Change in the Tropical Hadley Cell Since 1950

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Atmospheric bridge, oceanic tunnel, and global climatic teleconnections (2007, background): “…overturning cell forms that opposes the mean Hadley circulation between 15 N and 30 N [Waliser et al., 1999; Quan et al., 2004]; and the response is nonlinear; that is, the circulation between 15 N and 15 S is much stronger during El Niño than La Niña events (our Figure 6) [Quan et al., 2004].”
Recent behavior of the Hadley cell and tropical thermodynamics in climate models and reanalyses (2006, background): “[2] Several recent studies have shown that there are significant trends in the strength of the tropical atmospheric circulation over recent decades in major reanalysis products [Mitas and Clement, 2005; Quan et al., 2004; Tanaka et al., 2004].”
Local partitioning of the overturning circulation in the tropics and the connection to the Hadley and Walker circulations (2014, background): “…[e.g., Oort and Yienger, 1996; Chen et al., 2002; Vecchi et al., 2006; Yu and Zwiers, 2010 ], and trends in their position and strength [e.g., Quan et al., 2004; Mitas and Clement, 2005; Zhao and Moore, 2008; Hu and Fu, 2007; Stachnik and Schumacher, 2011], including possible changes under…”