Climate Dynamics,
Год журнала:
2020,
Номер
54(9-10), С. 4399 - 4421
Опубликована: Май 1, 2020
Abstract
As
evidence
of
climate
change
strengthens,
knowledge
its
regional
implications
becomes
an
urgent
need
for
decision
making.
Current
understanding
precipitation
changes
is
substantially
limited
by
our
the
atmospheric
circulation
response
to
change,
which
a
high
degree
remains
uncertain.
This
uncertainty
reflected
in
wide
spread
projected
multimodel
ensembles,
cannot
be
directly
interpreted
probabilistic
sense.
The
can
instead
represented
studying
discrete
set
physically
plausible
storylines
changes.
By
mining
CMIP5
model
output,
here
we
take
this
broader
perspective
and
develop
Southern
Hemisphere
(SH)
midlatitude
changes,
conditioned
on
global-mean
warming,
based
responses
two
remote
drivers:
enhanced
warming
tropical
upper
troposphere
strengthening
stratospheric
polar
vortex.
For
three
continental
domains
SH,
analyse
under
each
storyline.
To
allow
comparison
with
previous
studies,
also
link
both
those
Annular
Mode.
Our
results
show
that
leads
westerly
winds,
whilst
delayed
breakdown
(for
DJF)
or
JJA)
vortex
poleward
shift
winds
storm
tracks.
However,
not
zonally
symmetric
South
America,
Africa,
Australia
New
Zealand
exhibit
quite
specific
dependencies
drivers,
are
well
Environmental Research Letters,
Год журнала:
2019,
Номер
15(2), С. 024022 - 024022
Опубликована: Дек. 18, 2019
Abstract
Heat
waves
in
the
Arctic
may
strongly
impact
environment
and
local
communities.
Recently
several
indices
have
been
proposed
for
monitoring
environmental
changes
Arctic,
but
heat
not
addressed.
By
applying
a
structured
approach
evaluating
occurrences
of
periods
with
exceptionally
high
temperatures,
this
study
demonstrates
that
last
decades
there
was
an
increase
wave
over
terrestrial
Arctic.
The
is
mainly
Canadian
Archipelago
Greenland
are
surrounded
by
ocean
undergoing
sea-ice
melting
trend,
while
Eurasian
shows
no
significant
change
occurrence.
Since
2002
probability
experiencing
has
similar
or
even
higher
than
middle
low
latitudes
already
started
to
increasingly
threaten
vegetation,
ecology,
human
health
economy.
Nature Communications,
Год журнала:
2021,
Номер
12(1)
Опубликована: Фев. 16, 2021
The
Antarctic
sea
ice
area
expanded
significantly
during
1979-2015.
This
is
at
odds
with
state-of-the-art
climate
models,
which
typically
simulate
a
receding
cover
in
response
to
increasing
greenhouse
forcing.
Here,
we
investigate
the
hypothesis
that
this
discrepancy
between
models
and
observations
occurs
due
simulation
biases
drift
velocity.
As
control
use
Community
Earth
System
Model
(CESM)
Large
Ensemble,
has
40
realizations
of
past
future
change
all
undergo
retreat
recent
decades.
We
modify
CESM
replace
simulated
velocity
field
satellite-derived
estimate
observed
motion,
3
change.
find
expands
these
realizations,
spatial
structure
expansion
bearing
resemblance
observations.
results
suggest
reason
failed
capture
velocity,
implying
an
improved
representation
motion
crucial
for
more
accurate
projections.
Geophysical Research Letters,
Год журнала:
2021,
Номер
48(17)
Опубликована: Авг. 27, 2021
Abstract
This
study
investigates
how
El
Niño‐Southern
Oscillation
(ENSO)
modulates
winter
cold
anomalies
over
central
Eurasia
(CE)
using
reanalysis
data
during
1950–2019.
