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?
Data 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
| Date made available | 29 Mar 2021 |
|---|---|
| Publisher | NERC EDS UK Polar Data Centre |
| Date of data production | 1 Jan 2011 - 1 Jan 2051 |
| Geographical coverage | Smith Glacier, Pope Glacier, Kohler Glacier, Haynes Glacier Antarctica |
| Geospatial polygon | -76.4812, -110.3878, -73.05556, -113.2878 |
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