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Douglas E. Miller and Zhuo Wang

Atlantic and impact weather and climate over eastern North America and western Europe ( Hurrell 1995 ; Scaife et al. 2008 ). The NAO is a regional manifestation of the Arctic Oscillation (AO), or the northern annular mode (NAM), which is considered the dominant mode of variability in the Northern Hemisphere extratropics ( Thompson and Wallace 1998 ). Previous studies (e.g., DeWeaver and Nigam 2000 ; Hurrell et al. 2003 ) suggested that the internal dynamics of the atmosphere, particularly eddy

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Eric D. Maloney, Andrew Gettelman, Yi Ming, J. David Neelin, Daniel Barrie, Annarita Mariotti, C.-C. Chen, Danielle R. B. Coleman, Yi-Hung Kuo, Bohar Singh, H. Annamalai, Alexis Berg, James F. Booth, Suzana J. Camargo, Aiguo Dai, Alex Gonzalez, Jan Hafner, Xianan Jiang, Xianwen Jing, Daehyun Kim, Arun Kumar, Yumin Moon, Catherine M. Naud, Adam H. Sobel, Kentaroh Suzuki, Fuchang Wang, Junhong Wang, Allison A. Wing, Xiaobiao Xu, and Ming Zhao

representations of weather and future climate. These include biases in the cold tongue and intertropical convergence zone regions (e.g., Li and Xie 2014 ; Grose et al. 2014 ), the structure of El Niño–Southern Oscillation (ENSO) sea surface temperature (SST) and precipitation anomalies (e.g., Bellenger et al. 2014 ; Grose et al. 2014 ), simulation of the Madden–Julian oscillation (MJO; Kim et al. 2014a ; Hung et al. 2013 ; Jiang et al. 2015 ; Ahn et al. 2017 ), tropical monsoon precipitation and

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