Abstract.
Rock
glaciers
play
a
vital
role
in
the
hydrological
functioning
of
many
alpine
catchments.
Here,
we
investigate
seasonal
and
daily
freeze-thaw
cycles
previously
undocumented
Canfinal
rock
glacier
(RG)
located
Val
d'Ursé
catchment
(Bernina
Range,
Switzerland)
RG's
influence
on
dynamics
hydrogeological
system.
We
combine
digital
image
correlation
techniques,
geochemical
isotopic
analyses,
time-series
analysis,
monitoring
to
understand
An
acceleration
RG
creep
since
1990
has
occurred,
with
most
active
regions
exhibiting
horizontal
velocities
~1
m/yr.
Distinct
signatures
springs
influenced
by
discharge
reflect
contrasting
temporally-variable
groundwater
mixing
ratios.
A
novel
application
frequency-domain
analysis
air
temperature
spring
electrical
conductivity
enables
quantitative
understanding
thaw
subsurface
flow
dynamics.
gradual
decrease
time-lag
between
maximum
EC
minimum,
caused
dilution
from
ice
melt,
is
observed
over
snow-free
period,
implying
progressively
shorter
residence
times.
Through
our
multi-method
approach,
develop
conceptual
models
for
RG-influenced
systems
time-scales.
Abstract.
In
the
Central
Eastern
Alps,
an
increasing
number
of
high-altitude
streams
display
high
concentrations
toxic
solutes
such
as
Al,
F-,
Mn,
and
Ni
that
may
strongly
exceed
drinking
water
limits.
Previous
studies
have
shown
these
elements
are
mobilized
from
rock
glaciers
occurring
at
origin
streams.
This
is
caused
by
weathering
pyrite
producing
sulfuric
acid
therefore
promoting
leaching
crystalline
host
rocks.
After
mobilization,
temporally
stored
enriched
in
glacier
ice.
Today,
climate-change-induced
accelerated
melting
thus
leads
to
a
quick
focused
export
summer
when
ice
melt
rates
high.
The
temporal
storage
opens
up
opportunity
use
strong
chemical
signal
track
dynamics
identify
governing
processes
controlling
melt.
To
test
this
assess
consequences
on
streamwater
quality,
here
we
present
two-year
dataset
(2021,
2022)
monitoring
high-alpine
stream
originating
intact
located
Switzerland.
includes
monthly
sampling
discharge
measurements
outlet,
well
continuous
tracking
geogenic
fluxes
using
pressure
conductivity
probe.
Our
revealed
annual
with
seasonal
variation,
whereby
were
highest
during
warm
months.
2021,
several
tons
each,
which
remarkable
given
area
covers
only
about
40’000
m2.
Interestingly,
2022
30
%
lower
despite
record-high
temperatures.
A
similar
difference
was
observed
for
recorded
two
years.
suggests
both
controlled
amount
snowmelt
precipitation
infiltrating
into
system.
dry
weather
low
likely
lead
compared
snow
height
above
average.
Nevertheless,
years
degradation
significantly
contributed
downhill
stream.
Based
aspects,
conceptual
models
accumulation
their
driven
mobilization
degradation.
Finally,
argue
solute
exported
promising
future
research
direction
obtaining
more
reliable
estimates
glaciers.
Permafrost and Periglacial Processes,
Год журнала:
2024,
Номер
35(3), С. 243 - 261
Опубликована: Июнь 28, 2024
ABSTRACT
Computer
modeling
of
sporadic
and
isolated
patches
mountain
permafrost
distribution
is
difficult
to
implement
without
overestimating
it.
The
main
challenge
determine
the
very
areas
where
criteria
for
maintenance
are
met.
This
paper
aims
in
Southern
Carpathians
(SC),
a
typical
marginal
periglacial
range.
For
this
purpose,
collection
883
bottom
temperature
late
winter
snow
cover
(BTS)
points
was
used
as
proxy
presence
or
absence
order
train
several
machine
learning
models.
performances
each
model
were
evaluated
with
AUC
varying
between
0.99
Maxent
0.74
K‐nearest
neighbors
most
models
(five)
exhibiting
values
0.82
0.86.
Other
tests
such
confusion
matrices,
sensitivity
analyses,
data
shuffling,
size
reduction
indicated
that
Maxent,
AdaBoost,
support
vector
offered
best
results
while
logistic
regression,
neural
network,
gradient
boosting
exhibited
rather
poor
distributions.
final
ensemble
median
total
area
19.2
km
2
occupying
1%–9%
alpine
studied
massifs.
NDVI
proved
crucial
prediction
because
it
allows
delimiting
debris
surfaces
probable.
Deforestation
can
lead
to
an
increase
in
the
availability
of
nutrients
soil
and,
turn,
have
impact
on
quality
water
receiving
bodies.
This
study
assesses
deforestation
by
evaluating
in-stream
concentrations
dissolved
organic
carbon
(DOC)
and
nitrate,
their
internal
relationship,
those
with
stream
discharge
Wüstebach
headwater
catchment
(Germany).
has
monitored
associated
environmental
parameters
for
over
a
decade
as
part
TERENO
initiative.
Additionally,
there
is
paired
undisturbed
forested
that
serves
reference
stream.
Our
approach
included
more
advanced
correlation
analysis,
namely
wavelet
assists
determining
changes
lag
time
between
variables
interest
different
scales.
found
after
deforestation,
was
immediate
DOC
concentrations,
followed
nitrate
~1
year
later.
Overall,
mean
concentration
increased,
decreased
across
post-deforestation.
Elevated
nutrient
levels
peaked
around
2
3
years
clear-cutting,
returned
pre-deforestation
~5
years.
