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Processed line aerogravity data over the Thwaites Glacier region (2018/19 season)

Aerogravity data has an important role to play in constraining sub-surface geology under grounded ice and bathymetry beneath floating ice shelves. This dataset contains aerogravity collected by the British Antarctic Survey as part of the International Thwaites Glacier Collaboration (ITGC). Data were collected using both a traditional stabilised platform approach, and a more modern strapdown gravity system. Flights were flown at a constant altitude ~450 m above the ice surface where surface topography was flat. Gravity data is also recovered along draped sections by the strapdown system. In total 9872 km of data is presented, of this 6033 km was collected in the main survey area, while other data was collected on input and output transit flights. The aircraft used was the BAS twin otter VP-FBL equipped for aerogeophysical surveys. Data are available in ASCII file format (.xyz). Three databases are provided with aerogravity data: one with the Strapdown processing flow, a second with the LaCoste & Romberg processing flow, and a final simplified database with the optimal free air gravity anomalies from the strapdown system.

Simple

Date (Creation)
2019-09-24
Date (Revision)
2019-09-24
Date (Publication)
2019-09-24
Date (released)
2019-09-24
Edition

1.0

Unique resource identifier
https://doi.org/10.5285/b9b28a35-8620-4182-bf9c-638800b6679b
Codespace

doi

Unique resource identifier
GB/NERC/BAS/PDC/01241
Codespace

https://data.bas.ac.uk/

Other citation details

Please cite this item as: Jordan, T., Robinson, C., Porter, D., Locke, C., & Tinto, K. (2020). Processed line aerogravity data over the Thwaites Glacier region (2018/19 season) (Version 1.0) [Data set]. UK Polar Data Centre, Natural Environment Research Council, UK Research & Innovation. https://doi.org/10.5285/b9b28a35-8620-4182-bf9c-638800b6679b

Credit

No credit.

Status
Completed
Point of contact
Organisation name Individual name Electronic mail address Role
British Antarctic Survey Jordan, Tom Author
British Antarctic Survey

Robinson, Carl

Author

Lamont Doherty Earth Observatory

Porter, David Author

Lamont Doherty Earth Observatory

Locke, Caitlin Author

Lamont Doherty Earth Observatory

Tinto, Kirsty Author
NERC EDS UK Polar Data Centre

PDCServiceDesk@bas.ac.uk

Point of contact
Maintenance and update frequency
As needed
Maintenance note
Completed
Global Change Master Directory (GCMD) Science Keywords
  • EARTH SCIENCE > Cryosphere > Glaciers/Ice Sheets
  • EARTH SCIENCE > Solid Earth > Geodetics/Gravity
Theme
  • Antarctica

  • Crosson Ice Shelf

  • Dotson Ice Shelf

  • Geophysics

  • Gravity

  • ITGC

  • Strapdown

  • Thwaites Glacier

Place
  • Thwaites Glacier Antarctica

  • Dotson Ice Shelf Antarctica

  • Crosson Ice Sheld Antarctica

GEMET - INSPIRE themes, version 1.0

  • Elevation
  • Geology
Access constraints
Other restrictions
Other constraints
no limitations to public access
Access constraints
Other restrictions
Other constraints
no limitations
Use constraints
License
Other constraints
Open Government Licence v3.0
Use constraints
Other restrictions
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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Further by downloading this data the user acknowledges that they agree with the NERC data policy (), and the following conditions:





1. To cite the data in any publication as follows:



DATA REFERENCE



Jordan, T., Robinson, C., Porter, D., Locke, C., & Tinto, K. (2020). Processed line aerogravity data over the Thwaites Glacier region (2018/19 season) [Data set]. UK Polar Data Centre, Natural Environment Research Council, UK Research & Innovation. https://doi.org/10.5285/B9B28A35-8620-4182-BF9C-638800B6679B







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.

Unique resource identifier
doi
Codespace

doi

Association Type
Cross reference
Unique resource identifier
url
Codespace

url

Association Type
Cross reference
Unique resource identifier
url
Codespace

url

Association Type
dependency
Unique resource identifier
url
Codespace

url

Association Type
Cross reference
Spatial representation type
Text, table
Language
English
Character set
UTF8
Topic category
  • Geoscientific information
N
S
E
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Begin date
2019-01-29
End date
2019-02-07
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.

Title

European Petroleum Survey Group (EPSG) Geodetic Parameter Registry

Date (Publication)
2008-11-12
Cited responsible party
Organisation name Individual name Electronic mail address Role

European Petroleum Survey Group

EPSGadministrator@iogp.org

Publisher
Unique resource identifier
urn:ogc:def:crs:EPSG::3031
Version

6.18.3

Distributor

Distributor contact
Organisation name Individual name Electronic mail address Role
NERC EDS UK Polar Data Centre

PDCServiceDesk@bas.ac.uk

Distributor
Distributor format
Name Version
text/plain
application/pdf
Units of distribution

bytes

Transfer size
115343360
OnLine resource
Protocol Linkage Name

WWW:LINK-1.0-http--link

https://ramadda.data.bas.ac.uk/repository/entry/show?entryid=b9b28a35-8620-4182-bf9c-638800b6679b

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Units of distribution

bytes

Transfer size
115343360
OnLine resource
Protocol Linkage Name

WWW:LINK-1.0-http--link

https://ramadda.data.bas.ac.uk/repository/entry/show?entryid=b9b28a35-8620-4182-bf9c-638800b6679b

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Hierarchy level
Dataset
Statement

