Basal Melt Rate Beneath Pine Island Ice Shelf (2014)
The basal melt rate at a single location beneath Pine Island Ice Shelf was observed using an autonomous phase-sensitive radio echo-sounder (ApRES) during 2014. The ApRES was deployed approximately 10 km from the ice shelf front where the ice was 492 m thick and the ice shelf draft was approximately 422 m. The ApRES was deployed as part of the NERC Ice Sheet Stability Program (iStar).
Funding was provided by the NERC Ice Sheet Stability Research Program.
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- Date (Creation)
- 2018-10-09
- Date (Revision)
- 2018-10-09
- Date (Publication)
- 2018-10-09
- Date (released)
- 2018-10-09
- Edition
- 1.0
- Unique resource identifier
- https://doi.org/10.5285/0cf552a6-cd62-4da0-8289-8e4bab0a35a8
- Codespace
- doi
- Unique resource identifier
- GB/NERC/BAS/PDC/01106
- Codespace
- https://data.bas.ac.uk/
- Other citation details
- Please cite this item as: Lok, L., Nicholls, K., Brennan, P., & Davis, P. (2018). Basal Melt Rate Beneath Pine Island Ice Shelf (2014) (Version 1.0) [Data set]. Polar Data Centre, Natural Environment Research Council, UK Research & Innovation. https://doi.org/10.5285/0cf552a6-cd62-4da0-8289-8e4bab0a35a8
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- No credit.
- Status
- 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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- ApRES
- Melt rate
- Pine Island
- iStar
- Place
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- Pine Island Ice Shelf Antarctica
- GEMET - INSPIRE themes, version 1.0
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- Other constraints
- Open Government Licence v3.0
- Use constraints
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- Other constraints
- This data is governed by the NERC Data Policy: https://www.ukri.org/who-we-are/nerc/our-policies-and-standards/nerc-data-policy/
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- otherRestrictions Other restrictions
- Other constraints
- This data is governed by the NERC data policy and supplied under Open Government Licence v.3
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- No restrictions apply.
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- largerWorkCitation Larger work citation
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- crossReference Cross reference
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- Codespace
- doi
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- crossReference Cross reference
- Spatial representation type
- textTable Text, table
- Metadata language
- engEnglish
- Character set
- utf8 UTF8
- Topic category
-
- Climatology, meteorology, atmosphere
- Environment
- Begin date
- 2014-01-13
- End date
- 2014-11-30
- 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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- Statement
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Methodology:
The data was processed following Nicholls et al. (2015). Formally, the raw Lagrangian ice shelf thinning rate at two-hourly resolution was derived from the time-derivative of the distance between the ApRES antennas and the ice shelf base, and includes the basal melt rate signal as well as a component of ice-column vertical strain rate resulting from ice flow and snow compaction. To remove the component of ice-column vertical strain rate due to tidal variations, the raw thinning rate was low-pass filtered using a cut-off at 48 hours. At frequencies lower than this, variability in the strain rate component is small compared with the basal melt rate and varies on a much longer timescale than those of interest here.
Data collection:
Instrumentation: Autonomous phase-sensitive radio echo-sounder
Data quality:
The basal melt rate has an accuracy of ±0.2 m/yr and has been fully quality controlled. There are no missing values.
Resolution: Two hourly resolution with a 48-hour low pass filter applied.
- File identifier
- 0cf552a6-cd62-4da0-8289-8e4bab0a35a8 XML
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- engEnglish
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- utf8 UTF8
- Hierarchy level
- dataset Dataset
- Hierarchy level name
- dataset
- Date stamp
- 2018-10-09
- 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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