The cryosphere,
Journal Year:
2020,
Volume and Issue:
14(12), P. 4279 - 4297
Published: Dec. 1, 2020
Abstract.
Northwestern
Alaska
has
been
highly
affected
by
changing
climatic
patterns
with
new
temperature
and
precipitation
maxima
over
the
recent
years.
In
particular,
Baldwin
northern
Seward
peninsulas
are
characterized
an
abundance
of
thermokarst
lakes
that
dynamic
prone
to
lake
drainage
like
many
other
regions
at
southern
margins
continuous
permafrost.
We
used
Sentinel-1
synthetic
aperture
radar
(SAR)
Planet
CubeSat
optical
remote
sensing
data
analyze
recently
observed
widespread
drainage.
then
synoptic
weather
data,
climate
model
outputs
ice
growth
simulations
potential
drivers
future
pathways
in
this
region.
Following
warmest
wettest
winter
on
record
2017/2018,
192
were
identified
as
having
completely
or
partially
drained
early
summer
2018,
which
exceeded
average
rate
a
factor
∼
10
doubled
rates
previous
extreme
years
2005
2006.
The
combination
abundant
rain-
snowfall
extremely
warm
mean
annual
air
temperatures
(MAATs),
close
0
∘C,
may
have
led
destabilization
permafrost
around
margins.
Rapid
snow
melt
high
amounts
excess
meltwater
further
promoted
rapid
lateral
breaching
shores
consequently
sudden
some
largest
study
region
likely
persisted
for
millennia.
hypothesize
will
accelerate
become
dominant
landscape
change
Recent
MAATs
already
within
range
predictions
University
Fairbanks'
Scenarios
Network
Arctic
Planning
(UAF
SNAP)
ensemble
scenario
RCP6.0
2100.
With
MAAT
2019
just
below
∘C
nearby
Kotzebue,
Alaska,
station,
aggradation
basins
less
after
drainage,
strongly
decreasing
freeze-locking
carbon
sequestered
sediments,
signifying
prominent
regime
shift
ice-rich
lowland
regions.
Frontiers in Earth Science,
Journal Year:
2021,
Volume and Issue:
9
Published: Oct. 28, 2021
Ice-rich
permafrost
in
the
circum-Arctic
and
sub-Arctic
(hereafter
pan-Arctic),
such
as
late
Pleistocene
Yedoma,
are
especially
prone
to
degradation
due
climate
change
or
human
activity.
When
Yedoma
deposits
thaw,
large
amounts
of
frozen
organic
matter
biogeochemically
relevant
elements
return
into
current
biogeochemical
cycles.
This
mobilization
has
local
global
implications:
increased
thaw
thermokarst
thermal
erosion
settings
enhances
greenhouse
gas
fluxes
from
regions.
In
addition,
this
ice-rich
ground
is
special
concern
for
infrastructure
stability
terrain
surface
settles
along
with
thawing.
Finally,
understanding
distribution
domain
area
provides
a
window
past
allows
reconstruction
Ice
Age
environmental
conditions
mammoth-steppe
landscapes.
Therefore,
detailed
assessment
pan-Arctic
coverage
importance
estimate
its
potential
contribution
permafrost-climate
feedbacks,
assess
vulnerabilities,
understand
dynamics.
Building
on
previous
mapping
efforts,
objective
paper
compile
first
digital
map
spatial
database
coverage.
we
1)
synthesized,
analyzed,
digitized
geological
stratigraphical
maps
allowing
identification
occurrence
at
all
available
scales,
2)
compiled
field
data
expert
knowledge
creating
confidence
classes.
We
used
GIS-techniques
vectorize
harmonize
site
information
based
knowledge.
included
range
attributes
areas
lithological
stratigraphic
source
assigned
three
different
levels
presence
(confirmed,
likely,
uncertain).
Using
buffer
20
km
around
mapped
occurrences,
derived
an
extent
domain.
Our
result
vector-based
that
covers
approximately
2,587,000
2
,
whereas
found
within
480,000
region.
35%
total
today
located
tundra
zone,
65%
taiga
zone.
With
mapping,
outlined
substantial
created
unique
dataset
including
estimates.
Remote Sensing of Environment,
Journal Year:
2021,
Volume and Issue:
268, P. 112752 - 112752
Published: Oct. 29, 2021
Permafrost
is
warming
globally
which
leads
to
widespread
permafrost
thaw.
Particularly
ice-rich
vulnerable
rapid
thaw
and
erosion,
impacting
whole
landscapes
ecosystems.
Retrogressive
slumps
(RTS)
are
abrupt
disturbances
that
expand
by
several
meters
each
year
lead
an
increased
soil
organic
carbon
release.
Local
Remote
Sensing
studies
identified
increasing
RTS
activity
in
the
last
two
decades
number
of
or
heightened
growth
rates.
However,
a
large-scale
assessment
across
diverse
regions
at
high
temporal
resolution
allowing
further
determine
dynamics
its
main
drivers
still
lacking.
In
this
study
we
apply
disturbance
detection
algorithm
LandTrendr
for
automated
mapping
dynamic
North
Siberia
(8.1
×
106km2).
We
adapted
parametrised
segmentation
incorporate
Landsat+Sentinel-2
mosaics,
conducted
spectral
filtering,
spatial
masking
binary
machine-learning
object
classification
output
separate
between
false
positives
(F1
score:
0.609).
Ground
truth
data
calibration
validation
workflow
was
collected
from
9
known
cluster
sites
using
very
high-resolution
RapidEye
PlanetScope
imagery.
