“…2a): (1) 1938-1970, when higher subsidence rates were responsible for acceleration in RSLR, and (2) 1970-2010, when RSLR slowed (Rizzetto and Tosi, 2011). The identification of minor RSLR fluctuations, probably related to climatic phenomena such as the North Atlantic Oscillation (NAO), the East Atlantic/Western Russia (EA-WR), and the Scandinavian Patterns, and to variations in solar activity (Woolf et al, 2003;Kolker, 2005;Bellucci et al, 2007;Zanchettin et al, 2009), induced us to distinguish some subperiods: 1938-1950 (quite stable sea level), 1950-1970 (significant increase of RSLR), (slowing down of RSLR rates), 1990-1996 (increasing sea level), and 1996-2008 (new steady conditions). The last period (2008)(2009)(2010) was characterized by a rapid increase of RSLR, but it was too short to provide a correct trend.…”