Northern Winter Stationary Waves: Theory and Modeling

By I. Held, M. Ting, Hailan Wang. 2002

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The Tropical Dynamical Response to Latent Heating Estimates Derived from the TRMM Precipitation Radar (2004, result): “The results of previous studies (Wang and Ting 1999; Held et al. 2002) also suggest that the absence of orography, transients, and wave–mean-flow interactions are unlikely to have a strong influence on tropical circulation anomalies (except for orographic influences near the Tibetan Plateau).”
The predictability of the extratropical stratosphere on monthly time‐scales and its impact on the skill of tropospheric forecasts (2015, background): “1 of Butler and Polvani (2011) to include data up to June 2013 and has slight changes to both the Niño3.”
An Evaluation of the Large‐Scale Atmospheric Circulation and Its Variability in CESM2 and Other CMIP Models (2020, background): “Stationary waves, or zonal asymmetries, in the atmospheric circulation arise through interactions between the zonal mean flow, orography, diabatic heating, and transient vorticity and divergence fluxes (e.g., Held et al., 2002; Wang & Ting, 1999).”