Environmental Research Letters,
Journal Year:
2017,
Volume and Issue:
12(9), P. 094006 - 094006
Published: Aug. 23, 2017
Typically
20–40
extreme
cyclone
events
(sometimes
called
'weather
bombs')
occur
in
the
Arctic
North
Atlantic
per
winter
season,
with
an
increasing
trend
of
6
events/decade
over
1979–2015,
according
to
hourly
station
data
from
Ny-Ålesund.
This
increased
frequency
cyclones
is
consistent
observed
significant
warming,
indicating
that
meridional
heat
and
moisture
transport
they
bring
a
factor
rising
temperatures
region.
The
dominated
by
positive
monthly
about
3–4
November–December,
due
mainly
persistence
events.
A
negative
January
opposes
this,
while
there
no
February.
We
relate
regional
patterns
anomalously
low
sea-ice
conditions
recent
years,
together
associated
large-scale
atmospheric
circulation
changes
such
as
'blockinglike'
(e.g.
Scandinavian
blocking
December
Ural
during
January–February).
Journal of Climate,
Journal Year:
2017,
Volume and Issue:
30(16), P. 6561 - 6577
Published: June 15, 2017
There
is
increasing
interest
in
understanding
the
regional
impacts
of
different
global
warming
targets.
However,
several
climate
depend
on
atmospheric
circulation,
whose
response
to
change
remains
substantially
uncertain
and
not
interpretable
a
probabilistic
sense
multimodel
ensemble
projections.
To
account
for
these
uncertainties,
novel
approach
where
analyzed
as
function
carbon
emissions
conditional
plausible
storylines
circulation
here
presented
applied
CMIP5
models’
future
The
are
determined
based
three
remote
drivers
circulation:
tropical
polar
amplification
changes
stratospheric
vortex
strength.
As
an
illustration
this
approach,
it
shown
that
severity
projected
wintertime
Mediterranean
precipitation
decline
central
European
windiness
increase
strongly
depends
storyline
change.
For
given
magnitude
warming,
highest
impact
aspects
found
high
strengthening
vortex.
difference
wind
responses
between
substantial
equivalent
contribution
from
degrees
warming.
Improving
driver
thus
needed
better
bound
sector.
value
represent
uncertainty
projections
inform
selection
models
studies
discussed.
Journal of Climate,
Journal Year:
2017,
Volume and Issue:
30(10), P. 3549 - 3568
Published: Jan. 18, 2017
Abstract
Part
I
of
this
study
examines
the
relationship
among
winter
cold
anomalies
over
Eurasia,
Ural
blocking
(UB),
and
background
conditions
associated
with
Arctic
warming
Barents
Kara
Seas
(BKS)
using
reanalysis
data.
It
is
found
that
intensity,
persistence,
occurrence
region
UB-related
Eurasian
depend
strongly
on
strength
vertical
shear
(VS)
mean
westerly
wind
(MWW)
mid–high-latitude
Eurasia
related
to
BKS
warming.
Observational
analysis
reveals
during
1951–2015
UB
days
are
64%
(54%)
more
frequent
weak
MWW
winters,
26.9
(28.4)
per
winter,
than
strong
winters.
During
or
VS
as
frequently
observed
2000–15,
persistent
large
seen
together
widespread
midlatitude
resulting
from
increased
quasi
stationarity
persistence
UB.
By
contrast,
when
1979–99,
anomaly
less
intense
confined
a
narrow
Europe
because
rapid
westward
movement
For
case,
relatively
persistent.
The
maintained
primarily
by
reduced
downward
infrared
radiation
(IR),
while
surface
heat
fluxes,
IR,
advection
all
contribute
Thus,
since
2000
weakens
meridional
temperature
gradient,
MWW,
VS,
which
increases
(rather
its
amplitude)
then
leads
events
further
enhances
Atmospheric chemistry and physics,
Journal Year:
2014,
Volume and Issue:
14(17), P. 9403 - 9450
Published: Sept. 10, 2014
Abstract.
The
Arctic
climate
system
includes
numerous
highly
interactive
small-scale
physical
processes
in
the
atmosphere,
sea
ice,
and
ocean.
During
since
International
Polar
Year
2007–2009,
significant
advances
have
been
made
understanding
these
processes.
Here,
recent
are
reviewed,
synthesized,
discussed.
In
atmospheric
physics,
primary
cloud
radiative
transfer,
mesoscale
cyclones,
coastal,
fjordic
as
well
boundary
layer
surface
fluxes.
ice
its
snow
cover,
of
albedo
relationships
with
properties,
internal
structure
heat
salt
transfer
formation
superimposed
dynamics
ice.
For
ocean,
related
to
exchange
at
ice–ocean
interface,
diapycnal
mixing,
double-diffusive
convection,
tidal
currents
diurnal
resonance.
Despite
this
progress,
some
still
not
sufficiently
understood:
include
wave–turbulence
interactions
atmosphere
mechanical
weakening
Many
other
reasonably
understood
stand-alone
but
challenge
is
understand
their
impacts
feedbacks
on
Uncertainty
parameterization
continues
be
among
greatest
challenges
facing
modelling,
particularly
high
latitudes.
Further
improvements
require
new
year-round
field
campaigns
closely
combined
satellite
remote
sensing
studies
numerical
model
experiments.
Environmental Research Letters,
Journal Year:
2017,
Volume and Issue:
12(9), P. 094006 - 094006
Published: Aug. 23, 2017
Typically
20–40
extreme
cyclone
events
(sometimes
called
'weather
bombs')
occur
in
the
Arctic
North
Atlantic
per
winter
season,
with
an
increasing
trend
of
6
events/decade
over
1979–2015,
according
to
hourly
station
data
from
Ny-Ålesund.
This
increased
frequency
cyclones
is
consistent
observed
significant
warming,
indicating
that
meridional
heat
and
moisture
transport
they
bring
a
factor
rising
temperatures
region.
The
dominated
by
positive
monthly
about
3–4
November–December,
due
mainly
persistence
events.
A
negative
January
opposes
this,
while
there
no
February.
We
relate
regional
patterns
anomalously
low
sea-ice
conditions
recent
years,
together
associated
large-scale
atmospheric
circulation
changes
such
as
'blockinglike'
(e.g.
Scandinavian
blocking
December
Ural
during
January–February).