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...
Published in: | Journal of Glaciology |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
International Glaciology Society
2004
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Subjects: | |
Online Access: | https://doi.org/10.3189/172756503781830386 http://ecite.utas.edu.au/34079 |