Sea level lies at the intersection of Earth's solid, liquid, and gaseous components, and thus forms a fundamental boundary on our planet that affects both biology and geology.
Human society must adjust to changes in this boundary, which is now rising 2-3 mm per year. Although climatological factors such as seawater warming and glacial melting are major contributors to sea level rise, deformation of the solid earth also exerts an important, and often dominating, influence on sea level.