Nature Climate Change,
Journal Year:
2024,
Volume and Issue:
14(2), P. 156 - 162
Published: Jan. 10, 2024
Abstract
Ocean
eddies
play
a
critical
role
in
climate
and
marine
life.
In
the
rapidly
warming
Arctic,
little
is
known
about
how
ocean
eddy
activity
will
change
because
existing
models
cannot
resolve
Arctic
mesoscale
eddies.
Here,
by
employing
next-generation
global
sea
ice–ocean
model
with
kilometre-scale
horizontal
resolution
we
find
surge
of
kinetic
energy
upper
Ocean,
tripling
on
average
four-degree-warmer
world.
The
driving
mechanism
behind
this
an
increase
generation
due
to
enhanced
baroclinic
instability.
Despite
decline
ice,
killing
(a
process
which
are
dampened
ice
winds)
not
weaken
its
annual
mean
effect
considered
scenario.
Our
study
suggests
importance
adequately
representing
for
understanding
impacts
ecosystems.
Environmental Research Letters,
Journal Year:
2019,
Volume and Issue:
14(4), P. 045010 - 045010
Published: April 8, 2019
Key
observational
indicators
of
climate
change
in
the
Arctic,
most
spanning
a
47
year
period
(1971–2017)
demonstrate
fundamental
changes
among
nine
key
elements
Arctic
system.
We
find
that,
coherent
with
increasing
air
temperature,
there
is
an
intensification
hydrological
cycle,
evident
from
increases
humidity,
precipitation,
river
discharge,
glacier
equilibrium
line
altitude
and
land
ice
wastage.
Downward
trends
continue
sea
thickness
(and
extent)
spring
snow
cover
extent
duration,
while
near-surface
permafrost
continues
to
warm.
Several
exhibit
significant
statistical
correlation
temperature
or
reinforcing
notion
that
temperatures
precipitation
are
drivers
major
various
components
To
progress
beyond
presentation
physical
changes,
we
correspondence
between
biophysical
such
as
tundra
biomass
identify
numerous
disruptions
cascading
effects
throughout
trophic
levels.
These
include:
increased
delivery
organic
matter
nutrients
near‐coastal
zones;
condensed
flowering
pollination
plant
species
periods;
timing
mismatch
pollinators;
vulnerability
insect
disturbance;
shrub
biomass;
ignition
wildfires;
growing
season
CO2
uptake,
counterbalancing
shoulder
winter
emissions;
carbon
cycling,
regulated
by
local
hydrology
thaw;
conversion
terrestrial
aquatic
ecosystems;
shifting
animal
distribution
demographics.
The
system
now
clearly
trending
away
its
20th
Century
state
into
unprecedented
state,
implications
not
only
within
but
Arctic.
indicator
time
series
this
study
freely
downloadable
at
AMAP.no.
Geophysical Research Letters,
Journal Year:
2020,
Volume and Issue:
47(10)
Published: April 17, 2020
Abstract
We
examine
CMIP6
simulations
of
Arctic
sea‐ice
area
and
volume.
find
that
models
produce
a
wide
spread
mean
area,
capturing
the
observational
estimate
within
multimodel
ensemble
spread.
The
provides
more
realistic
sensitivity
September
to
given
amount
anthropogenic
CO
2
emissions
global
warming,
compared
with
earlier
CMIP
experiments.
Still,
most
fail
simulate
at
same
time
plausible
evolution
surface
temperature.
In
vast
majority
available
simulations,
Ocean
becomes
practically
free
(sea‐ice
<1
×
10
6
km
)
in
for
first
before
Year
2050
each
four
emission
scenarios
SSP1‐1.9,
SSP1‐2.6,
SSP2‐4.5,
SSP5‐8.5
examined
here.
The cryosphere,
Journal Year:
2019,
Volume and Issue:
13(1), P. 49 - 78
Published: Jan. 9, 2019
Abstract.
We
introduce
the
OSI-450,
SICCI-25km
and
SICCI-50km
climate
data
records
of
gridded
global
sea-ice
concentration.
These
three
are
derived
from
passive
microwave
satellite
offer
distinct
advantages
compared
to
existing
records:
first,
all
provide
quantitative
information
on
uncertainty
possibly
applied
filtering
at
every
grid
point
time
step.
