Our comparison of the GPS data to models
for glacial isostatic adjustment suggests that some parts of western coastal Greenland were experiencing accelerated melting of coastal ice by the late 1990s.
The data has been adjusted
for glacial isostatic adjustment.
You really need to look at multi-decadal time periods to determine trends, as in Church and White 2011 who found «1900 to 2009 is 1.7 ± 0.2 mm / year and since 1961 is 1.9 ± 0.4 mm / year» and «For 1993 — 2009 and after correcting
for glacial isostatic adjustment, the estimated rate of rise is 3.2 ± 0.4 mm / year from the satellite data and 2.8 ± 0.8 mm / year from the in situ data».
Not exact matches
Some groups have tried to develop models of the rebounding land, so that sea level researchers can apply «
Glacial Isostatic Adjustments» (GIA) to their data to correct
for the effects.
Finally, they believe that an
adjustment of +0.3 mm / yr is necessary to account
for Peltier's
Glacial Isostatic Adjustments (see Section 4).
We suggest that the resolution of this issue is consistent with our estimate of the approximately +7 m Holsteinian global sea level, and is provided by Raymo & Mitrovica [58], who pointed out the need to make a
glacial isostatic adjustment (GIA) correction
for post-
glacial crustal subsidence at the places where Hearty and others deduced local sea - level change.
«We have to account
for the fact that the ocean basins are actually getting slightly bigger... water volume is expanding,» he said, a phenomenon they call
glacial isostatic adjustment (GIA).
A deglacial model
for Antarctica: geological constraints and glaciological modelling as a basis
for a new model of Antarctic
glacial isostatic adjustment.