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
Elementa Science of the Anthropocene,
Год журнала:
2022,
Номер
10(1)
Опубликована: Янв. 1, 2022
With
the
Arctic
rapidly
changing,
needs
to
observe,
understand,
and
model
changes
are
essential.
To
support
these
needs,
an
annual
cycle
of
observations
atmospheric
properties,
processes,
interactions
were
made
while
drifting
with
sea
ice
across
central
during
Multidisciplinary
Observatory
for
Study
Climate
(MOSAiC)
expedition
from
October
2019
September
2020.
An
international
team
designed
implemented
comprehensive
program
document
characterize
all
aspects
system
in
unprecedented
detail,
using
a
variety
approaches,
multiple
scales.
These
measurements
coordinated
other
observational
teams
explore
cross-cutting
coupled
Ocean,
ice,
ecosystem
through
physical
biogeochemical
processes.
This
overview
outlines
breadth
complexity
research
program,
which
was
organized
into
4
subgroups:
state,
clouds
precipitation,
gases
aerosols,
energy
budgets.
Atmospheric
variability
over
revealed
important
influences
persistent
large-scale
winter
circulation
pattern,
leading
some
storms
pressure
winds
that
outside
interquartile
range
past
conditions
suggested
by
long-term
reanalysis.
Similarly,
MOSAiC
location
warmer
wetter
summer
than
reanalysis
climatology,
part
due
its
close
proximity
edge.
The
comprehensiveness
characterizing
analyzing
phenomena
is
demonstrated
via
case
study
examining
air
mass
transitions
vertical
evolution.
Overall,
successfully
met
objectives
most
measurement
date
conducted
ice.
obtained
data
will
broad
coupled-system
scientific
provide
foundation
advancing
multiscale
modeling
capabilities
Arctic.
Journal of Climate,
Год журнала:
2019,
Номер
32(14), С. 4235 - 4261
Опубликована: Апрель 12, 2019
Abstract
A
winter
Eurasian
cooling
trend
and
a
large
decline
of
sea
ice
concentration
(SIC)
in
the
Barents–Kara
Seas
(BKS)
are
striking
features
recent
climate
changes.
The
question
arises
as
to
what
extent
these
phenomena
related.
mechanism
is
presented
that
establishes
link
between
SIC
midlatitude
cold
extremes.
Such
potential
weather
linkages
mediated
by
whether
there
weak
north–south
gradient
background
tropospheric
vorticity
(PV).
strong
PV
gradient,
which
usually
occurs
North
Atlantic
Pacific
Ocean
midlatitudes,
acts
barrier
inhibits
atmospheric
blocking
southward
air
intrusion.
Conversely,
more
persistent
weakened
regions
over
Eurasia,
Greenland,
northwestern
America
because
energy
dispersion
intensified
nonlinearity.
small
climatological
gradients
mid-
high-latitude
Eurasia
have
become
weaker
decades
BKS
temperatures
show
positive
trends
due
loss,
this
has
led
Ural-region
blocking.
These
factors
contribute
increased
East
Asia.
It
found,
however,
years
when
Asian
extremes
can
even
occur
absence
negative
anomalies.
Thus,
magnitude
an
important
controller
Arctic–midlatitude
linkages,
but
it
plays
no
role
if
Ural
not
present.
“PV
barrier”
concept
presents
critical
insight
into
producing
hypothesized
set
up
such
other
locations.
Annals of the New York Academy of Sciences,
Год журнала:
2021,
Номер
1504(1), С. 167 - 186
Опубликована: Июль 27, 2021
Abstract
We
analyze
the
polar
sea
ice
distribution
and
global
level
pressure
(SLP)
baroclinicity
distributions
over
“satellite”
period
of
1979–2020.
In
Arctic,
there
are
statistically
significant
extent
(SIE)
decreases
in
all
calendar
months,
annual
mean
has
lost
2.22
million
km
2
four
decades.
The
Antarctic
SIE,
marked
contrast,
increased
up
to
2014,
then
commenced
a
remarkable
retreat
(the
decreased
by
2.03
3
years
2017),
subsequently
near
its
long‐term
average
value
2020.
shifts
seasonal‐mean
SLP
patterns
consistent
with
warming
planet.
At
synoptic
scale,
we
diagnose
changes
baroclinicity,
mechanism
which
cyclones,
fronts,
other
weather
systems
generated.
Through
novel
presentation,
give
an
overview
relative
roles
vertical
shear
static
stability
influencing
trends
baroclinicity.
both
Arctic
regions,
is
shown
have
each
season
(with
sole
exception
summer).
This
increase,
coupled
midlatitude
results
poleward
storm
tracks.
