LAUSR

Although global mean sea‐level rise since 1900 and regional mean sea‐level change since the 1960s have been accounted for in terms of the sum of contributions, the same budget closure has not been achieved for local relative sea‐level change from a global network of tide gauges. To address this, we combine new estimates of sterodynamic sea‐level change (SDSL; including ocean dynamics), glacial isostatic adjustment (GIA), change in land ice mass and terrestrial water storage, and other local vertical land motion. We find that the observed trends over 1958–2015 at all 272 tide gauges distributed worldwide agree with the sum of contributions (within 90% confidence estimates), with similar mean trend (1.1 mm yr−1) and comparable spatial variability (standard deviation of 2.0 and 1.9 mm yr−1 respectively). SDSL is the dominant contribution to both local observed mean trend and spatial variability, except at locations close to former ice‐sheets, where GIA dominates.