Figure 8 : Accelerations for sea level records artificially extended to 2100.

From: Timescales for detecting a significant acceleration in sea level rise

Figure 8

These records have been adjusted for interannual variability by Calafat and Chambers27 (ad) Fremantle to illustrate a site with relatively large interannual variability; (eh) Newlyn to illustrate a site with relatively small interannual variability; and (il) the CMSL, created by averaging their 10 tide gauge records. Hatched area highlights plot regions where accelerations are significantly different from zero (95% confidence interval). Note, for each sea level record, the plots show results for just one of the 10,000 randomly generated noise time signals.