Baroclinic instability and large?scale wave propagation in a planetary?scale atmosphere
نویسندگان
چکیده
Midlatitude atmospheric variability is dominated by the dynamics of baroclinically unstable jet stream, which meanders and sheds eddies at scale Rossby deformation radius. The interact with each other jet, affecting on a wide range scales, but mechanisms planetary-scale fluctuations are not well understood. Here, we develop theoretical framework to explore stability motions in an idealized two-layer model atmosphere. based combination vertical shear Sverdrup relation, providing dynamic link between two layers, meridional eddy heat fluxes parameterized as diffusive process memory past baroclinicity jet. We find that instability exists if does exceed particular threshold. inclusion eddy-memory effect enables westward or eastward propagation planetary waves relative barotropic mean flow. Importantly, growing propagate slowly stationary, could have important implications for formation blocking events. Our results suggest that, ongoing polar amplification due global warming corresponding reduction wind, background conditions growth via baroclinic becoming more favorable.
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ژورنال
عنوان ژورنال: Quarterly Journal of the Royal Meteorological Society
سال: 2022
ISSN: ['1477-870X', '0035-9009']
DOI: https://doi.org/10.1002/qj.4232