How will sea level respond to changes in natural and anthropogenic forcings by 2100?

248 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? (2013, methodology): “…methods for projecting GMSLR, which depend on calibrating a relationship between global climate change or radiative forcing and the rate of GMSLR from observational data Unauthenticated | Downloaded 01/05/21 01:42 PM UTC (Rahmstorf 2007; Vermeer and Rahmstorf 2009; Jevrejeva et al. 2010).”
The solid Earth’s influence on sea level (2013, background): “Even more drastic scenarios that predict 1.3–2.0 m of global rise in the next century (Grinsted et al., 2009; Jevrejeva et al., 2010; Pfeffer et al., 2008; Rahmstorf, 2007; Vermeer and Rahmstorf, 2009) make sea level one of the most tangible and dramatic consequences of future climate change.”
The land ice contribution to sea level during the satellite era (2017, methodology): “These models use the relationship between past changes in SLR and surface air temperature to predict future changes based on climate warming scenarios (Jevrejeva et al 2010, Rahmstorf 2007).”