It
is
found
that
ENSO
can
significantly
influence
air
temperature
CE
mainly
through
modulating
the
strength
and
location
of
cyclonic
anomaly
Ural
blocking
(UB)
or
long‐lived
UB
events.
A
strong
(weak)
on
southeastern
(eastern)
side
Mountains
tends
to
occur
midlatitude
(high‐latitude)
La
Niña
(El
Niño)
winters.
Such
anomalous
circulation
leads
a
CE,
especially
East
Asia,
due
enhanced
(weakened)
advection
toward
Niño).
The
UB‐related
in
(high
latitude)
shown
be
related
weakened
(enhanced)
eastward
extension
westerly
winds
Environmental Research Letters,
Год журнала:
2021,
Номер
16(6), С. 064059 - 064059
Опубликована: Май 17, 2021
Abstract
We
investigate
linear
trends
in
Antarctic
skin
temperatures
(temperatures
from
about
the
top
millimeter
of
surface)
over
four
seasons
using
ERA5
ensemble
mean
reanalysis
data.
During
1950–2020,
statistically
significant
warming
occurred
East
and
West
Antarctica
spring,
autumn
winter,
Peninsula
winter.
A
surface
energy
budget
analysis
revealed
that
increases
downward
longwave
radiation
related
to
air
temperature
total
column
integrated
cloud
had
a
key
role
warming.
There
were
negative
sea
level
pressure
around
periphery
throughout
year,
associated
circulation
contributed
warm
advection
middle
latitudes
Peninsula.
Over
interior
Antarctica,
increase
moisture
lower
enhanced
low-level
cover.
two-dimensional
parameter
diagram
showed
for
time
segments
longer
than
30
years
starting
before
1960
exhibited
winter
In
also
long
segments.
summer,
cooling
less
years.
For
all
studied
intervals,
when
positive
trends,
more
70%
vice
versa.
This
result
demonstrates
on
space
scales,
changes
with
variations
atmospheric
loading
play
dominant
controlling
temperatures.
npj Climate and Atmospheric Science,
Год журнала:
2022,
Номер
5(1)
Опубликована: Март 18, 2022
Abstract
Sea
ice
extent
(SIE)
in
the
Weddell
attained
exceptionally
low
levels
April
(1.97
million
km
2
)
and
May
(3.06
2019,
with
values
being
~22%
below
long-term
mean.
Using
in-situ,
satellite
atmospheric
reanalysis
data,
we
show
large
negative
SIE
anomalies
were
driven
by
passage
of
a
series
intense
explosive
polar
cyclones
(with
record
pressure),
also
known
as
‘bombs’,
which
had
rivers
on
their
eastern
flanks.
These
storms
led
to
poleward
propagation
record-high
swell
wind
waves
(~9.6
m),
resulting
southward
advection
(~50
km).
Thermodynamic
processes
played
part,
including
anomalous
heat
(>138
W
m
−2
moisture
(>300
kg
−1
s
fluxes
from
midlatitudes,
along
ocean
mixed-layer
warming
(>2
°C).
The
circulation
associated
an
amplified
wave
number
three
pattern
leading
enhanced
meridional
flow
between
midlatitudes
Antarctic.
Weather and Climate Dynamics,
Год журнала:
2022,
Номер
3(3), С. 777 - 809
Опубликована: Июль 21, 2022
Abstract.
Atmospheric
general
circulation
changes
from
March
1979
to
February
2022
are
examined
using
the
ERA5
reanalysis.
Maps
of
linear
trends
and
time
series
for
specific
areas
presented.
Attention
is
concentrated
on
monthly,
seasonal
annual
means,
but
shorter-timescale
variability
also
considered,
including
extremes.
Changes
in
near-tropopause
winds
main
focus,
related
temperature,
wind
other
variables
throughout
troposphere
discussed.
Middle-
upper-tropospheric
warming
larger
subtropics
outer
tropics
than
deep
tropics,
except
over
Pacific.
