Wave-1 and 2 are distinct atmospheric circulation patterns whereby we have "one" notable ridge and trough signal, or "two" ridges and troughs throughout a given spacial domain.  Certain tropospheric patterns constructively interfere or enhance wave-1 resonance by nature of the fact that they project upon the climatological wave-1 or wave-2 circulations.  This has been almost a perfect progression for a major SSW, and we're seeing that. Wave-1 preconditioning/displacement and elongation