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The Influence of the Basic State on the Northern Hemisphere Circulation Response to Climate Change
2010
Journal of Climate
Employing a comprehensive atmospheric general circulation model, the authors have shown in a previous study that the time-mean Northern Hemisphere (NH) winter circulation response to a CO 2 doubling perturbation depends significantly on parameterized orographic gravity wave drag (OGWD) parameter settings, which are essentially related to the strength of OGWD. A possible implication is that aspects of the greenhouse gas-induced circulation response could depend directly on the formulation and
doi:10.1175/2009jcli3167.1
fatcat:fq525sgu3zccdg6l3e4zqgdz7u