Abstract:
The dataset consists of 14 selected lines of radar data, collected from the Little Dome C region close to Concordia Station in East Antarctica. The data were collected in austral field seasons 2016-17, and 2017-18, from within the search region for the planned European project Beyond EPICA - Oldest Ice, an EU-funded 10-nation consortium project to drill an ice core that spans up to 1.5 million years of climate and atmospheric history. Radar lines were recorded using the BAS DELORES sledge-borne, over-snow, ice radar system and geolocated with a precise GPS system.
This data was generated within the project Beyond EPICA - Oldest Ice (BE-OI). The project has received funding from the European Union's Horizon 2020 research and innovation programme under grant agreement No. 730258 (BE-OI CSA). It has received funding from the Swiss State Secretariat for Education, Research and Innovation (SERI) under contract number 16.0144. It is further supported by national partners and funding agencies in Belgium, Denmark, France, Germany, Italy, Norway, Sweden, Switzerland, the Netherlands and the UK. Logistic support is mainly provided by AWI, BAS, ENEA and IPEV. Collection of this data also benefited from support by the joint French-Italian Concordia Programme, which established and runs the permanent station Concordia at Dome C. We particularly acknowledge those who collected the data in the field, and assisted with the processing: Robert Mulvaney, Massimo Frezzotti, Marie Cavitte, Ed King, Carlos Martin, Catherine Ritz, Julius Rix.
Keywords:
DELORES, EPICA, Little Dome C, oldest ice, radar
Mulvaney, R., King, E., Martin, C., Rix, J., Cavitte, M., Ritz, C., & Frezotti, M. (2022). Ice radar data from Little Dome C, Antarctica, 2016-2018 (Version 1.0) [Data set]. NERC EDS UK Polar Data Centre. https://doi.org/10.5285/3ea504d8-41c2-40dc-86dc-284c341badaa
| Access Constraints: | No restrictions apply. |
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| Use Constraints: | Data supplied under Open Government Licence v3.0 http://www.nationalarchives.gov.uk/doc/open-government-licence/version/3/. |
| Creation Date: | 2022-03-03 |
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| Dataset Progress: | Complete |
| Dataset Language: | English |
| ISO Topic Categories: |
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| Parameters: |
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| Personnel: | |
| Name | UK Polar Data Centre |
| Role(s) | Metadata Author |
| Organisation | British Antarctic Survey |
| Name | Robert Mulvaney |
| Role(s) | Investigator, Technical Contact |
| Organisation | British Antarctic Survey |
| Name | Edward King |
| Role(s) | Investigator |
| Organisation | British Antarctic Survey |
| Name | Carlos Martin |
| Role(s) | Investigator |
| Organisation | British Antarctic Survey |
| Name | Julius Rix |
| Role(s) | Investigator |
| Organisation | British Antarctic Survey |
| Name | Marie Cavitte |
| Role(s) | Investigator |
| Organisation | The University of Texas at Austin |
| Name | Catherine Ritz |
| Role(s) | Investigator |
| Organisation | University of Grenoble Alpes / CNRS |
| Name | Massimo Frezotti |
| Role(s) | Investigator |
| Organisation | Roma Tre University |
| Parent Dataset: | N/A |
| Reference: | Cavitte, M. G. P., Young, D. A., Mulvaney, R., Ritz, C., Greenbaum, J. S., Ng, G., Kempf, S. D., Quartini, E., Muldoon, G. R., Paden, J., Frezzotti, M., Roberts, J. L., Tozer, C. R., Schroeder, D. M., and Blankenship, D. D.: A detailed radiostratigraphic data set for the central East Antarctic Plateau spanning from the Holocene to the mid-Pleistocene, Earth Syst. Sci. Data, 13, 4759-4777, https://doi.org/10.5194/essd-13-4759-2021, 2021. | |
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| Quality: | Position data recorded by L1/L2 geodetic GPS, mounted along-track mid-way between the centres of the transmit and received dipole antennas. Rinex position data is recorded at 10 second intervals, and the Rinex files post-processed to account for satellite vehicle ephemeris, and atmospheric effects, using the Canadian Spatial Reference System - Precise Point Positioning available at Geodetic tools and data (nrcan.gc.ca). Note that the SEG-Y standard specifies that the Sample Interval in the Binary File Header should be expressed as microseconds for time data, and must be an integer. To overcome these limitations, the vertical sampling interval is expressed as 12000 picoseconds. |
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| Lineage: | The ground based DELORES (DEep LOoking Radio Echo Sounder), system transmits a broadband impulse signal through a 20 m dipole antenna and receives reflections from the ice sheet base and internal reflecting horizons via a second 20 m dipole antenna. Signal/noise ratio is improved by moving the radar system slowly along the survey line with a high pulse repetition frequency, and 1024x onboard pulse stacking. Scattering losses are avoided by directly coupling the dipole transmit and receive antennae to the surface, orientated along-track. The ground based nature of the survey allowed for very tight line spacing to be achieved (generally 250 m or 500 m between lines); however, the total area of Little Dome C coverage was limited compared to the earlier airborne surveys. | |
| Temporal Coverage: | |
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| Start Date | 2016-12-14 |
| End Date | 2017-01-07 |
| Start Date | 2017-11-17 |
| End Date | 2017-12-27 |
| Spatial Coverage: | |
| Latitude | |
| Southernmost | -75.417 |
| Northernmost | -75.267 |
| Longitude | |
| Westernmost | 122.167 |
| Easternmost | 122.717 |
| Altitude | |
| Min Altitude | 3224 m |
| Max Altitude | 3230 m |
| Depth | |
| Min Depth | 2525 m |
| Max Depth | 3250 m |
| Data Resolution: | |
| Latitude Resolution | N/A |
| Longitude Resolution | N/A |
| Horizontal Resolution Range | 1 meter - < 30 meters |
| Vertical Resolution | N/A |
| Vertical Resolution Range | 10 meters - < 30 meters |
| Temporal Resolution | N/A |
| Temporal Resolution Range | N/A |
| Location: | |
| Location | Antarctica |
| Detailed Location | Little Dome C region, centred approximately 35 km from Concordia Station |
| Sensor(s): |
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| Data Collection: | The DELORES radar system raw data events file processed to a format suitable for import to a seismic processing package (ReflexW, version 7.5, Sandmeier Geophysical Research, 2017). Positional data for each shot is interpolated from the processed L1/L2 GPS position data recorded mid-way between the transmit and receive antennas and taken to be the nadir position of the basal radar reflection. Several filters are applied, in the time and depth domains, to increase the signal/noise ratio of the internal reflecting horizons and bedrock return, including suppression of the direct air wave, bandpass filtering, a gain function to correct for spherical spreading loss and migration to collapse diffractions to their source points. The original sampling period of 4 ns is averaged to 12 ns (expressed as 12000 ps) in the post-processed data. Because the collection of ground-based radar data is dependent on the speed of the vehicle, which varies due to the terrain roughness during collection, the radar data are interpolated onto a 5 m regular horizontal spacing during the post-processing. |
| Distribution: | |
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| Distribution Media | Online Internet (HTTP) |
| Distribution Size | 300 MB |
| Distribution Format | N/A |
| Fees | N/A |
| Data Storage: | The dataset consists of: 14 SEG-Y files holding the post-processed radar data, one per radar line; a CSV table of the coordinates of the endpoints of the 14 lines; and a PNG map of the survey grid. |