Skilful multi-year predictions of tropical trans-basin climate variability

被引:111
作者
Chikamoto, Yoshimitsu [1 ]
Timmermann, Axel [1 ,2 ]
Luo, Jing-Jia [3 ]
Mochizuki, Takashi [4 ]
Kimoto, Masahide [5 ]
Watanabe, Masahiro [5 ]
Ishii, Masayoshi [6 ]
Xie, Shang-Ping [7 ]
Jin, Fei-Fei [8 ]
机构
[1] Univ Hawaii Manoa, Int Pacific Res Ctr, Honolulu, HI 96822 USA
[2] Univ Hawaii Manoa, Dept Oceanog, Honolulu, HI 96822 USA
[3] Bur Meteorol, Ctr Australian Weather & Climate Res, Melbourne, Vic 3001, Australia
[4] Japan Agcy Marine Earth Sci & Technol, Kanazawa Ku, Yokohama, Kanagawa 2360001, Japan
[5] Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba 2778568, Japan
[6] Japan Meteorol Agcy, Meteorol Res Inst, Tsukuba, Ibaraki 3050052, Japan
[7] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
[8] Univ Hawaii Manoa, Dept Meteorol, Honolulu, HI 96822 USA
来源
NATURE COMMUNICATIONS | 2015年 / 6卷
基金
美国国家科学基金会;
关键词
SEA-SURFACE TEMPERATURE; DECADAL-SCALE CLIMATE; OCEAN HEAT UPTAKE; DATA ASSIMILATION; WARMING HIATUS; INDO-PACIFIC; EL-NINO; ATLANTIC; ENSO; CIRCULATION;
D O I
10.1038/ncomms7869
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Tropical Pacific sea surface temperature anomalies influence the atmospheric circulation, impacting climate far beyond the tropics. The predictability of the corresponding atmospheric signals is typically limited to less than 1 year lead time. Here we present observational and modelling evidence for multi-year predictability of coherent trans-basin climate variations that are characterized by a zonal seesaw in tropical sea surface temperature and sea-level pressure between the Pacific and the other two ocean basins. State-of-the-art climate model forecasts initialized from a realistic ocean state show that the low-frequency trans-basin climate variability, which explains part of the El Nino Southern Oscillation flavours, can be predicted up to 3 years ahead, thus exceeding the predictive skill of current tropical climate forecasts for natural variability. This low-frequency variability emerges from the synchronization of ocean anomalies in all basins via global reorganizations of the atmospheric Walker Circulation.
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页数:7
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