| Title | Ocean loading effects on the prediction of Antarctic glacial isostatic uplift and gravity rates |
| Author | Simon, K M; James, T S; Ivins, E R |
| Source | Journal of Geodesy 2010, 13 pages, https://doi.org/10.1007/s00190-010-0368-4 |
| Year | 2010 |
| Alt Series | Earth Sciences Sector, Contribution Series 20090174 |
| Publisher | Springer Nature |
| Document | serial |
| Lang. | English |
| Media | on-line; digital |
| File format | pdf |
| Area | Antarctica |
| Lat/Long WENS | -180.0000 180.0000 -60.0000 -90.0000 |
| Subjects | geophysics; surficial geology/geomorphology; Nature and Environment; crustal uplift; gravity; crustal movements; sea level fluctuations; sea level changes; ice thickness; glaciation; global positioning
system |
| Illustrations | sketch maps; cross-sections; formulae |
| Released | 2010 02 12 |
| Abstract | The effect of regional ocean loading on predicted rates of crustal uplift and gravitational change due to glacial isostatic adjustment (GIA) is determined for Antarctica. The effect is found to be
significant for the ICE-3G and ICE-5G loading histories (up to -8 mm/year and -3 mm/year change in uplift rate and -3 cm/year and -1 cm/year equivalent water height change (EWHC) of surface mass, respectively). The effect is smaller (+1 mm/year;
+0.25 cm/year) for the IJ05 loading history. The impact of ocean loading on the rate of change of the long-wavelength zonal harmonics of the Earth's gravitational field is also significantly smaller for IJ05 than ICE-3G. A simple analytical formula
is derived that is accurate to about 3% in a root-mean-square sense that relates predicted or observed gravitational change at the surface of the Earth (r = a) to the EWHC. A fundamental difference in the definition of the load histories accounts for
the differing sensitivities to ocean loading. IJ05 defines its surface load history relative to the present-day surface load, rather than specifying an absolute loading history, and thus implicitly approximates the temporal and spatial mass exchange
between grounded ice and open ocean. In contrast, ICE-3G and ICE-5G specify an absolute load history and explicit regional ocean loading substantially perturbs predicted GIA rates. Conclusions of previous studies that used IJ05 predictions without
ocean loading are relatively robust. |
| GEOSCAN ID | 247820 |
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