1887

Abstract

Summary

Between 2009 and 2018, we applied the three-dimensional Surface Nuclear Magnetic Resonance method (3D-SNMR) to the monitoring of water accumulation in the Tête Rousse glacier in French Alps. 3D-SNMR data allow for non-invasive observations of water and ice dynamics following three drainages of the accumulated water (2010, 2011 and 2012). We detected two principal reservoir in respectively the downhill and uphill zones of the glacier. After each drainage, meltwater refilled the downhill reservoir but its volume reduced. In 2018, the downhill reservoir contained about 10% of the volume relative that measured in 2010. In 2018, the water volume in the uphill reservoir was about 26,000 m3. It makes about the half of the volume considered dangerous in 2009 when first detected in the downhill reservoir (50,000 m3). The total volume assessed for the entire glacier in 2018 was about 31,500 m3 against 24,800 m3 measured in 2014. The increase in the volumes of the uphill zone accompanies a change in the geometry of the downhill cavern.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.202320122
2023-09-03
2025-11-16
Loading full text...

Full text loading...

References

  1. Haeberli, W., Alean, J.C., Müller, P. and Funk, M. [1989] Assessing risks from glacier hazards in high mountain regions: some experiences in the Swiss Alps. Annals of Glaciology, 13, 96–102.
    [Google Scholar]
  2. Jansson, P., Hock, R. and Schneider, T. [2003] The concept of glacier storage: A review. Journal of Hydrology, 282, 116–129.
    [Google Scholar]
  3. Legchenko, A., Descloitres, M., Vincent, C., Guyard, H., Garambois, S., Chalikakis, K. and Ezerski, M.[2011] Three-dimensional magnetic resonance imaging for groundwater. New Journal of Physics, 13, 025022.
    [Google Scholar]
  4. Legchenko, A., Vincent, C., Baltassat, J.M., Girard, J.F., Thibert, E., Gagliardini, O., Descloitres, M., Gilbert, A., Garambois, S., Chevalier, A., and Guyard, H. [2014] Monitoring water accumulation in a glacier using magnetic resonance imaging. Cryosphere, 8, 155–166, Z014.
    [Google Scholar]
  5. LegchenkoA. [2013] Magnetic resonance imaging for groundwater. Wiley-ISTE, ISBN: 978-1-84821-568-9.
    [Google Scholar]
  6. Tikhonov, A. and Arsenin, V. [1977] Solution of ill-posed problems. John Wiley&Sons, Inc.
    [Google Scholar]
  7. Vallot, J. and Delebecque, A. [1892] Sur les causes de la catastrophe survenue à Saint-Gervais (Haute Savoie). Les Comptes Rendus de l’Académie des sciences, 115, 264–266.
    [Google Scholar]
  8. Vincent, C., Garambois, S., Thibert, E., Lefèbvre, E., Le Meur, E. and Six, D. [2010] Origin of the outburst flood from Tête Rousse glacier in 1892 (Mont-Blanc area, France). Journal of Glaciology, 56(195), 688–698.
    [Google Scholar]
  9. Vincent, C., Descloitres, M., Garambois, S., Legchenko, A., Guyard, H., Lefebvre, E. and Gilbert, A. [2012] Detection of a subglacial lake in Glacier de Tete Rousse (Mont Blanc area, France). Journal of Glaciology, 58(211), 866–878.
    [Google Scholar]
  10. Vincent, C., Thibert, E., Gagliardini, O., Legchenko, A., Gilbert, A., Garambois, S., Condom, T., Baltassat, J.M. and Girard, J. F. [2015] Mechanisms of subglacial cavity filling in Glacier de Tête Rousse, French Alps. Journal of glaciology, 61(228), 609–623.
    [Google Scholar]
/content/papers/10.3997/2214-4609.202320122
Loading
/content/papers/10.3997/2214-4609.202320122
Loading

Data & Media loading...

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error