Second,
they
based
dynamic
tie
points,
which
capture
evolution
surface
characteristics
ice
cover
accommodate
potential
calibration
differences
between
missions.
Third,
produced
in
context
sustained
services
offering
committed
extension,
documentation,
traceability,
user
support.
The
differ
underlying
(SMMR
&
SSM/I
SSMIS
or
AMSR-E
AMSR2),
imaging
frequency
channels
(37
GHz
either
6
19
GHz),
their
horizontal
resolution
(25
50
km),
period
cover.
algorithms
an
evaluation.
find
that
compare
well
with
independent
estimates
concentration
both
regions
very
high
low
hence
trust
these
will
prove
helpful
for
a
better
understanding
Earth's
Geophysical Research Letters,
Journal Year:
2020,
Volume and Issue:
47(9)
Published: April 23, 2020
Abstract
Both
the
Arctic
and
Antarctic
sea
ice
extents
(SIEs)
from
44
coupled
models
in
Coupled
Model
Intercomparison
Project
Phase
6
(CMIP6)
are
evaluated
by
comparing
them
with
observations
CMIP5
results.
The
CMIP6
multimodel
mean
can
adequately
reproduce
seasonal
cycles
of
both
SIE.
observed
September
SIE
declining
trend
(−0.82
±
0.18
million
km
2
per
decade)
between
1979
2014
is
slightly
underestimated
(−0.70
0.06
decade).
weak
but
significant
upward
not
captured,
which
was
an
issue
already
phase.
Compared
models,
have
lower
intermodel
spreads
values
trends,
although
their
biases
relatively
larger.
did
new
summer
tendencies
after
2000,
including
faster
decline
larger
interannual
variability
The cryosphere,
Journal Year:
2020,
Volume and Issue:
14(5), P. 1519 - 1536
Published: May 7, 2020
Abstract.
A
new
version
of
sea
ice
motion
and
age
products
includes
several
significant
upgrades
in
processing,
corrects
known
issues
with
the
previous
version,
updates
time
series
through
2018,
regular
planned
for
future.
First,
we
provide
a
history
these
NASA
distributed
at
National
Snow
Ice
Data
Center.
Then
discuss
improvements
to
algorithms,
validation
results
(Version
4)
older
versions,
intercompare
two.
While
Version
4
algorithm
changes
were
significant,
impact
on
is
relatively
minor,
particularly
more
recent
years.
The
reduce
biases
by
∼
0.01
0.02
cm
s−1
error
standard
deviations
0.3
s−1.
Overall,
speed
increased
over
3
0.5
2.0
most
series.
shows
higher
positive
trend
Arctic
0.21
per
decade
compared
0.13
3.
estimates
indicates
than
3,
especially
earlier
record,
but
similar
trends
toward
less
multiyear
ice.
Changes
derived
from
product
show
shift
cover,
pack
high
concentration
cover
dominated
first-year
ice,
which
susceptible
summer
melt.
We
also
observe
an
increase
≥
30
years,
has
been
shown
other
studies
anticipated
annual
decrease
extent.
Remote Sensing,
Journal Year:
2018,
Volume and Issue:
10(12), P. 2038 - 2038
Published: Dec. 14, 2018
In
this
paper,
we
review
the
use
of
satellite-based
remote
sensing
in
combination
with
situ
data
to
inform
Earth
surface
modelling.
This
involves
verification
and
optimization
methods
that
can
handle
both
random
systematic
errors
result
effective
model
improvement
for
monitoring
prediction
applications.
The
reasons
diverse
products
include
(i)
their
complementary
areal
temporal
coverage,
(ii)
covariant
information
content,
(iii)
ability
complement
observations,
which
are
often
sparse
only
locally
representative.
To
improve
our
understanding
complex
behavior
system
at
sub-surface,
need
large
volumes
from
high-resolution
modelling
sensing,
since
exhibits
a
high
degree
heterogeneity
discontinuities
space
time.
spatial
variability
biosphere,
hydrosphere,
cryosphere
anthroposphere
calls
an
increased
observation
(EO)
attaining
previously
considered
prohibitive.
We
availability
discuss
recent
examples
where
satellite
is
used
infer
observable
quantities
directly
or
indirectly,
particular
emphasis
on
key
parameters
necessary
weather
climate
prediction.
Coordinated
remote-sensing
modelling/assimilation
capabilities
required
support
international
application-focused
effort.