Current Climate Change Reports,
Год журнала:
2019,
Номер
5(4), С. 407 - 420
Опубликована: Ноя. 15, 2019
Abstract
Purpose
of
Review
This
review
brings
together
recent
research
on
the
structure,
characteristics,
dynamics,
and
impacts
extratropical
cyclones
in
future.
It
draws
using
idealized
models
complex
climate
simulations,
to
evaluate
what
is
known
unknown
about
these
future
changes.
Recent
Findings
There
are
interacting
processes
that
contribute
uncertainties
cyclone
changes,
e.g.,
changes
horizontal
vertical
structure
atmosphere
increasing
moisture
content
due
rising
temperatures.
Summary
While
precipitation
intensity
will
most
likely
increase,
along
with
associated
increased
latent
heating,
it
unclear
extent
for
which
particular
conditions
this
feedback
increase
cyclones.
Future
could
focus
bridging
gap
between
models,
as
well
better
understanding
regional
Communications Earth & Environment,
Год журнала:
2020,
Номер
1(1)
Опубликована: Дек. 10, 2020
Abstract
The
stratosphere,
the
layer
of
atmosphere
at
heights
between
10-50
km,
is
an
important
source
variability
for
weather
and
climate
Earth’s
surface
on
timescales
weeks
to
decades.
Since
stratospheric
circulation
evolves
more
slowly
than
that
troposphere
below,
it
can
contribute
predictability
surface.
Our
synthesis
studies
coupling
stratosphere
reveals
also
contributes
substantially
a
wide
range
climate-related
extreme
events.
These
events
include
cold
air
outbreaks
heat,
pollution,
wildfires,
wind
extremes,
storm
clusters,
as
well
changes
in
tropical
cyclones
sea
ice
cover,
they
have
devastating
consequences
human
health,
infrastructure,
ecosystems.
A
better
understanding
vertical
atmosphere,
along
with
improved
representation
numerical
models,
therefore
expected
help
predict
from
decades
terms
event
type,
magnitude,
frequency,
location,
timing.
With
stratosphere-troposphere
coupling,
may
be
possible
link
tropospheric
extremes
forcing,
which
will
crucial
emergency
planning
management.
Quarterly Journal of the Royal Meteorological Society,
Год журнала:
2019,
Номер
146(727), С. 762 - 779
Опубликована: Ноя. 19, 2019
Abstract
We
report
an
increase
in
winter
(DJF)
cyclone
densities
the
areas
around
Svalbard
and
northwestern
Barents
Sea
a
decrease
southeastern
during
1979–2016.
Despite
high
interannual
variability,
trends
are
significant
at
90%
confidence
level.
The
changes
appear
as
result
of
shift
into
more
meridional
storm
track
high‐latitude
North
Atlantic,
associated
with
positive
trend
Scandinavian
Pattern.
A
Brunt–Väisälä
frequency
east
Eady
Growth
Rate
north
indicate
increased
baroclinicity,
favouring
enhanced
activity
these
regions.
For
first
time,
we
apply
composite
analysis
to
explicitly
address
regional
consequences
wintertime
Atlantic.
find
tendency
toward
warmer
moist
atmospheric
state
over
Svalbard.
Journal of Climate,
Год журнала:
2021,
Номер
34(10), С. 3733 - 3749
Опубликована: Фев. 11, 2021
Abstract
For
the
last
few
decades
Northern
Hemisphere
midlatitudes
have
seen
an
increasing
number
of
temperature
extreme
events.
It
has
been
suggested
that
some
these
extremes
are
related
to
planetary
wave
activity.
In
this
study
we
identify
propagation
regions
at
300
hPa
using
ERA-Interim
dataset
from
1980
2017
and
link
them
in
densely
populated
Hemisphere.
Most
studies
used
background
flow
fields
monthly
or
seasonal
scale
investigate
propagation.
a
phenomenon
is
influenced
by
threshold
incidents
nonlinear
processes,
can
distort
net
Rossby
signal.
A
novel
aspect
our
investigation
lies
use
daily
data
allowing
it
be
diagnosed
for
limited
but
important
periods
across
wider
range
latitudes,
including
polar
region.
We
show
winter
associated
with
circulation
anomalies
both
Arctic
tropics,
while
relative
importance
areas
differs
according
specific
midlatitude
particular,
trains
connecting
tropical
Pacific
Atlantic
may
North
America
Siberia.
seas
markedly
Eurasian
regions.
Analysis
synoptic
suggests
pre-existing
local
play
key
role
development
those
extremes,
as
well
amplification
large-scale
trains.
also
demonstrate
warm
create
cold
outbreaks
Siberia
America.