Different approaches have been used to compute the mean rate of 20th century global mean
sea level (GMSL) rise from the available tide gauge data: computing average rates from only very long, nearly continuous records; using more numerous but shorter records and filters to separate
nonlinear trends from decadal - scale quasi-periodic variability; neural network methods; computing regional
sea level for specific basins then averaging; or projecting tide gauge records onto empirical orthogonal functions (EOFs) computed from modern altimetry or EOFs from ocean models.