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Synchronous coupled ice-ocean model of Smith Glacier forced by warm climate
GB/NERC/BAS/PDC/01480

Summary

Abstract:
The output of a 40-year coupled ice-ocean run of Smith Glacier, the adjoining Dotson and Crosson ice shelves, and the nearby continental shelf, with ocean boundary conditions forced with a climatology downscaled from a regional model of the Amundsen Sea.

Funding was provided by the NERC Standard Grant NE/M003590/1 - Is ice loss from West Antarctica driven by ocean forcing or ice and ocean feedbacks?

Keywords:
Dotson ice shelf, Smith glacier, coupled modelling, ice shelf, ice stream

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Citation

Goldberg, D. (2021). Synchronous coupled ice-ocean model of Smith Glacier forced by warm climate (Version 1.0) [Data set]. UK Polar Data Centre, Natural Environment Research Council, UK Research & Innovation. https://doi.org/10.5285/4b2910bd-19db-4a15-a003-88f61137d8ec

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