地球科学进展

地球科学进展 ›› 2018, Vol. 33 ›› Issue (8): 808 -817. doi: 10.11867/j.issn.1001-8166.2018.08.0808

综述与评述 上一篇    下一篇

热带北大西洋模态年际变率的研究进展与展望
杨韵( ), 李建平, 谢飞, 冯娟, 孙诚   
  1. 北京师范大学全球变化与地球系统科学研究院,北京 100875
  • 收稿日期:2018-04-08 修回日期:2018-06-14 出版日期:2018-08-10
  • 基金资助:
    国家重点研发计划项目“全球变化及应对”重点专项“全球变暖‘停滞’现象辨识与机理研究”(编号:2016YFA0601803);国家自然科学基金青年科学基金项目“印度洋偶极子年代际变率:ENSO强迫和内部变率”(编号:41606008)资助.

Progresses and Prospects for North Tropical Atlantic Mode Interannual Variability

Yun Yang( ), Jianping Li, Fei Xie, Juan Feng, Cheng Sun   

  1. College of Global Change and Earth System Science,Beijing Normal University,Beijing 100875,China
  • Received:2018-04-08 Revised:2018-06-14 Online:2018-08-10 Published:2018-09-14
  • About author:

    First author:Yang Yun(1988-),female,Anshan City,Liaoning Province,Lecturer. Research areas include ocean-atmosphere interaction and climate change. E-mail:yunyang@bnu.edu.cn

  • Supported by:
    Project supported by the National Key Research and Development Program of China “Research on the global warming hiatus: The impact of ocean dynamics to heat redistribution”(No.2016YFA0601803);The National Natural Science Foundation of China “Indian Ocean Dipole decadal variability: ENSO forcing and internal variability”(No.41606008).
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热带北大西洋模态(NTAM)年际变率是北半球春季热带北大西洋的主导变率。它对热带辐合带的南北移动、周边国家的降水以及全球气候都有显著的影响。通过回顾前人的相关研究,归纳了NTAM的几种形成机制,概括了NTAM对气候系统的影响,综述了模式对于NTAM年际变率的模拟能力,总结了以往研究进展中存在的薄弱环节。最后以此为契机,对未来NTAM的研究方向进行了展望。

关键词: 热带北大西洋模态, 年际变率, 海气相互作用

North Tropical Atlantic Mode (NTAM) is the leading variability of the boreal spring sea surface temperature anomalies over the North Tropical Atlantic at interannual timescale. It is also known as the northern pole of the Atlantic Meridional Mode (AMM). NTAM shows significant impact on the shift of Intertropical Convergence Zone, the precipitation of the surrounding countries, the quasi-biennial oscillation of El Nino-Southern Oscillation (ENSO), and the recent global warming hiatus. Despite its distinct influence on global climate, NTAM has not received equivalent attention as other tropical variability (e.g. ENSO). By revisiting previous studies, this paper summarized the triggers and mechanisms responsible for the evolution and development of NTAM, including remote forcing from ENSO, south tropical Atlantic as well as North Atlantic Oscillation (NAO), local air-sea coupling, and the interactions among different triggers. Also, this paper detailedly introduced the ability of CMIP5 (The fifth phase of the Coupled Model Intercomparison Project) model simulation. The prominent model biases over the equatorial Atlantic significantly limit the study of NTAM. Finally, a future prospective of NTAM interannual variability was presented.

Key words: North Tropical Atlantic Mode, Interannual variability, Ocean-atmosphere interaction.

中图分类号: 

图1 HadISST 1870—2017年春季SST
(a)热带大西洋(30°S~30°N, 70°W~20°E) EOF分解的第二模态,黑框代表AMM北部的一支;(b)热带北大西洋(0°~30°N, 100°W~20°E)EOF分解的第一模态,单位为℃;(c)NTAM指数(SST在5°~25°N, 60°~20°W的均值)在不同月份的方差(单位:℃ 2)
Fig.1 HadISST boreal spring SST during 1870-2017
(a) 2 nd EOF mode over the tropical Atlantic (30°S~30°N, 70°W~20°E), the black box represents the northern pole of the AMM;(b) 1 st EOF mode over the northern tropical Atlantic (0°~30°N, 100°W~20°E) (unit: ℃); (c) The variance of NTAM index (SST averaged over 5°~25°N, 60°~20°W) in calendar months (unit: ℃ 2)
图1 HadISST 1870—2017年春季SST
(a)热带大西洋(30°S~30°N, 70°W~20°E) EOF分解的第二模态,黑框代表AMM北部的一支;(b)热带北大西洋(0°~30°N, 100°W~20°E)EOF分解的第一模态,单位为℃;(c)NTAM指数(SST在5°~25°N, 60°~20°W的均值)在不同月份的方差(单位:℃ 2)
Fig.1 HadISST boreal spring SST during 1870-2017
(a) 2 nd EOF mode over the tropical Atlantic (30°S~30°N, 70°W~20°E), the black box represents the northern pole of the AMM;(b) 1 st EOF mode over the northern tropical Atlantic (0°~30°N, 100°W~20°E) (unit: ℃); (c) The variance of NTAM index (SST averaged over 5°~25°N, 60°~20°W) in calendar months (unit: ℃ 2)
图2 NTAM的触发因子示意图
Fig.2 Schematic diagram of NTAM triggers
图2 NTAM的触发因子示意图
Fig.2 Schematic diagram of NTAM triggers
表1 NTAM与其他变率的相关系数
Table 1 Correlation coefficients between NTAM and other variability
NAT NAH Atlantic Niño AMO (年代际)
相关系数 -0.24 -0.16 -0.08* 0.64
表1 NTAM与其他变率的相关系数
Table 1 Correlation coefficients between NTAM and other variability
NAT NAH Atlantic Ni?o AMO (年代际)
相关系数 -0.24 -0.16 -0.08* 0.64
图3 NTAM的气候影响示意图
Fig.3 Schematic diagrams of NTAM impacts on global climate
图3 NTAM的气候影响示意图
Fig.3 Schematic diagrams of NTAM impacts on global climate
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