The influence of time‐dependent ocean‐continent geometry on predictions of post‐glacial sea level change in Australia and New Zealand
- 15 March 1998
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 25 (6) , 793-796
- https://doi.org/10.1029/98gl00498
Abstract
No abstract availableThis publication has 9 references indexed in Scilit:
- Postglacial sea-level change on a rotating Earth: first results from a gravitationally self-consistent sea-level equationGeophysical Journal International, 1996
- Shoreline reconstructions for the Persian Gulf since the last glacial maximumEarth and Planetary Science Letters, 1996
- Haskell [1935] revisitedJournal of Geophysical Research, 1996
- The effect of spatially non-uniform water loads on prediction of sea-level changeGeophysical Journal International, 1993
- On postglacial geoid subsidence over the equatorial oceansJournal of Geophysical Research, 1991
- Ice‐3G: A new global model of Late Pleistocene deglaciation based upon geophysical predictions of post‐glacial relative sea level changeJournal of Geophysical Research, 1991
- Late Pleistocene and Holocene sea-level change in the Australian region and mantle rheologyGeophysical Journal International, 1989
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981
- On Postglacial Sea LevelGeophysical Journal of the Royal Astronomical Society, 1976