Our
presents
first
their
2001–2019.
50,895
steady
increase
RTS-affected
area
2001
2019
Siberia,
with
more
2016
onward.
Overall
331%
compared
2000
(2000:
20,158
ha,
2001–2019:
66,699
ha).
Contrary
this,
5
focus
show
spatio-temporal
variability
annual
dynamics,
alternating
periods
decreased
development,
indicating
close
relationship
drivers.
The
majority
active
onward
only
small
proportion
initiated
during
period,
mainly
caused
enlarging
existing
not
new
RTS.
detected
suggests
advancing
underlines
importance
assessing
large-scales.
Obtaining
such
consistent
products
will
help
parametrise
regional
global
climate
change
models.
Water,
Journal Year:
2022,
Volume and Issue:
14(3), P. 372 - 372
Published: Jan. 26, 2022
Under
a
warming
climate,
permafrost
degradation
has
resulted
in
profound
hydrogeological
consequences.
Here,
we
mainly
review
240
recent
relevant
papers.
Permafrost
boosted
groundwater
storage
and
discharge
to
surface
runoffs
through
improving
hydraulic
connectivity
reactivation
of
flow
systems,
resulting
reduced
summer
peaks,
delayed
autumn
flattened
annual
hydrographs,
deepening
elongating
paths.
As
result
degradation,
lowlands
underlain
by
more
continuous,
colder,
thicker
are
getting
wetter
uplands
mountain
slopes,
drier.
However,
additional
contribution
melting
ground
ice
stream-flows
seems
limited
most
basins.
the
table
supra-permafrost
water
lowering;
subaerial
taliks
forming;
connecting
expanding;
thermokarst
activities
intensifying.
These
processes
may
profoundly
impact
on
ecosystem
structures
functions,
terrestrial
processes,
subsurface
coupled
engineered
infrastructures,
socioeconomic
development.
During
last
20
years,
substantial
rapid
progress
been
made
many
aspects
cryo-hydrogeology.
these
studies
still
inadequate
desired
spatiotemporal
resolutions,
multi-source
data
assimilation
integration,
as
well
cryo-hydrogeological
modeling,
particularly
over
rugged
terrains
ice-rich,
warm
(>−1
°C)
zones.
Future
research
should
be
prioritized
following
aspects.
First,
better
understand
concordant
changes
mechanisms,
trends
for
hydrometeorology,
geocryology,
hydrogeology,
ecohydrology
thin
regions.
Second,
aim
towards
revealing
physical
chemical
mechanisms
heat
transfer
moisture
migration
vadose
zone
expanding
taliks,
coupling
hydrothermal
dynamics
supra-,
intra-
sub-permafrost
waters,
that
water-resource
hydrochemical
biogeochemical
movements
solutes
pollutants
waters
induced
thawing
permafrost.
Third,
urgently
need
establish
improve
predictive
distributed
cryo-hydrogeology
models
with
optimized
parameterization.
In
addition,
also
emphasize
automatically,
intelligently,
systematically
monitoring,
predicting,
evaluating,
adapting
impacts
from
degrading
at
scales.
Systematic,
in-depth,
abilities
can
greatly
advance
cryo-hydrogeology,
cryo-ecohydrology
help
manage
water,
ecosystems,
land
resources
regions
an
adaptive
sustainable
manner.
Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: March 28, 2023
Industrial
contaminants
accumulated
in
Arctic
permafrost
regions
have
been
largely
neglected
existing
climate
impact
analyses.
Here
we
identify
about
4500
industrial
sites
where
potentially
hazardous
substances
are
actively
handled
or
stored
the
permafrost-dominated
of
Arctic.
Furthermore,
estimate
that
between
13,000
and
20,000
contaminated
related
to
these
sites.
Ongoing
warming
will
increase
risk
contamination
mobilization
toxic
since
1100
3500
5200
located
stable
start
thaw
before
end
this
century.
This
poses
a
serious
environmental
threat,
which
is
exacerbated
by
change
near
future.
To
avoid
future
hazards,
reliable
long-term
planning
strategies
for
needed
take
into
account
impacts
cimate
change.
Environmental Science Advances,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Jan. 1, 2025
Climate
change
leads
to
releases
of
persistent
organic
pollutants
and
chemicals
emerging
concern
as
glaciers
melt
permafrost
thaws.
Increased
human
activity
in
the
Arctic
may
enhance
local
emissions
potentially
problematic
chemicals.
Polar Geography,
Journal Year:
2019,
Volume and Issue:
42(4), P. 267 - 286
Published: Oct. 2, 2019
The
Arctic
is
experiencing
pronounced
climatic
and
environmental
changes.
These
changes
pose
a
risk
to
infrastructure,
impacting
the
accessibility
development
of
remote
locations
adding
additional
pressures
on
local
regional
budgets.
This
study
estimates
costs
fixed
infrastructure
affected
by
climate
change
impacts
in
region,
specifically
permafrost
thaw.
Geotechnical
models
are
forced
data
from
six
CMIP5
used
evaluate
geotechnical
characteristics
between
decades
2050–2059
2006–2015
under
RCP8.5
scenario.
Country-specific
estimate
value
affected.
results
show
27%
increase
lifecycle
replacement
across
circumpolar
regions.
In
addition,
more
than
14%
total
assets
at
damages
due
specific
stressors,
such
as
loss
bearing
capacity
thaw
subsidence
ground
ice
melt.
Regions
Northern
Canada
Western
Siberia
projected
be
particularly
may
require
annual
spending
excess
1%
GRP
support
existing
into
future.