This
linked
with
a
strengthening
meridional
expansion
tropical
easterlies
that
has
received
little
previous
attention.
The
change
occurs
predominantly
first
half
period.
Warming
several
mid-latitude
subtropical
land
comes
close
matching
large
Arctic,
some
seasons
at
least.
Westerly
upper-level
weaken
Arctic
winter
strengthen
northern
middle
latitudes,
contrary
arguments
based
due
solely
amplified
warming.
jet-stream
region
eastern
North
Atlantic
western
Europe
shifts
southward.
Westerlies
band
stretching
south-eastwards
Pacific
southern
Australia,
as
well
polar-jet-stream
surrounds
Antarctica.
Extreme
increase
Atlantic.
Net
kinetic
energy
increases,
mostly
associated
sub-monthly
along
storm
tracks
Available
potential
less.
Geopotential
height
shows
distinct
pattern
stationary
long-wave
structures.
There
increases
surface
pressure
mid-latitudes
decreases
Ocean
offshore
Several
comparisons
made
between
JRA-55
reanalysis
observations
it
assimilated.
They
show
reassuring
agreement,
regional
differences
require
further
investigation.
Environmental Research Letters,
Год журнала:
2022,
Номер
17(3), С. 034030 - 034030
Опубликована: Янв. 13, 2022
Abstract
Arctic
warming
and
its
association
with
the
mid-latitudes
has
been
a
hot
topic
over
past
two
decades.
Although
many
studies
have
explored
these
issues,
it
is
not
clear
how
their
linkage
changed
time.
The
results
show
that
winter
low
tropospheric
temperatures
in
Asia
experienced
phases
Phase
I
(2007/2008–2012/2013)
was
characterized
by
warm
cold
Eurasia,
phase
II
Eurasia
(2013/2014–2018/2019).
A
strengthened
temperature
between
occurred
during
I,
followed
weakened
II.
Simulation
experiments
forced
observed
sea
ice
variability
largely
reproduce
patterns,
suggesting
loss
contributes
to
phasic
(or
low-frequency)
variations
atmosphere
makes
Arctic–Asia
fluctuate
weakening
of
post-2012/2013
associated
amplified
expanded
warming.
corresponding
anomalies
level
pressure
resembled
positive-phase
North
Atlantic
Oscillation
This
study
implies
Arctic—cold
Arctic—warm
patterns
would
alternately
happen
context
loss,
which
increases
difficulty
correctly
predicting
Asian
temperature.
Climate Dynamics,
Год журнала:
2022,
Номер
58(11-12), С. 3513 - 3526
Опубликована: Янв. 5, 2022
Abstract
Growing
evidence
indicates
that
the
atmospheric
and
oceanic
circulation
experiences
a
systematic
poleward
shift
in
warming
climate.
However,
complexity
of
climate
system,
including
coupling
between
ocean
atmosphere,
natural
variability
land-sea
distribution,
tends
to
obfuscate
causal
mechanism
underlying
shift.
Here,
using
an
idealised
coupled
aqua-planet
model,
we
explore
shifting
circulation,
by
isolating
contributing
factors
from
direct
CO
$$_2$$
2
forcing,
indirect
surface
warming,
wind-stress
feedback
dynamics.
We
find
that,
contrast
particular
enhanced
subtropical
plays
important
role
driving
This
emerges
background
Ekman
convergence
anomalous
heat
absence
dynamical
change.
It
expands
tropical
warm
water
zone,
causes
mid-latitude
temperature
gradient,
hence
forces
corresponding
associated
wind
pattern.
The
wind,
turn
drives
circulation.
Our
simulations,
despite
being
idealised,
capture
main
features
observed
changes,
for
example,
patterns
near-surface
sea
level
pressure,
storm
tracks,
precipitation
large-scale
implying
increase
greenhouse
gas
concentrations
not
only
raises
temperature,
but
can
also
systematically
zones
poleward.