Ice-shelf elevation changes due to atmospheric pressure variations

The inverse barometer effect (IBE) is the isostatic response of ocean surface height to changes in atmospheric pressure (Pair) at a rate of about 1 cm hPa-1. The IBE is a significant contributor to variability of ice-shelf surface elevation (ice), as we demonstrate with simultaneous global positioni...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Padman, L, King, MA, Goring, D, Corr, H, Coleman, R
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciology Society 2004
Subjects:
Online Access:https://doi.org/10.3189/172756503781830386
http://ecite.utas.edu.au/34079