Abstract:
An airborne radar survey was flown over the Institute and Moller ice streams in the Weddell Sea sector of West Antarctica in the austral summer of 2010/11 as part of the Institute-Moller Antarctic Funding Initiative (IMAFI) project (grant reference number: NE/G013071/1). This project was a NERC Antarctic Funding Initiative (AFI) collaborative project between the British Antarctic Survey and the Universities of Edinburgh, York, Aberdeen and Exeter with the aim to test the hypothesis that the Institute and Moller ice streams are underlain by weak marine sediments which control the flow of the overlying ice.
Operating from two static field camps close to the ice divide between the Institute and Moller ice streams and Patriot Hills, we collected ~25,000 km of airborne radio-echo sounding data across 28 survey lines. Our aircraft was equipped with dual-frequency carrier-phase GPS for navigation, radar altimeter for surface mapping, wing-tip magnetometers, a LaCoste and Romberg air-sea gravimeter, and an ice-sounding radar system (PASIN).
We present here the full radar dataset consisting of the deep-sounding chirp and shallow-sounding pulse-acquired data in their processed form, as well as the navigational information of each trace, the surface and bed elevation picks, ice thickness, and calculated absolute surface and bed elevations. This dataset comes primarily in the form of NetCDF and georeferenced SEGY files. To interactively engage with this newly-published dataset, we also created segmented quicklook PDF files of the radar data.
Keywords:
Antarctic, aerogeophysics, ice thickness, radar, surface elevation
Ross, N., Bingham, R., Ferraccioli, F., Jordan, T., Le Brocq, A., Rippin, D., & Siegert, M. (2021). Processed airborne radio-echo sounding data from the IMAFI survey covering the Institute and Moller ice streams and the Patriot Hills, West Antarctica (2010/2011) (Version 1.0) [Data set]. NERC EDS UK Polar Data Centre. https://doi.org/10.5285/f32b298b-7906-4360-9e34-16739af73bb7
| Access Constraints: | None |
|---|---|
| Use Constraints: | This data is covered by a UK Open Government Licence (http://www.nationalarchives.gov.uk/doc/open-government-licence/version/3/). Further by downloading this data the user acknowledges that they agree with the NERC data policy (http://www.nerc.ac.uk/research/sites/data/policy.asp), and the following conditions: 1. To cite the data in any publication as follows: Ross, N., Bingham, R., Ferraccioli, F., Jordan, T., Le Brocq, A., Rippin, D., & Siegert, M. (2021). Processed airborne radio-echo sounding data from the IMAFI survey covering the Institute and Moller ice streams and the Patriot Hills, West Antarctica (2010/2011) (Version 1.0) [Data set]. NERC EDS UK Polar Data Centre. https://doi.org/10.5285/F32B298B-7906-4360-9E34-16739AF73BB7 2. The user recognizes the limitations of data. Use of the data is at the users' own risk, and there is no warranty as to the quality or accuracy of any data, or the fitness of the data for your intended use. The data are not necessarily fully quality assured and cannot be expected to be free from measurement uncertainty, systematic biases, or errors of interpretation or analysis, and may include inaccuracies in error margins quoted with the data. |
| Creation Date: | 2021-07-16 |
|---|---|
| Dataset Progress: | Complete |
| Dataset Language: | English |
| ISO Topic Categories: |
|
| Parameters: |
|
| Personnel: | |
| Name | PDC BAS |
| Role(s) | Metadata Author |
| Organisation | British Antarctic Survey |
| Name | Dr Neil Ross |
| Role(s) | Investigator |
| Organisation | Newcastle University |
| Name | Mr Carl Robinson |
| Role(s) | Investigator |
| Organisation | British Antarctic Survey |
| Name | Dr Tom Jordan |
| Role(s) | Investigator |
| Organisation | British Antarctic Survey |
| Name | Dr David Rippin |
| Role(s) | Investigator |
| Organisation | University of York |
| Name | Dr Anne Le Brocq |
| Role(s) | Investigator |
| Organisation | University of Exeter |
| Name | Dr Hafeez Jeofry |
| Role(s) | Investigator |
| Organisation | Imperial College London |
| Name | Dr Fausto Ferraccioli |
| Role(s) | Investigator |
| Organisation | British Antarctic Survey |
| Name | Mr Hugh Corr |
| Role(s) | Investigator |
| Organisation | British Antarctic Survey |
| Name | Prof Robert Bingham |
| Role(s) | Investigator |
| Organisation | University of Edinburgh |
| Name | Prof Martin Siegert |
| Role(s) | Investigator |