The
had
no
influence
anti-correlation
nitrate.
However,
both
compounds
likely
altered
due
increased
result
deforestation.
Wavelet
coherence
analysis
revealed
“underlying”
changing
strengths
directions
main
correlations
DOC,
scales
resulting
from
severe
forest
management
interventions
(here
deforestation).
information
provides
new
valuable
insights
decision
making
into
such
interventions.
Abstract.
In
the
Central
Eastern
Alps,
an
increasing
number
of
high-altitude
streams
display
high
concentrations
toxic
solutes
such
as
Al,
F-,
Mn,
and
Ni
that
may
strongly
exceed
drinking
water
limits.
Previous
studies
have
shown
these
elements
are
mobilized
from
rock
glaciers
occurring
at
origin
streams.
This
is
caused
by
weathering
pyrite
producing
sulfuric
acid
therefore
promoting
leaching
crystalline
host
rocks.
After
mobilization,
temporally
stored
enriched
in
glacier
ice.
Today,
climate-change-induced
accelerated
melting
thus
leads
to
a
quick
focused
export
summer
when
ice
melt
rates
high.
The
temporal
storage
opens
up
opportunity
use
strong
chemical
signal
track
dynamics
identify
governing
processes
controlling
melt.
To
test
this
assess
consequences
on
streamwater
quality,
here
we
present
two-year
dataset
(2021,
2022)
monitoring
high-alpine
stream
originating
intact
located
Switzerland.
includes
monthly
sampling
discharge
measurements
outlet,
well
continuous
tracking
geogenic
fluxes
using
pressure
conductivity
probe.
Our
revealed
annual
with
seasonal
variation,
whereby
were
highest
during
warm
months.
2021,
several
tons
each,
which
remarkable
given
area
covers
only
about
40’000
m2.
Interestingly,
2022
30
%
lower
despite
record-high
temperatures.
A
similar
difference
was
observed
for
recorded
two
years.
suggests
both
controlled
amount
snowmelt
precipitation
infiltrating
into
system.
dry
weather
low
likely
lead
compared
snow
height
above
average.
Nevertheless,
years
degradation
significantly
contributed
downhill
stream.
Based
aspects,
conceptual
models
accumulation
their
driven
mobilization
degradation.
Finally,
argue
solute
exported
promising
future
research
direction
obtaining
more
reliable
estimates
glaciers.
Abstract.
In
the
Central
Eastern
Alps,
an
increasing
number
of
high-altitude
streams
display
high
concentrations
toxic
solutes
such
as
Al,
F-,
Mn,
and
Ni
that
may
strongly
exceed
drinking
water
limits.
Previous
studies
have
shown
these
elements
are
mobilized
from
rock
glaciers
occurring
at
origin
streams.
This
is
caused
by
weathering
pyrite
producing
sulfuric
acid
therefore
promoting
leaching
crystalline
host
rocks.
After
mobilization,
temporally
stored
enriched
in
glacier
ice.
Today,
climate-change-induced
accelerated
melting
thus
leads
to
a
quick
focused
export
summer
when
ice
melt
rates
high.
The
temporal
storage
opens
up
opportunity
use
strong
chemical
signal
track
dynamics
identify
governing
processes
controlling
melt.
To
test
this
assess
consequences
on
streamwater
quality,
here
we
present
two-year
dataset
(2021,
2022)
monitoring
high-alpine
stream
originating
intact
located
Switzerland.
includes
monthly
sampling
discharge
measurements
outlet,
well
continuous
tracking
geogenic
fluxes
using
pressure
conductivity
probe.
Our
revealed
annual
with
seasonal
variation,
whereby
were
highest
during
warm
months.
2021,
several
tons
each,
which
remarkable
given
area
covers
only
about
40’000
m2.
Interestingly,
2022
30
%
lower
despite
record-high
temperatures.
A
similar
difference
was
observed
for
recorded
two
years.
suggests
both
controlled
amount
snowmelt
precipitation
infiltrating
into
system.
dry
weather
low
likely
lead
compared
snow
height
above
average.
Nevertheless,
years
degradation
significantly
contributed
downhill
stream.
Based
aspects,
conceptual
models
accumulation
their
driven
mobilization
degradation.
Finally,
argue
solute
exported
promising
future
research
direction
obtaining
more
reliable
estimates
glaciers.
Abstract.
Rock
glaciers
play
a
vital
role
in
the
hydrological
functioning
of
many
alpine
catchments.
Here,
we
investigate
seasonal
and
daily
freeze-thaw
cycles
previously
undocumented
Canfinal
rock
glacier
(RG)
located
Val
d'Ursé
catchment
(Bernina
Range,
Switzerland)
RG's
influence
on
dynamics
hydrogeological
system.
We
combine
digital
image
correlation
techniques,
geochemical
isotopic
analyses,
time-series
analysis,
monitoring
to
understand
An
acceleration
RG
creep
since
1990
has
occurred,
with
most
active
regions
exhibiting
horizontal
velocities
~1
m/yr.
Distinct
signatures
springs
influenced
by
discharge
reflect
contrasting
temporally-variable
groundwater
mixing
ratios.
A
novel
application
frequency-domain
analysis
air
temperature
spring
electrical
conductivity
enables
quantitative
understanding
thaw
subsurface
flow
dynamics.
gradual
decrease
time-lag
between
maximum
EC
minimum,
caused
dilution
from
ice
melt,
is
observed
over
snow-free
period,
implying
progressively
shorter
residence
times.
Through
our
multi-method
approach,
develop
conceptual
models
for
RG-influenced
systems
time-scales.