Stratosphere–Troposphere Coupling in a Relatively Simple AGCM: The Importance of Stratospheric Variability

167 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

The Steady-State Atmospheric Circulation Response to Climate Change–like Thermal Forcings in a Simple General Circulation Model (2010, background): “Gerber and Polvani (2009) and Chan and Plumb (2009) revealed the sensitivity of the results in Polvani and Kushner (2002) to the presence of topography and the tropospheric equilibrium temperature profile, respectively.”
Sudden Stratospheric Warmings (2020, background): “More recently, idealized GCM studies have found a sharp increase in SSW frequency as planetary scale zonal asymmetries in the underlying ﬂow are increased, either by topography (e.g., Taguchi and Yoden (2002); Gerber and Polvani (2009)) or thermal perturbations (Lindgren et al., 2018).”
Impact of stratospheric ozone on Southern Hemisphere circulation change: A multimodel assessment (2010, background): “Gerber and Polvani [2009] and Chan and Plumb [2009] have also shown that the stratospheric influence on the tropospheric circulation is highly sensitive to the background flow in the troposphere.”