| Organisation | Bristol Glaciology Centre, University of Bristol |
| Parent Dataset: | N/A |
| Reference: | Details of survey location and design can be found at: Ross, N., Bingham, R. G., Corr, H. F. J., Ferraccioli, F., Jordan, T. A., Le Brocq, A., Rippin, D. M., Young, D., Blankenship, D. D., and Siegert, M. J. (2012): Steep reverse bed slope at the grounding line of the Weddell Sea sector in West Antarctica, Nature Geoscience, 5, 393-396, 2012. doi: https://doi.org/10.1038/NGEO1468 Jordan, T.A., Ferraccioli, F., Ross, N., Corr, H.F.J., Leat, P.T., Bingham, R.C., Rippin, D.M., Le Brocq, A & Siegert, M.J. 2010. Inland extent of the Weddell Sea Rift imaged by new aerogeophysical data. Tectonophysics, 585, 137-160. https://doi.org/10.1016/j.tecto.2012.09.010 Jeofry, H., Ross, N., Corr, H.F., Li, J., Morlighem, M., Gogineni, P. and Siegert, M.J., 2018. A new bed elevation model for the Weddell Sea sector of the West Antarctic Ice Sheet. Earth System Science Data, 10(2), pp.711-725.doi: https://doi.org/10.5194/essd-10-711-2018 More information on the radar system and processing can be found at: Corr, H.F., Ferraccioli, F., Frearson, N., Jordan, T., Robinson, C., Armadillo, E., Caneva, G., Bozzo, E. and Tabacco, I., 2007. Airborne radio-echo sounding of the Wilkes Subglacial Basin, the Transantarctic Mountains and the Dome C region. Terra Antartica Reports, 13, pp.55-63. Heliere, F., Lin, C.-C., Corr, H., and Vaughan, D.: Radio echo sounding of Pine Island Glacier, West Antarctica: Aperture synthesis processing and analysis of feasibility from space, IEEE Transactions on Geoscience and Remote Sensing, 45, 2573-2582, 2007. doi: https://doi.org/10.1109/TGRS.2007.897433 |
|
|---|---|---|
| Quality: | - Line spacing: 7.5 km - Trace spacing (post-processed data): ~10 m - Vertical resolution: ~8.4 m - Radar centre frequency: 150 MHz - Radar bandwidth: 12 MHz - Radar Receiver vertical sampling frequency: 22 MHz - Absolute GPS positional accuracy: ~0.1 m (relative accuracy is one order of magnitude better). Banking angle was limited to 10 degrees during aircraft turns to avoid phase issues between GPS receiver and transmitter. Please note: - The surface and bed pick information (surface and bed elevation, ice thickness, etc.) can be found at: https://doi.org/10.5285/7946c497-72fc-41cb-a9b2-bf9980efe156. - The SEGY files for the SAR-processed chirp data can be found at: https://doi.org/10.5285/8a975b9e-f18c-4c51-9bdb-b00b82da52b8. However, note that the following issues were found with the DOI above: a) The 'IceSurfacePositioning' files suffered from duplicated and/or missing values throughout which required fixing by re-connecting the trace time between the surface files and the native GPS files. b) The X/Y values found in the 'SEGY' files were not geospatially accurate. c) Only SAR-chirp SEGY (DLRsar) files are provided, however the pulse-data and another version of the processed chirp (cHG) had not yet been released. The datasets found here have been considerably curated and improved, and thus can be considered the latest and full dataset. |
|
| Lineage: | ** Instrumentation and Processing: Radar data were collected using the bistatic PASIN radar echo sounding system mounted on the BAS Twin Otter aircraft "Bravo Lima" and operating with a centre frequency of 150 MHz and using two interleaved pulses: a 4-microseconds, 12 MHz bandwidth linear chirp (deep sounding) and a 0.1-microseconds unmodulated pulse (shallow sounding). Chirp compression was applied using a Blackman window to minimise sidelobe levels, resulting in a processing gain of 10 dB. For the SAR data, 2-D Synthetic Aperture Radar (SAR) processing based on the Omega-K algorithm was applied to the data to enhance both along-track resolution and echo signal noise (see Heliere et al., 2007). The coherent SAR-chirp data (cHG) was processed using an coherent averaging filter along a moving window of length 250. The incoherent SAR-chirp data (DLRsar) was processed using an incoherent averaging filter along a moving window of length 9. Both cHG and DLRsar chirp products are complimentary and are best suited to assess the bed and internals in deep ice conditions. The coherent pulse-data was processed using a coherent averaging filter along a moving window of length 33. This data is best used to assess the internal structure and bed in shallow ice conditions. The bed reflector was first automatically depicted on the chirp data using a semi-automatic picker in the PROMAX software package. All the picks were