Chapter 4 Global glacial isostatic adjustment and modern instrumental records of relative sea level history

By W. Richard Peltier. 2001

241 citations recorded by the source corpus.

Subfields: Atmospheric Science, Geophysics, Oceanography

View Paper: https://www.semanticscholar.org/paper/73d5a73c0544c1794b9a16ad9718283044137d56

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Citations in the corpus

Assessing risk of and adaptation to sea-level rise in the European Union: an application of DIVA (2010, methodology): “The latter is a combination of glacial-isostatic adjustment according to the geo-physical model of Peltier (2000) and an assumed uniform 2 mm/year subsidence in deltas.”
Sea level rise and the warming of the oceans in the Simple Ocean Data Assimilation (SODA) ocean reanalysis (2005, methodology): “…from a minimum of 1 mm yr 1 [Nakiboglu and Lambeck, 1991; Shennan and Woodworth, 1992; Lambeck et al., 1998; Cabanes et al., 2001] to a maximum of about 2 mm yr 1 [Douglas, 1991, 1997; Trupin and Wahr, 1990; Peltier, 2001; Miller and Douglas, 2004; Church et al., 2004] during the 20th century.”
Global climate change and potential effects on Pacific salmonids in freshwater ecosystems of southeast Alaska (2009, background): “However, the increase of sea level relative to land is complicated by isostatic rebound (Peltier 2001).”
Nonlinear trends and multiyear cycles in sea level records (2006, methodology): “RSL data sets were corrected for local datum changes and glacial isostatic adjustment (GIA) of the solid Earth [Peltier, 2001].”
Ongoing glacial isostatic contributions to observations of sea level change (2011, methodology): “A correction of this estimate for GIA should be obtained by the removal of a similarly averaged map of absolute sea level rates (Peltier 2001).”
Interannual variations of the mass balance of the Antarctica and Greenland ice sheets from GRACE (2006, methodology): “In the recent years several studies have provided geoid rate maps due to GIA (e.g., Peltier, 2001; Peltier, 2004; Ivins and James, 2005; Tamisiea et al., in press).”
Recent global sea level acceleration started over 200 years ago? (2008, methodology): “All data sets were corrected for local datum changes and glacial isostatic adjustment (GIA) of the solid Earth [Peltier, 2001].”
Global glacial isostatic adjustment: palaeogeodetic and space‐geodetic tests of the ICE‐4G (VM2) model (2002, methodology): “…Laurentian platform cannot be higher than that in VM2, according to the new analyses of Laurentian relaxation times of Peltier (1998a) and Dyke and Peltier (2001), which fix the relaxation time in southeast Hudson Bay to a value near 3.4 kyr (the Lambeck et al., 1996, model, denoted VANU in Fig.”
Spatial Variability of Sea Level Rise in Twenty-First Century Projections (2010, background): “SLR patterns relative to land are also inﬂuenced by geological processes such as glacial isostatic adjustment (Peltier 2001).”