic interannual and decadal variability of ENSO very well. This indicates that the reconstructed T_e dataset is useful for climate research, especially for the large-scale low frequency or decadal variability of ENSO .

Key words: reconstructed subsurface entrainment temperature, intermediate coupled model, El Niñ, o-Southern Oscillation

中图分类号:

P731

杜娟,郑飞,朱江. 一个重构的 153 年热带太平洋次表层上卷海温资料[J]. 热带海洋学报, 2012, 31(1): 1-9.

DU Juan,ZHENG Fei,ZHU Jiang. A reconstructed subsurface entrainment temperature data over the tropical Pacific for the past 153y[J]. Journal of Tropical Oceanography, 2012, 31(1): 1-9.

参考文献

[1] ZHANG RONGHUA, LEVITUS S. Interannual variability of the coupled tropical Pacific ocean–atmospheric system associated with the El Niño–Southern Oscillation [J]. J Climate, 1997, 10(4): 1312-1330.
[2] 李崇银. 关于 ENSO 本质的进一步研究 [J]. 气候与环境研究, 2002, 7 ( 2 ): 160 - 174.
[3] MCPHADEN M J. Genesis and evolution of the 1997 ～ 98 El Niño [J]. Science, 1999, 283(5404): 950-953.
[4] 巢纪平, 袁绍宇, 巢清尘, 等. 热带西太平洋暖池次表层暖水的起源 —— 对 1997/1998 年 ENSO 事件的分析 [J]. 大气科学, 2003, 27(2): 145 - 151.
[5] 李崇银, 穆穆, 周广庆, 等. ENSO 机理及其预测研究 [J]. 大气科学, 2008, 32(4): 761 - 781.
[6] CANE M A, ZEBIAK S E, DOLAN S C. Experimental forecast of El Niño [J]. Nature, 1986, 321: 827-832.
[7] WANG WEIMIN, MCPHADEN M J. The surface-layer heat balance in the equatorial Pacific Ocean Part Ⅱ: Interannual variability [J]. J Phys Oceanogr, 2000, 30(11): 2989–3008.
[8] 朱杰顺, 周广庆, ZHANG RONGHUA, 等. 参数化次表层上卷海温改进 ENSO 模拟 [J]. 大气科学, 2006, 30(5): 940-951.
[9] ZHANG RONGHUA, ZEBIAK S E, KLEEMAN R, et al. A new intermediate coupled model for El Niño simulation and prediction [J]. Geophys Res Lett, 2003, 30(19), doi: 10. 1029 /2003GL018010.
[10] ZHANG RONGHUA, BUSALACCHIA J, DEWITT D G. The roles of atmospheric Stochastic Forcing (SF) and oceanic entrainment temperature ( T _e ) in decadal modulation of ENSO [J]. J Climate, 2008, 21(4): 674-704.
[11] ZHANG RONGHUA, KLEEMAN R, ZEBIAK S E, et al. An empirical parameterization of subsurface entrainment temperature for improved SST simulations in an intermediate ocean model[J]. J Climate, 2005, 18(2): 350-371.
[12] KEENLYSIDE N S, KLEEMAN R. Annual cycle of equatorial zonal currents in the Pacific [J]. J Geophys Res, 2002, 107(C8), doi: 10. 1029/2000JC000711.
[13] MCCREARY J P. A linear stratified ocean model of the equatorial undercurrent [J]. Philosophical Transactions of Royal Society (London), 1981, 298(1444): 603-635.
[14] ZEBIAK S E, CANE M A. A model El Niño–Southern Oscillation [J]. Mon Wea Rev, 1987, 115(10): 2262-2278.
[15] ZHANG RONGHUA, ZEBIAK S E, KLEEMAN R, et al. Retrospective El Niño forecast using an improved intermediate coupled model[J]. Mon Wea Rev, 2005, 133(9): 2777-2802.
[16] CHANG PING, JI L, SARAVANAN R. A hybrid coupled model study of tropical Atlantic variability[J]. J Climate, 2001, 14(3): 361-390.
[17] ZHENG FEI, DU JUAN, ZHU JIANG. A reconstructed wind stress dataset for climate research over the tropical pacific during a 153-year period [J]. Atmos Oceanic Sci Lett, 2009, 2(5): 277-283.
[18] KAPLAN A, CANE M, KUSHNIR Y, et al. Analyses of global sea surface temperature 1856-1991 [J]. J Geophys Res, 1998, 103(C9): 18567-18589.
[19] REYNOLDS R W, SMITH T M. Improved global sea surface temperature analysis using optimum interpolation [J]. J Climate, 1994, 7(6): 929 - 948.
[20] 赵永平, 吴爱明, 陈永利, 等. 热带太平洋气候变率的三类模态及与 ENSO 强度变化的关系 [J]. 热带海洋学报, 2003, 22(4): 1-9.
[21] ZHENG FEI, ZHU JIANG, ZHANG RONGHUA, et al. Improved ENSO forecasts by assimilating sea surface temperature observations into an intermediate coupled model [J]. Adv Atmos Sci, 2006, 23(4): 615-624.
[22] 黄嘉佑. 气象统计分析与预报方法 [M]. 北京: 气象出版社, 1990: 8-27.
[23] CARTON J A, GIESE B S. A reanalysis of ocean climate using Simple Ocean Data Assimilation (SODA) [J]. Mon Wea Rev, 2008, 136(8): 2999-3017.
[24] BEHRINGER D W, XUE YAN. Evaluation of the global ocean data assimilation system at NCEP [G]// The Pacific Ocean eighth symposium on integrated observing and assimilation systems for atmosphere, oceans, and land surface. Seattle: Amer Meteor Soc, 2004: 11-15.
[25] BEHRINGER D W, JI MING, LEETMAA A. An improved coupled model for ENSO prediction and implications for ocean initialization. Par t Ⅰ: The ocean data assimilation system [J]. Mon Wea Rev, 1998, 126(4): 1013 - 1021.
[26] JI MING, LEETMAA A, DERBER J. An ocean analysis system for seasonal to interannual climate studies [J]. Mon Wea Rev, 1995, 123(2): 460 - 481.
[27] JI MING, SMITH T M. Ocean model response to temperature data and varying surface wind stress: Intercomparisons and implications for climate forecast [J]. Mon Wea Rev, 1995, 123(6): 1811 - 1821.
[28] MONTEREY G I, LEVITUS S. Seasonal variability of mixed layer depth for the world ocean, NOAA NESDIS Atlas 14 [M]. Wash D C: U S. Gov Printing Office, 1997: 96.
[29] 吴洪宝, 吴蕾. 气候变率诊断和预测方法 [M]. 北京: 气象出版社, 2005: 235-235.
[30] TORRENCE C, COMPO G P. A Practical Guide to Wavelet Analysis [J]. Bull Amer Meteor Soc, 1998, 79(1): 61-78.
[31] FARGE M. Wavelet transforms and their applications to turbulence [J]. Annu Rev Fluid Mech, 1992, 24: 395-458.

一个重构的 153 年热带太平洋次表层上卷海温资料

A reconstructed subsurface entrainment temperature data over the tropical Pacific for the past 153y

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