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AbstractAbstract
[en] The extratropical low-frequency variability is one of the most important components in extratropical dynamics. While there are some understanding of the high-frequency, synoptic scale storm track eddy development due to baroclinic instability theory, its low-frequency counterpart is poorly understood and the theory for that is slowly evolving. The main difficulty seems to be lying on the fact that the problem is three dimensional in nature
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Shepherd, T.G. (ed.); McGill Univ., Montreal, PQ (Canada). Dept. of Atmospheric and Oceanic Sciences; 219 p; Feb 1994; p. 193-202; 17. Stanstead seminar; Quebec (Canada); 13-18 Jun 1993; Also available from OSTI as DE94017651; NTIS; US Govt. Printing Office Dep
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