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Articles | Volume 11, issue 1
Articles | Volume 11, issue 1
https://doi.org/10.5194/se-11-75-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-11-75-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 11, issue 1
Research article
 | 
17 Jan 2020
Research article |  | 17 Jan 2020

Characterisation of subglacial water using a constrained transdimensional Bayesian transient electromagnetic inversion

Siobhan F. Killingbeck, Adam D. Booth, Philip W. Livermore, C. Richard Bates, and Landis J. West

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Cited articles

Andersen, J. L. and Sollid, J. L.: Glacial chronology and glacial geomorphology in the marginal zones of the glaciers Midtdalsbreen and Nigardsbreen, south Norway, Norsk Geogr. Tidsskr., 25, 1–38, 1971. 
Archie, G. E.: Classification of carbonate reservoir rocks and petrophysical considerations, AAPG Bull., 36, 278–298, 1952. 
Auken, E., Jørgensen, F., and Sørensen, K. I.: Large-scale TEM investigation for groundwater, Explor. Geophys., 34, 188–194, 2003. 
Auken, E., Christiansen, A. V., Kirkegaard, C., Fiandaca, G., Schamper, C., Behroozmand, A. A., Binley, A., Nielsen, E., Effersø, F., Christensen, N. B., and Sørensen, K.: An overview of a highly versatile forward and stable inverse algorithm for airborne, ground-based and borehole electromagnetic and electric data, Explor. Geophys., 46, 223–235, 2015. 
Barnett, C. T.: Simple inversion of time-domain electromagnetic data, Geophysics, 49, 925–933, 1984. 
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This paper presents MuLTI-TEM, a Bayesian inversion tool for inverting TEM data with independent depth constraints to provide statistical properties and uncertainty analysis of the resistivity profile with depth. MuLTI-TEM is highly versatile, being compatible with most TEM survey designs, ground-based or airborne, along with the depth constraints being provided from any external source. Here, we present an application of MuLTI-TEM to characterise the subglacial water under a Norwegian glacier.
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