afterwards checked and corrected by hand if necessary. The picked travel time was then converted to depth using a radar wave speed of 168 m/microseconds and a constant firn correction of 10 m. Surface elevation is derived from radar altimeter for ground clearance < 750 m, and the PASIN system for higher altitudes. ** Coordinates and Positions: The coordinates provided in the NetCDF for the surface and bed elevation for each radar trace are in longitude and latitude (WGS84, EPSG: 4326). The navigation attributes for the radar data in the NetCDF are in projected X and Y coordinates (Polar Stereographic, EPSG: 3031), as follows: Latitude of natural origin: -71 Longitude of natural origin: 0 Scale factor at natural origin: 0.994 False easting: 0 False northing: 2082760.109 The coordinates in the SEGY data are also in projected X and Y coordinates (Polar Stereographic, EPSG: 3031), although note that these are in integer format due to the SEGY limitations (see section below). Positions are calculated for the phase centre of the aircraft antenna. All positions (Longitude, Latitude and Height) are referred to the WGS1984 ellipsoid. ** Dataset: Please note: Due to the unstable nature of SEGY-formatted data and its uncertain long-term future, as well as the issues documented below, we also provide the full radar data in NetCDF format. The dataset provided here consists of three parts: a NetCDF file per flightline, two SEGY files per flightline (two chirp and one pulse), and one quicklook PDF file per flightline. These are described in more details below. - NetCDF: The NetCDF files contain the two processed deep-sounding chirp (cHG and DLRsar) and shallow-sounding pulse-acquired data in their processed form, as well as the associated metadata, navigational information (in both EPSG: 3031 and WGS84 EPSG: 4326), and the associated radar-related information for each trace (e.g. surface/bed elevation and picks, ice thickness, aircraft altitude, range to surface, time of trace) which are provided as separate attributes in the NetCDF file. The navigational position of each trace comes from the surface files, and the processed GPS files when no surface information was provided or when duplicates were found in the surface file (see Quality section above). Note that for these, interpolation of the navigational data might have been required to match closely the Coordinated Universal Time (UTC) of each trace in the surface files. No data is shown as "-9999" throughout the files. Note: When the radar was flown over shallow-ice areas (< 200 m in ice thickness), we also provide an additional surface and bed elevation information (variables ending ''_thinIcelayerData' in the NetCDF file). These were picked using a pre-processed version of the pulse-acquisition mode (not provided here) and are more accurate in areas of thin ice. However, note that care should be taken when linking the attributes from the 'thinIcelayerData'' with the attributes in the rest of the NetCDF. This is due to the fact that the pulse and chirp data are acquired in an alternating mode and thus the longitude, latitude, time of trace and other variables are slightly different (offset) from the rest of the data found in the NetCDF. NetCDF attributes: - 'traces': Trace number for the radar data (x axis) - 'fast_time': Two-way travel time (y axis) (units: microseconds) - 'x_coordinates': Cartesian x-coordinates for the radar data (x axis) (units: meters in WGS84 EPSG:3031) - 'y_coordinates': Cartesian y-coordinates for the radar data (x axis) (units: meters in WGS84 EPSG:3031) - 'chirp_cHG_data'': Radar data for the processed (coherent) SAR-chirp (also known as cHG) (units: power in dBm) - 'chirp_DLRsar_data': Radar data for the processed (incoherent) SAR-chirp (also known as DLRsar) (units: power in dBm) - 'pulse_data': Radar data for the processed (coherent) pulse (units: power in dBm) - 'longitude_layerData': Longitudinal position of the trace number (units: degree_east in WGS84 EPSG:4326) - 'latitude_layerData': Latitudinal position of the trace number (units: degree_north in WGS84 EPSG:4326) - 'UTC_time_layerData': Coordinated Universal Time (UTC) of trace (also known as resTime) (units: seconds) - 'PriNumber_layerData': Incremental integer reference number related to initialisation of the radar system that permits processed SEGY data and picked surface and bed to be linked back to raw radar data (also known as PriNum) (units: arbitrary - integers) - 'terrainClearanceAircraft_layerData': Terrain