Eddy-Mediated Regime Transitions in the Seasonal Cycle of a Hadley Circulation and Implications for Monsoon Dynamics

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Stratospheric Ozone Depletion: The Main Driver of Twentieth-Century Atmospheric Circulation Changes in the Southern Hemisphere (2011, background): “This is rather surprising, given our current understanding of the interplay between the Hadley cell and the midlatitude, eddy-driven jet (Walker and Schneider 2006; Schneider and Bordoni 2008).”
WATER VAPOR AND THE DYNAMICS OF CLIMATE CHANGES (2009, background): “…of the cross-equatorial JJA Hadley cell is not primarily controlled by the eddy momentum flux divergence (Ro| & 0.5 in much of its upper branch) [Walker and Schneider 2005, 2006; Schneider and Bordoni 2008; see Dima et al. 2005 for a more detailed analysis of the tropical zonal momentum balance].”
Expansion of the Hadley Cell under Global Warming: Winter versus Summer (2012, background): “1 2012 American Meteorological Society the winter HC is relatively closer to the nearly inviscid limit while the summer HC is more subject to the influence of eddy momentum fluxes originating from the midlatitudes (Schneider and Bordoni 2008; Bordoni and Schneider 2010).”