Ongoing glacial isostatic contributions to observations of sea level change

By M. Tamisiea. 2011

156 citations recorded by the source corpus.

Subfields: Aerospace Engineering, Astronomy and Astrophysics, Oceanography

View Paper: https://www.semanticscholar.org/paper/7942ef9891ee7dcd0d511ff80db561e3ca223e50

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Aerospace Engineering

1. Richard M. Westaway
2. Jonathan L. Bamber
3. P. Whitehouse
4. B. Marzeion
5. Bert Wouters

In Astronomy and Astrophysics

1. Richard M. Westaway
2. Erik Ivins
3. Jonathan L. Bamber
4. P. Whitehouse
5. B. Marzeion
6. Bert Wouters

In Oceanography

1. P. Whitehouse
2. Richard M. Westaway
3. L. Caron
4. S. Adhikari
5. G. Blewitt
6. Erik Ivins
7. Eric Y. Larour
8. Jonathan L. Bamber

Citations in the corpus

• GIA Model Statistics for GRACE Hydrology, Cryosphere, and Ocean Science (2018, background): “GIA uncertainty on ocean mass and sea level trends have been treated by Tamisiea (2011), and the influence of forebulge collapse on North American hydrology has been discussed by Roy and Peltier (2017).”
• The land ice contribution to sea level during the satellite era (2017, methodology): “It implies a positive contribution from land hydrology and/or other factors such as a GIA trend on ocean basin volume closer to the lower end of estimates of −0.15 mm yr−1 (Tamisiea 2011).”
• Glacial isostatic adjustment modelling: historical perspectives, recent advances, and future directions (2018, background): “This ocean syphoning effect explains why mid-Holocene sea-level highstands are observed across many equatorial regions (Mitrovica and Peltier, 1991b; Mitrovica and Milne, 2002), and it must also be accounted for when interpreting contemporary measurements of global sea-level change derived from sate”