Synchronous coupled ice-ocean model of Smith Glacier forced by warm climate
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?
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- Date (Creation)
- 2021-03-29
- Date (Revision)
- 2021-03-29
- Date (Publication)
- 2021-03-29
- Date (released)
- 2021-03-29
- Edition
- 1.0
- Unique resource identifier
- https://doi.org/10.5285/4b2910bd-19db-4a15-a003-88f61137d8ec
- Codespace
- doi
- Unique resource identifier
- GB/NERC/BAS/PDC/01480
- Codespace
- https://data.bas.ac.uk/
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- NE/M003590/1
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- Other citation details
- Please cite this item as: 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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- No credit.
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- completed Completed
https://www.bas.ac.uk/team/business-teams/information-services/uk-polar-data-centre/
- Maintenance and update frequency
- asNeeded As needed
- Maintenance note
- completed Completed
- Theme
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- Dotson ice shelf
- Smith glacier
- coupled modelling
- ice shelf
- ice stream
- Place
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- Smith Glacier, Pope Glacier, Kohler Glacier, Haynes Glacier Antarctica
- Dotson Ice Shelf, Crosson Ice Shelf Antarctica
- GEMET - INSPIRE themes, version 1.0
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- no limitations to public access
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- Open Government Licence v3.0
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- Data released under Open Government Licence V3.0:
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- Spatial representation type
- textTable Text, table
- Metadata language
- engEnglish
- Character set
- utf8 UTF8
- Topic category
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- Environment
- Oceans
- Begin date
- 2011-01-01
- End date
- 2051-01-01
- Supplemental Information
- It is recommended that careful attention be paid to the contents of any data, and that the author be contacted with any questions regarding appropriate use. If you find any errors or omissions, please report them to polardatacentre@bas.ac.uk.
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https://www.bas.ac.uk/team/business-teams/information-services/uk-polar-data-centre/
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- application/netcdf
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- application/netcdf
- Name
- application/netcdf
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- 8267812045
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- Statement
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Methodology:
The output was generated using the Massachusetts Institute of Technology general circulation model (www.MITgcm.org) version c67r, with changes as described in Goldberg et al (2018).
Boundary conditions were downscaled from Kimura et al. for the year 2007. Bathymetry and initial ice geometry from BedMachine v1 (https://nsidc.org/data/NSIDC-0756/versions/1), and ice velocities calibrated with MEaSUREs v2 (https://nsidc.org/data/NSIDC-0484/versions/2).
Methodology can be found in
Goldberg, D.N., Gourmelen, N., Kimura, S., Millan, R., and Snow, K. (2019). How accurately should we model ice shelf melt rates? Geophysical Research Letters, 46, 189-199. https://doi.org/10.1029/2018GL080383.
- File identifier
- 4b2910bd-19db-4a15-a003-88f61137d8ec XML
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- engEnglish
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- utf8 UTF8
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- dataset Dataset
- Hierarchy level name
- dataset
- Date stamp
- 2021-03-29
- Metadata standard name
- ISO 19115 Geographic Information - Metadata
- Metadata standard version
- ISO 19115:2003(E)
https://www.bas.ac.uk/team/business-teams/information-services/uk-polar-data-centre/
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