Impacts of Atlantic multidecadal variability on the tropical Pacific: a multi-model study

被引:34
|
作者
Ruprich-Robert, Yohan [1 ]
Moreno-Chamarro, Eduardo [1 ]
Levine, Xavier [1 ]
Bellucci, Alessio [2 ,3 ]
Cassou, Christophe [4 ]
Castruccio, Frederic [5 ]
Davini, Paolo [6 ]
Eade, Rosie [7 ]
Gastineau, Guillaume [8 ]
Hermanson, Leon [7 ]
Hodson, Dan [9 ]
Lohmann, Katja [10 ]
Lopez-Parages, Jorge [4 ]
Monerie, Paul-Arthur [9 ]
Nicoli, Dario [2 ]
Qasmi, Said [4 ,11 ]
Roberts, Christopher D. [12 ]
Sanchez-Gomez, Emilia [4 ]
Danabasoglu, Gokhan [5 ]
Dunstone, Nick [7 ]
Martin-Rey, Marta [13 ]
Msadek, Rym [4 ]
Robson, Jon [9 ]
Smith, Doug [7 ]
Tourigny, Etienne [1 ]
机构
[1] Barcelona Supercomp Ctr, Barcelona, Spain
[2] Fdn Ctr EuroMediterraneo Cambiamenti Climatici, Bologna, Italy
[3] CNR, Ist Sci Atmosfera & Clima, Bologna, Italy
[4] Univ Toulouse, CNRS, CERFACS, CECI, Toulouse, France
[5] Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA
[6] CNR, Ist Sci Atmosfera & Clima, Turin, Italy
[7] Met Off, Exeter, Devon, England
[8] Sorbonne Univ, CNRS, MNHN, IRD,LOCEAN, Paris, France
[9] Univ Reading, Natl Ctr Atmospher Sci, Dept Meteorol, Reading, Berks, England
[10] Max Planck Inst Meteorol, Hamburg, Germany
[11] Univ Toulouse, CNRS, CNRM, Meteo France, Toulouse, France
[12] ECMWF, Reading, Berks, England
[13] CSIC, Inst Ciencias Mar, Barcelona, Spain
基金
美国国家科学基金会; 欧盟地平线“2020”; 美国海洋和大气管理局;
关键词
EQUATORIAL PACIFIC; NORTH-ATLANTIC; EL-NINO; HIATUS; PRECIPITATION; CIRCULATIONS; TRENDS; LINK;
D O I
10.1038/s41612-021-00188-5
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Atlantic multidecadal variability (AMV) has been linked to the observed slowdown of global warming over 1998-2012 through its impact on the tropical Pacific. Given the global importance of tropical Pacific variability, better understanding this Atlantic-Pacific teleconnection is key for improving climate predictions, but the robustness and strength of this link are uncertain. Analyzing a multi-model set of sensitivity experiments, we find that models differ by a factor of 10 in simulating the amplitude of the Equatorial Pacific cooling response to observed AMV warming. The inter-model spread is mainly driven by different amounts of moist static energy injection from the tropical Atlantic surface into the upper troposphere. We reduce this inter-model uncertainty by analytically correcting models for their mean precipitation biases and we quantify that, following an observed 0.26 degrees C AMV warming, the equatorial Pacific cools by 0.11 degrees C with an inter-model standard deviation of 0.03 degrees C.
引用
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页数:11
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