{"refrec":{"BRefID":36294,"RR":"<b>Soomere, T.</b> (2003). Anisotropy of wind and wave regimes in the Baltic proper. <i>J. Sea Res. 49(4)</i>: 305-316. <a href=\"https://dx.doi.org/10.1016/s1385-1101(03)00034-0\" target=\"_blank\">https://dx.doi.org/10.1016/s1385-1101(03)00034-0</a>","BEntID":36294,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>J. Sea Res. 49(4)</i>: 305-316. <a href=\"https://dx.doi.org/10.1016/s1385-1101(03)00034-0\" target=\"_blank\">https://dx.doi.org/10.1016/s1385-1101(03)00034-0</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Soomere, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Soomere, T.","Englishabstract":"The directional distribution of moderate and strong winds in the Baltic Sea region is shown to be strongly anisotropic. The dominating wind direction is south-west and a secondary peak corresponds to north winds. North-west storms are relatively infrequent and north-east storms are extremely rare. Angular distribution of extreme wind speed also has a two-peaked shape with maxima corresponding to south-west and north winds, and a deep minimum for easterly winds. The primary properties of the anisotropy such as prevailing winds, frequency of their occurrence, directional distribution of mean and maximum wind speeds coincide on both sides of the Baltic proper. The specific wind regime penetrates neither into the mainland nor into the Gulf of Finland or the Gulf of Riga. Properties of the saturated wave field in the neighbourhood of proposed sites of the Saaremaa (Ösel) deep harbour are analysed on the basis of the wave model WAM forced by steady winds. The directional distribution of wave heights in typical and extreme storms is highly anisotropic. 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