CMIP3 and CMIP5 representation of sea surface temperature in the Tropical Atlantic Ocean

J. M. B. Alves, Emerson Mariano Da Silva, F. Júnior, C. Silveira
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Abstract

This study evaluates WCRP-CMIP3 and CMIP5 representation of the Sea Surface Temperature (SST) in the Atlantic Tropical Basin. The Atlantic Ocean presents thermal variability modes on intraseasonal, interannual and decadal time-scales that affect the climate of the North Atlantic, Caribbean, Western Africa, Northeast Brazil, the Gulf of Guinea Region and Southeast Atlantic (region of the Angolan resurgence). Two main SST modes in the Atlantic are the equatorial and meridional dipoles. These principal modes of SST interannual variabilities are investigated principally by empirical orthogonal function analysis (EOFs) to periods December-January and March-May. For the period of March-May, this study too analyses the relationships of these modes from coupled models of WCRP as rainfall in Northeastern Brazil compared to the observations (1971-2000 - ERSST). This investigation showed principally  that although some models showed high value correlations (above 0.8 in absolute value) for both CMIP3 and CMIP5 with observations using their first two auto values EOFs coefficients of SST in the Tropical Atlantic basin, the simulations in most CMIP3-5 models do not represented the spatial thermal configuration in the basin compared to the observations, and also largely do not reproduce the pattern of correlation between to March-May between precipitation in northern of the NEB and the TSMs in the Tropical Atlantic.
CMIP3 和 CMIP5 对热带大西洋海面温度的描述
本研究评估了 WCRP-CMIP3 和 CMIP5 对大西洋热带盆地海面温度(SST)的表示。大西洋在季内、年际和十年时间尺度上呈现热变率模式,影响北大西洋、加勒比海、非洲西部、巴西东北部、几内亚湾地区和东南大西洋(安哥拉回升地区)的气候。大西洋的两种主要 SST 模式是赤道偶极和子午线偶极。主要通过对 12 月至 1 月和 3 月至 5 月期间的经验正交函数分析(EOFs)来研究这些主要的 SST 年际变化模式。在 3-5 月期间,本研究还分析了巴西东北部降雨量与观测数据(1971-2000 年 - ERSST)的关系,并将这些模式与 WCRP 耦合模式进行了比较。这项调查主要表明,虽然一些模式利用其热带大西洋海盆 SST 的前两个自动值 EOFs 系数,显示 CMIP3 和 CMIP5 与观测值有很高的相关性(绝对值在 0.8 以上),但与观测值相比,大多数 CMIP3-5 模式的模拟并不能代表海盆的空间热配置,而且在很大程度上也不能再现东北大西洋北部 3-5 月降水量与热带大西洋 TSM 之间的相关模式。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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