Recent global sea level acceleration started over 200 years ago?

By Svetlana Jevrejeva, John C. Moore, Aslak Grinsted, Philip L. Woodworth. 2008

484 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/f14c5342d21fd31ea994f9430c06324a10b104d9

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Citations in the corpus

Climate change impacts on marine ecosystems. (2012, background): “Viewed more positively, protection from local stressors can make reefs more resilient in the face of global change (Knowlton & Jackson 2008).”
Is there a 60‐year oscillation in global mean sea level? (2012, methodology): “…multi-decadal oscillation is between 50 and 60 years, based on analysis of two gauges in the North Atlantic [Sturges and Douglas, 2011] or a GMSL reconstruction from numerous gauges, the majority of which are in the North Atlantic before 1950 [Jevrejeva et al., 2008; Wenzel and Schröter, 2010].”
The solid Earth’s influence on sea level (2013, background): “2A) during the past 10– 100 yr (Church and White, 2011), and perhaps longer (Jevrejeva et al., 2008), has been attributed to the melting of continental ice into the oceans (Leuliette and Miller, 2009; Miller and Douglas, 2004).”
Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? (2013, methodology): “The relatively constant rate of twentieth-century GMSLR requires an explanation for the apparent onset of GMSLR during the nineteenth or early twentieth century (e.g., Jevrejeva et al. 2008; Gehrels and Woodworth 2013), before substantial anthropogenic climate change had occurred.”
Global sea-level rise and its relation to the terrestrial reference frame (2009, result): “However, it suggests that previous estimates (Holgate 2007; Jevrejeva et al. 2008; Wöppelmann et al. 2009) represent an upper bound, as well as a significant departure from altimetry-based estimates of 3.3 ± 0.4 mm/year over the recent period from 1993 to 2007.”
Reconstructing sea level from paleo and projected temperatures 200 to 2100AD (2009, background): “The issue of how well the Amsterdam record represents global sea level was treated in some detail in Jevrejeva et al. (2008b) , and the representativity error dominates the uncertainties in local station vertical movement.”
How will sea level respond to changes in natural and anthropogenic forcings by 2100? (2010, methodology): “, 2009], constrained by the global sea level record from tide gauges [Jevrejeva et al., 2008], and driven by various forcing time series.”
Contemporary sea level rise. (2010, background): “Another global mean sea level reconstruction from 1700 to the present ( Jevrejeva et al. 2008) reported a sea level acceleration of ∼0.01 mm year−2.”