clearance distance from platform to air interface with ice, sea or ground (also known as resHt) (units: meters) - 'aircraft_altitude_layerData': Aircraft altitude (also known as Eht) (units: meters relative to WGS84 ellipsoid) - 'surface_altitude_layerData': Ice surface elevation for the trace number from radar altimeter and LiDAR (units: meters relative to WGS84 ellipsoid) - 'surface_pick_layerData': Location down trace of surface pick (BAS system) (units: microseconds) - 'bed_altitude_layerData': Bedrock elevation for the trace number derived by subtracting ice thickness from surface elevation (units: meters relative to WGS84 ellipsoid) - 'bed_pick_layerData': Location down trace of bed pick (BAS system) (units: microseconds) - 'land_ice_thickness_layerData': Ice thickness for the trace number obtained by multiplying the two-way travel-time between the picked ice surface and ice sheet bed by 168 m/microseconds and applying a 10 meter correction for the firn layer (units: meters) When the radar was flown over shallow-ice areas (< 200 m in ice thickness; see above),the following variables are also provided in the NetCDF: - 'trace_number_thinIcelayerData': Pre-processed pulse radar trace number for thin ice areas (< 200 m ice thickness) - 'longitude_thinIcelayerData': Longitudinal position of the trace number (units: degree_east in WGS84 EPSG:4326) for thin ice areas (< 200 m ice thickness) - 'latitude_thinIcelayerData': Latitudinal position of the trace number (units: degree_north in WGS84 EPSG:4326) for thin ice areas (< 200 m ice thickness) - 'UTC_time_thinIcelayerData': Coordinated Universal Time (UTC) of trace (also known as resTime) for the pre-processed pulse data (units: seconds) for thin ice areas (< 200 m ice thickness) - 'PriNum_thinIcelayerData': Incremental integer reference number related to initialisation of the radar system that permits the pre-processed pulse SEGY data and picked surface and bed to be linked back to raw radar data (also known as PriNum) (units: arbitrary - integers) for thin ice areas (< 200 m ice thickness) - 'terrain_clearanceAircraft_thinIcelayerData': Terrain clearance distance from platform to air interface with ice, sea or ground (also known as resHt) (units: meters) for thin ice areas (< 200 m ice thickness) - 'aircraft_altitude_thinIcelayerData': Aircraft altitude (also known as Eht) (units: meters relative to WGS84 ellipsoid) for thin ice areas (< 200 m ice thickness) - 'surface_altitude_thinIcelayerData': Ice surface elevation for the trace number in the pre-processed pulse data from radar altimeter and LiDAR (units: meters relative to WGS84 ellipsoid) for thin ice areas (< 200 m ice thickness) - 'surface_pick_thinIcelayerData': Location down trace of surface pick (BAS system) for thin ice areas (< 200 m ice thickness) (units: microseconds) - 'bed_altitude_thinIcelayerData': Bedrock elevation for the trace number in the pre-processed pulse data derived by subtracting ice thickness from surface elevation (units: meters relative to WGS84 ellipsoid) for thin ice areas (< 200 m ice thickness) - 'bed_pick_thinIcelayerData': Location down trace of bed pick (BAS system) for thin ice areas (< 200 m ice thickness) (units: microseconds) - 'land_ice_thickness_thinIcelayerData': Ice thickness for the trace number in the pre-processed pulse data obtained by multiplying the two-way travel-time between the picked ice surface and ice sheet bed by 168 m/microseconds and applying a 10 meter correction for the firn layer (units: meters) for thin ice areas (< 200 m ice thickness) - SEGY: The SEGY files are provided for the two processed-chirp products (cHG and DLRsar) and for the pulse-acquired data and have been georeferenced using the navigational position of each trace from the surface files, and the processed GPS files when no surface information was provided in the surface files. Note that for these, interpolation of the navigational data might have been required to match closely the Coordinated Universal Time (UTC) of each trace in the surface files. SEGY header description: - byte number 1-4 and 5-8 (SEQWL and SEQWR): Trace number for each SEGY trace - byte number 9-12 (FFID): PriNumber for each SEGY trace - byte number 73-76 (SRCX): Cartesian x-coordinates for each SEGY trace (units: meters in WGS84 EPSG:3031) - byte number 77-80 (SRCY): Cartesian y-coordinates for each SEGY trace (units: meters in WGS84 EPSG:3031) - byte number 115-116 (NSMP): Number of samples for each SEGY