Atmospheric blocking in a high resolution climate model: influences of mean state, orography and eddy forcing

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The DOE E3SM Coupled Model Version 1: Description and Results at High Resolution (2019, background): “Blocking of flow with resulting air stagnation problems is also better resolved as mountains and valleys come into focus (Berckmans et al., 2013; Jung et al., 2012; Matsueda et al., 2009; Schiemann et al., 2017).”
Persistent Extratropical Regimes and Climate Extremes (2015, background): “In some models, however, the biases in blocking and other regimes have been much reduced, probably through a combination of increased vertical as well as horizontal model resolution and improved parameterisations [11–16].”
Low‐frequency nonlinearity and regime behavior in the Northern Hemisphere extratropical atmosphere (2017, background): “It is likely that the superior performance of the T1279 model configuration results from more realistic orography [Jung et al., 2012; Berckmans et al., 2013] and also from more realistic representation of nonlinear Rossby wave breaking processes, which are known to be important in maintaining…”