The connections of Black Sea storminess activity with teleconnection patterns (climatic indexes) were performed on the base of visual wave observations (Voluntary Observing Ship) and WAM modelling. The annual maximal waves are more affected by AMO and PDO, but annual mean waves by NAO. It is shown that for qualitative analysis of climatic variability of waves on short- and middle-time periods, in general, one can use numerical simulation data even at one point of sea combining classical correlation analysis with wavelet analysis methods and parametric spectral analysis. In WAM modelling data, a long-term periodicity cannot be defined.
