Change to the height of sea level, both globally and locally   due to  a change in ocean volume as a result of a change in the mass of water in the ocean ,  changes in ocean volume as a result of changes in ocean water density ,  changes in the shape of the ocean basins and changes in the Earth's gravitational and rotational fields and  local subsidence or uplift of the land. Global mean sea level change resulting from change in the mass of the ocean is called barystatic. The amount of barystatic sea level change due to the addition or removal of a mass of water is called its sea level equivalent . Sea level changes, both globally and locally, resulting from changes in water density are called steric. Density changes induced
IPCC
Climate Change 2022: Impacts, Adaptation and Vulnerability
IPCC Report