{"refrec":{"BRefID":127391,"RR":"<b>Wakelin, S.L.; Woodworth, P.L.; Flather, R.A.; Williams, J.A.</b> (2003). Sea-level dependence on the NAO over the NW European Continental Shelf. <i>Geophys. Res. Lett. 30(7)</i>: 1403","BEntID":121461,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geophys. Res. Lett. 30(7)</i>: 1403","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Wakelin, S.L.; Woodworth, P.L.; Flather, R.A.; Williams, J.A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Wakelin, S.L. <i>et al.</i>","Englishabstract":"The connection between changes in the North Atlantic Oscillation ( NAO) and the sea level over the northwest European continental shelf is investigated for the period 1955 - 2000 using a two-dimensional model of tides and storm surges. There is a clear spatial pattern in the correlation between sea level and the NAO on a winter-mean timescale. Correlations are positive (> 0.8) in the northeast and negative (< - 0.7) in the south. The sensitivity of the sea level to the NAO is strongest in the southern North Sea ( up to 96 mm per unit NAO index), where most of the sensitivity is present also in the non-hydrostatic component of sea level. 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