Methodology:

PROCESSING:



Gravity data during the ITGC survey were collected using both a strapdown (Jordan and Becker 2018) and traditional stabilised platform approach (Valliant 1992). The initial strapdown gravity signal was recovered from raw INS and GPS data using a Kalman filtering technique implemented in the TerraPos GPS processing software. Raw data were processed in a tightly coupled manner solving for gravity, position, and sensor orientation simultaneously. Ionospheric and clock errors were solved using Precise Point Positioning (PPP) technique with accurate satellite clock and orbit corrections used in the 'Final' ephemeris data downloaded more than a month after the survey was completed. The applied Kalman filter included a gravity smoothing filter assuming a 5km gravity correlation constant and 10 mGal permitted standard deviation. In order to minimise thermal effects on the QA2000 accelerometers, the IMU was warmed up from ambient temperatures inside an insulating enclosure for at least three hours before each flight. However, very significant thermal drift of >30 mGal across a flight remained apparent when comparing the data to an independent Operation IceBridge (OIB) dataset (Cochran and Bell 2010, updated 2018). A thermal correction (C) based on the sensor internal temperature (T) was calibrated by comparison with the existing regional OIB data. The thermal correction took the form of a polynomial:



C= -0.0174T^2 + 2.2619T + 5.8554



After thermal correction long wavelength residual errors (>~30 minutes/100 km) attributed to hysteresis in the thermal response of the gravity system were still apparent. These were corrected for by a combination of statistical levelling, and fitting the long wavelength residual errors to the gravity field revealed by the OIB dataset.



The stabilised platform gravity data was collected using a LaCoste & Romberg sensor (S83) mounted in a ZLS stabilised platform. Raw gravity data was collected at 1Hz. The GPS positional data processed using TerraPos, described above, was used to calculate standard gravimetric corrections for vertical acceleration, Eotvos effect, Latitude and elevation (free air). Sensor drift was low and stable, and was calculated based on a series of still reading taken before and after every survey flight. The final free air anomaly was filtered with two passes of a B-Spline filter with smoothness 1 and tension of 0.05. Before each pass of the B-Spline filter the data was manually edited to remove spikes and other data errors at the start of line segments.



All the processing has been carried using Geosoft Oasis Montaj software.





RESOLUTION:



The line spacing for the survey is variable between 5 km and 10 km. Line data is generally designed to interleave with existing OIB data. Along-track resolution of the strapdown data is ~5 km.





DATA FORMAT:



Data are provided in ASCII file format (.xyz).



Three databases are provided with aerogravity data: one with the Strapdown processing flow, a second with the L&R processing flow, and a final simplified database with the optimal free air gravity anomalies from the strapdown system.





The strapdown data set includes the following channels:



Name of the file : 'Thw_tera_pos_grav_share.XYZ'



Flight: Flight number



Date: GPS date (YYY/MM/DD)



Time: GPS time (HH:MM:SS.SSSS)



Lat_deg: Latitude (DD.DDDDDDD)



Lon_deg: Longitude (DD.DDDDDDD)



Hght_GRS80: Elevation on the GRS80 ellipsoid (m)



X: X coordinate m Polar stereographic true scale -71



Y: Y coordinate m Polar stereographic true scale -71



Heading: Heading (degrees from Geodetic N)



Roll: Role (degrees from local level Geodetic)



Pitch: Pitch (degrees from local level Geodetic)



FAA: Initial free air gravity anomaly (mGal)



ICEBRIDGE: Reference gravity values from grid of ICEBRIDGE gravity anomalies (mGal).



IMU__C_: Internal temperature of IMU (degrees C).



Synthetic_Dicebr...(29)

Data collection:

Data was collected using the BAS twin otter VP-FBL, equipped for aerogeophysical surveys. Strapdown gravity data were recorded using an iMAR RQH-4001 inertial measurement unit (IMU) owned by Lamont-Doherty Earth Observatory. This sensor package consists of three Honeywell QA2000 accelerometers (mounted in mutually perpendicular directions), and three ring laser gyroscopes. Coincident GPS data were recorded with a NovAtel receiver. The stabilised platform gravity data were collected using a LaCoste & Romberg sensor (S83) mounted in a ZLS stabilised platform.

Data quality:

The standard deviation of the strapdown gravity crossover errors after thermal correction and levelling to OIB data was 2.2 mGal, consistent with a Root Mean Square Error (RMSE) of 1.56 mGal. The Stabilised platform gravity system did not perform as well, and the data from this system is included here for completeness.

Metadata

File identifier
b9b28a35-8620-4182-bf9c-638800b6679b XML
Metadata language
English
Character set
UTF8
Hierarchy level
Dataset
Hierarchy level name

dataset

Date stamp
2019-09-24
Metadata standard name

ISO 19115 Geographic Information - Metadata

Metadata standard version

ISO 19115:2003(E)

Metadata author
Organisation name Individual name Electronic mail address Role
NERC EDS UK Polar Data Centre

polardatacentre@bas.ac.uk

Point of contact
 
 

Overviews

Spatial extent

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Keywords

Antarctica Crosson Ice Shelf Dotson Ice Shelf Geophysics Gravity ITGC Strapdown Thwaites Glacier
GEMET - INSPIRE themes, version 1.0

Elevation Geology
Global Change Master Directory (GCMD) Science Keywords

EARTH SCIENCE > Cryosphere > Glaciers/Ice Sheets EARTH SCIENCE > Solid Earth > Geodetics/Gravity


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