Extended Data Fig. 2: GMSL change related to spatially uniform covariance functions.
From: Modern sea-level rise breaks 4,000-year stability in southeastern China
This covariance function (g(t)) primarily reflects contributions from processes that are not explained by GIAg(t), such as centennial GMSL fluctuations (as GIAg(t) typically has a temporal resolution of 500–1,000 years), GMSL variation associated with mountain glaciers and global thermosteric expansion. Dark shading, 68% CI; light shading, 95% CI.
