Abstract Details
(2020) Noble Gas, Tritium, and CFC Tracers In a Perennial Firn Aquifer, Southeast Greenland
Solomon DK & Miller OL
https://doi.org/10.46427/gold2020.2424
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13e: Room 4, Thursday 25th June 08:03 - 08:06
D. Kip Solomon
View all 2 abstracts at Goldschmidt2020
View abstracts at 7 conferences in series
Olivia L. Miller
Olivia L. Miller
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Submitted by Rolf Kipfer on Wednesday 24th June 08:20
Dear Kip Thanks for sharing with us some new insights on water recharge in and under glaciers. Obviously, we have 'warm' conditions in the glacier, thus you are dealing with supra-glacial recharge. Atmospheric noble gas concentrations (e.g. excess air) were found to be good markers to trace recharge in glacier being driven by 'some kind of melt water.' Thus, did you also analyse the complete suite of atmospheric noble gases and if you did, can you shortly comment on that? Best regards - RoKi
Dear Kip Thanks for sharing with us some new insights on water recharge in and under glaciers. Obviously, we have 'warm' conditions in the glacier, thus you are dealing with supra-glacial recharge. Atmospheric noble gas concentrations (e.g. excess air) were found to be good markers to trace recharge in glacier being driven by 'some kind of melt water.' Thus, did you also analyse the complete suite of atmospheric noble gases and if you did, can you shortly comment on that? Best regards - RoKi
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