trace - byte number 117-118 (SI): Sampling interval for each SEGY trace Note that the current version of the SEGY (Revision 1.0) does not yet allow to store double-precision floats in the "Source X/Y" trace headers and thus the X and Y positions for each trace are rounded to the nearest integer when exporting the data. This will affect the accurate position of each trace in the SEGY data, however the precise X and Y position of each trace can be obtained from the NetCDF files if necessary. When loading in the georeferenced SEGY files into seismic-interpretation software for data visualisation and analysis, the user might be warned that duplicate traces are found within the data and that this might cause "bad performance". This is caused by the rounding of the X and Y positions in the SEGY headers as explained above and should only affect the position of a relatively small amount of traces. - Quicklook: The quicklook PDF files were produced to allow for a quick visualisation of the radar data and the position of each flightline with regards to the rest of the survey flightlines. The radar image in the PDF is from the processed chirp radar data (DLRsar) and is split into 25-km segments for the IMAFI survey. These segments (and the radar images associated with them) are the same as those shown on the Polar Airborne Geophysics Data Portal. |
|
| Ownership: | The project is a UK NERC Antarctic Funding Initiative (AFI) collaborative project between BAS and the Universities of Edinburgh, York, Aberdeen and Exeter with grant reference number NE/G013071/1. This work was also partly funded by the British Antarctic Survey core program (Geology and Geophysics team), in support of the Natural Environment Research Council (NERC). | |
| Temporal Coverage: | |
|---|---|
| Start Date | 2010-12-20 |
| End Date | 2011-01-09 |
| Spatial Coverage: | |
| Latitude | |
| Southernmost | -84.11 |
| Northernmost | -75.3 |
| Longitude | |
| Westernmost | -108.9 |
| Easternmost | -58.7 |
| Altitude | |
| Min Altitude | N/A |
| Max Altitude | N/A |
| Depth | |
| Min Depth | N/A |
| Max Depth | N/A |
| Data Resolution: | |
| Latitude Resolution | N/A |
| Longitude Resolution | N/A |
| Horizontal Resolution Range | 30 meters - < 100 meters |
| Vertical Resolution | N/A |
| Vertical Resolution Range | 1 meter - < 10 meters |
| Temporal Resolution | N/A |
| Temporal Resolution Range | N/A |
| Location: | |
| Location | Antarctica |
| Detailed Location | Institute and Moller ice streams |
| Sensor(s): |
|
|---|---|
| Source(s): |
|
| Data Collection: | ** Instrument: Radar data were collected using the bistatic PASIN (Polarimetric radar Airborne Science Instrument) radar echo sounding system mounted on the BAS Twin Otter aircraft "Bravo Lima" and operating with a centre frequency of 150 MHz and using two interleaved pulses: a 4-microseconds, 12 MHz bandwidth linear chirp (deep sounding) and a 0.1-microseconds unmodulated pulse (shallow sounding). The Pulse Repetition Frequency was 15,635 Hz (pulse repetition interval: 64 microseconds). ** Antenna configuration: 8 folded dipole elements: 4 transmitters (port side) 4 receivers (starboard side) Antenna gain: 11 dBi (with 4 elements) Transmit power: 1 kW into each 4 antennae Maximum transmit duty cycle: 10% at full power (4 x 1 kW) ** Radar receiver configuration: Receiver vertical sampling frequency: 22 MHz (resulting in sampling interval of 45.4546 ns) Receiver coherent stacking: 25 Receiver digital filtering: -50 dBc at Nyquist (11 MHz) Effective PRF: 312.5 Hz (post-hardware stacking) Sustained data rate: 10.56 Mbytes/second |
| Distribution: | |
|---|---|
| Distribution Media | Online Internet (HTTP) |
| Distribution Size | 77 GB |
| Distribution Format | netCDF |
| Fees | N/A |
| Data Storage: | This dataset comprises of: - 65x NetCDF files (one per flightline) containing the two chirp (cHG and DLRsar) and the pulse (pL) radar data, the navigational data of each trace, as well as the surface and bed elevation/pick information, ice thickness data, aircraft altitude, etc. In areas of thin ice (< 200m), additional surface/bed elevation and surface/bed picks are also provided (see Lineage section) (Total size: 37GB). - 195x georeferenced SEGY files (3x per flightline): 65x for chirp cHG, 65x for chirp DLRsar, and 65x for pulse (pL). (Total size: 39GB). - 65x quicklook PDF files (one per flightline) containing the segmented radar profiles and a map of the segment for quick visualisation (Total size: 600 MB). |