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@ARTICLE{Jouvet:454075,
author = {Jouvet, Guillaume and Röllin, Stefan and Sahli, Hans and
Corcho, José and Gnägi, Lars and Compagno, Loris and
Sidler, Dominik and Schwikowski, Margit and Bauder, Andreas
and Funk, Martin},
title = {{M}apping the age of ice of {G}auligletscher combining
surface radionuclide contamination and ice flow modeling},
journal = {The Cryosphere},
volume = {14},
number = {11},
issn = {1994-0424},
address = {Katlenburg-Lindau},
publisher = {Copernicus},
reportid = {PUBDB-2021-00406},
pages = {4233 - 4251},
year = {2020},
abstract = {In the 1950s and 1960s, specific radionuclides were
released into the atmosphere as a result of nuclear weapons
testing. This radioactive fallout left its signature on the
accumulated layers of glaciers worldwide, thus providing a
tracer for ice particles traveling within the gravitational
ice flow and being released into the ablation zone. For
surface ice dating purposes, we analyze here the activity of
$^{239}$Pu, $^{240}$Pu and $^{236}$U radionuclides derived
from more than 200 ice samples collected along five
flowlines at the surface of Gauligletscher, Switzerland. It
was found that contaminations appear band-wise along most of
the sampled lines, revealing a V-shaped profile consistent
with the ice flow field already observed. Similarities to
activities found in ice cores permit the isochronal lines at
the glacier from 1960 and 1963 to be identified. Hence this
information is used to fine-tune an ice flow/mass balance
model, and to accurately map the age of the entire glacier
ice. Our results indicate the strong potential for combining
radionuclide contamination and ice flow modeling in two
different ways. First, such tracers provide unique
information on the long-term ice motion of the entire
glacier (and not only at its surface), and on the long-term
mass balance, and therefore offer an extremely valuable data
tool for calibrating ice flows within a model. Second, the
dating of surface ice is highly relevant when conducting
“horizontal ice core sampling”, i.e., when taking
chronological samples of surface ice from the distant past,
without having to perform expensive and logistically complex
deep ice-core drilling. In conclusion, our results show that
an airplane which crash-landed on the Gauligletscher in 1946
will likely soon be released from the ice close to the place
where pieces have emerged in recent years, thus permitting
the prognosis given in an earlier model to be revised
considerably.},
cin = {MPSD / CFEL-MPT},
cid = {I:(DE-H253)MPSD-20120731 / I:(DE-H253)CFEL-MPT-20160915},
pnm = {899 - ohne Topic (POF3-899)},
pid = {G:(DE-HGF)POF3-899},
experiment = {EXP:(DE-MLZ)NOSPEC-20140101},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000596668500001},
doi = {10.5194/tc-14-4233-2020},
url = {https://bib-pubdb1.desy.de/record/454075},
}