EGU25-5645, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-5645
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Monday, 28 Apr, 10:45–12:30 (CEST), Display time Monday, 28 Apr, 08:30–12:30
 
Hall X5, X5.165
Equivalent source inversion to homogenise magnetic airborne surveys in Antarctica flown on irregular flight lines, line spacing, heights and decades.
Maximilian Lowe1,2, Wolfgang Szwillus1, Alan Aitken3, Mareen Lösing3, Lu Li3,4, Graeme Eagles5, and Jörg Ebbing1
Maximilian Lowe et al.
  • 1Kiel University, Institute of Geosciences, Kiel, Germany (max.lowe@ifg.uni-kiel.de)
  • 2NERC - British Antarctic Survey, Cambridge, United Kingdom.
  • 3University of Western Australia, School of Earth Sciences, Perth, Australia.
  • 4Commonwealth Scientific and Industrial Research Organisation, Perth, Australia.
  • 5Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany.

Magnetic data collection in Antarctica is commonly carried out using airborne platforms, which allow to cover large spatial areas. Airborne surveys in Antarctica have been conducted since the 1950s as part of international and collaborative efforts. A challenge in creating a homogenous magnetic data compilation for Antarctica arises from heterogeneity in data collection through the decades, for example from different flight lines spacing, different observation height and long time period between surveys. Traditional data processing is performed manually or semi-automated which is time consuming due to the factors described above.

Equivalent source technique is a powerful tool to automate the data processing to combine irregular airborne surveys on different observation heights and time periods. The magnetic field data from different airborne surveys can be represented by a set of equivalent sources that accurately reproduce the input data. The magnetic forward response of the equivalent sources can be calculated at any height making upward / downward continuation obsolete and allowing a uniform observation height between surveys. Furthermore, the magnetic field can be calculated on a regular grid, removing irregular flight lines from airborne data compilations. Combining the equivalent source method with despiking-, wavelet filtering-, IGRF/DGRF correction- and weighted distance base station correction routines allow a fully automated processing workflow to create a harmonised magnetic compilation containing irregular airborne surveys with decreased noise.

We present a test case in East Antarctica to highlight the potential of an automated processing workflow to harmonise magnetic airborne data without biases arising from manual processing. Here, we utilise ICECAP data (2009-2017) and RAE data (1956-1960) as well as the ADMAP data compilation grid as prior. The next step is to use ADMAP line data to create a fully automated homogeneous continent wide Antarctic magnetic data compilation under the SCAR ADMAP working group umbrella.

How to cite: Lowe, M., Szwillus, W., Aitken, A., Lösing, M., Li, L., Eagles, G., and Ebbing, J.: Equivalent source inversion to homogenise magnetic airborne surveys in Antarctica flown on irregular flight lines, line spacing, heights and decades., EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-5645, https://doi.org/10.5194/egusphere-egu25-5645, 2025.