@article{fdi:010065381, title = {{M}echanisms of subglacial cavity filling in {G}lacier de {T}ete {R}ousse, {F}rench {A}lps}, author = {{V}incent, {C}. and {T}hibert, {E}. and {G}agliardini, {O}. and {L}egchenko, {A}natoli and {G}ilbert, {A}. and {G}arambois, {S}. and {C}ondom, {T}homas and {B}altassat, {J}. {M}. and {G}irard, {J}. {F}.}, editor = {}, language = {{ENG}}, abstract = {{T}he deadliest outburst flood from an englacial cavity occurred on {G}lacier de {T}ete {R}ousse in the {M}ont {B}lanc area, {F}rench {A}lps, in 1892. {A} subglacial reservoir was discovered in the same glacier in 2010 and drained artificially in 2010, 2011 and 2012 to protect the 3000 inhabitants downstream. {T}he mechanism leading to the spontaneous refilling of the cavity following these pumping operations has been analyzed. {F}or this purpose, the subglacial water volume changes between 2010 and 2013 were reconstructed. {T}he size of the cavity following the pumping was found to have decreased from 53 500 m(3) in 2010 to 12 750 m(3) in 2013. {C}reep and the partial collapse of the cavity roof explain a large part of the volume loss. {A}nalysis of cavity filling showed a strong relationship between measured surface melting and the filling rate, with a time delay of 4-6 hours. {A} permanent input of 15 m(3) d(-1), not depending on surface melt, was also found. {T}he meltwater and rain from the surface is conveyed to bedrock through crevasses and probably through a permeable layer of rock debris at the glacier bed. {T}he drainage pathway permeability was estimated at 0.054 m s(-1) from water discharge measurements and dye-tracing experiments.}, keywords = {glacier hazards ; glaciological natural hazards ; jokulhlaups ({GLOF}s) ; subglacial lakes ; subglacial processes ; {FRANCE} ; {ALPES}}, booktitle = {}, journal = {{J}ournal of {G}laciology}, volume = {61}, numero = {228}, pages = {609--623}, ISSN = {0022-1430}, year = {2015}, DOI = {10.3189/2015{J}o{G}14{J}238}, URL = {https://www.documentation.ird.fr/hor/fdi:010065381}, }