Geoscience Letters,
Journal Year:
2024,
Volume and Issue:
11(1)
Published: Feb. 25, 2024
Abstract
Victoria
mode
(VM),
the
second
dominant
of
North
Pacific
sea
surface
temperature
variability,
has
been
identified
as
one
important
factors
influencing
Indian
summer
monsoon
(ISM)
onset.
The
positive
phase
May
VM
delays
ISM
onset
by
both
tropical
and
extratropical
pathways.
Here,
we
found
a
significant
interdecadal
enhancement
their
relationship
since
early
1990s,
which
is
mainly
attributed
to
structure
changes
increased
variance
VM.
In
recent
decades,
shown
more
warm
SST
anomalies
in
central
Pacific,
drive
large-scale
divergent
circulation
effectively.
This
enhanced
leads
low-level
divergence
reduced
rainfall
Asian
region.
excites
equatorial
Rossby
wave
response
anomalous
easterly
winds
northern
Ocean,
delaying
Besides,
after
1992/1993
stimulates
stronger
train.
stationary
train
induces
cooling
northwest
India,
weakens
land-sea
thermal
contrast
delayed
finding
should
be
taken
into
account
improve
short-term
predictions
Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
51(3)
Published: Jan. 30, 2024
Abstract
The
Pacific–Japan
(PJ)
pattern
traditionally
refers
to
the
meridional
dipole
mode
of
rainfall
and
low‐level
circulation
over
tropical
western
North
Pacific
mid‐latitude
East
Asia.
However,
recent
studies
have
reported
that
PJ
can
also
affect
Indian
summer
monsoon
(ISM)
via
anomalous
Ocean.
We
summarize
currently
available
indices
re‐examine
linkage
between
ISM.
found
only
are
significantly
correlated
with
in
southern
India
two
containing
signals
Maritime
Continent.
Continent
stimulate
anomalies
Ocean,
thereby
strengthening
PJ–ISM
linkage.
When
associated
removed,
becomes
weak
insignificant.
should
be
chosen
carefully
when
studying
climatic
impacts
pattern.
Journal of Geophysical Research Atmospheres,
Journal Year:
2025,
Volume and Issue:
130(5)
Published: Feb. 28, 2025
Abstract
It
was
previously
revealed
that
winter
precipitation
in
East
Asia
is
linked
to
tropical
Sea
Surface
Temperature
(SST)
anomalies
the
Indian
and
Pacific
Oceans.
While
several
teleconnection
pathways
have
been
identified,
accurately
measuring
these
connections
determining
relative
contributions
of
SSTs
remains
a
challenge.
We
employed
novel
causal
inference
approach
quantify
effects
on
Asian
precipitation,
focusing
its
leading
mode
(denoted
as
Pr).
Using
PCMCI
method,
we
first
derived
graph
between
Pr
eastern/western
Ocean
EP,
WP,
IO
respectively).
Based
graph,
then
applied
quantitative
analysis
using
Wright's
path
method.
The
results
indicated
WP‐SST
had
most
substantial
impact
Pr,
with
1
Standard
Deviation
(SD)
increase
0.24
SD
decrease
at
1‐month
lag
0.17
2‐month
lag.
monsoon
winds
subtropical
jet
stream
are
identified
critical
mediators
this
effect.
Additionally,
EP‐SST
notable
positive
influence
warming
0.12
lag,
while
IO‐SST
exhibits
minor
essential
note
that,
traditional
regression
indicates
explained
largest
portion
variance
among
three
SSTs,
but
exerts
more
significant
role
driving
variations,
aligning
numerical
experiments.
Ocean-Land-Atmosphere Research,
Journal Year:
2023,
Volume and Issue:
3
Published: Jan. 30, 2023
Climate
change
in
the
South
China
Sea
and
its
surrounding
areas
(SCSSA),
which
include
Indo-Pacific
Oceans,
Southeast
Asia,
Tibetan
Plateau,
could
exert
profound
impacts
on
both
regional
global
climate
patterns.
This
study
examines
unique
characteristics
of
SCSSA
context
warming,
highlighting
rapid
warming
core
areas,
such
as
Oceans
Plateau.
The
has
led
to
increased
Asian
summer
monsoon
precipitation,
expanded
Hadley
circulation,
an
extended
influence
Madden–Julian
Oscillation,
marked
changes
tropical
cyclone
frequency
genesis
location
SCSSA.
These
Plateau
affect
not
only
downstream
climates
(East
North
America,
Antarctica,
America)
through
anomalous
Rossby
waves
but
also
upstream
regions
(North
Africa,
Europe,
Atlantic,
Middle
East)
by
modulating
atmospheric
overturning
circulations
wave
discusses
projected
under
various
future
scenarios,
indicating
that
effects
local
remote
weather
extremes
would
be
intensified.
Understanding
these
dynamics
is
crucial
for
mitigating
consequences
change.
Fundamental Research,
Journal Year:
2024,
Volume and Issue:
unknown
Published: March 1, 2024
The
East
Asian
monsoon
transitional
zone
(MTZ)
is
a
northeast-southwest
oriented
belt
between
the
wet
areas
and
northwestern
dry
of
China
with
fragile
ecology
high
climate
sensitivity.
in
MTZ
characterized
by
strong
instability
large
variability,
resulting
frequent
occurrence
extreme
weather
events.
A
number
studies
have
focused
on
dry-wet
characteristics
from
different
perspectives,
taking
into
account
increasing
problems
water
scarcity
ecological
risks.
This
study
reviews
multi-scale
variations,
underlying
mechanisms
future
projections
conditions
over
under
global
warming.
main
findings
last
few
decades
are
summarized
as
follows:
1)
interannual
variability
summer
precipitation
combined
impacts
oceanic
forcings
internal
atmospheric
teleconnection
patterns
at
mid-high
latitudes;
2)
an
interdecadal
decrease
amount
was
observed
late
1990s
due
to
Silk-Road
pattern-like
wave
train
triggered
Atlantic
Multidecadal
Oscillation-like
SST
warming
North
positive-to-negative
phase
shift
Pacific
Decadal
Oscillation
(PDO);
3)
pronounced
drying
trend
has
been
during
1951–2005,
which
mainly
attributed
human
activities
including
increased
aerosols,
land-use
changes,
thermal
forcing
Tibetan
Plateau,
PDO;
4)
projected
increase
considerable
uncertainties
Arctic
Polar-Eurasian
pattern.
review
attempts
provide
clear
systematic
picture
distinctive
changing
features
MTZ,
attract
interest
scientific
community
change
this
unique
"transition"
domain.
Water,
Journal Year:
2025,
Volume and Issue:
17(2), P. 219 - 219
Published: Jan. 15, 2025
Winter
precipitation
(P)
in
East
Asia
(EA)
is
characterized
by
a
wetter
south
and
drier
north.
Most
of
the
existing
research
has
concentrated
on
elucidating
mechanisms
winter
P
southern
EA,
with
relatively
less
attention
given
to
northern
(NEA).
Our
analysis
showed
that
correlation
coefficient
(c.c.)
average
anomaly
percentage
(PAP)
between
EA
NEA
0.24
for
period
1950–2023,
indicating
substantial
regional
difference.
An
empirical
orthogonal
function
(EOF)
was
conducted
PAP
NEA.
The
first
second
mode
(EOF1
EOF2)
account
45.5%
17.9%
total
variance,
respectively.
EOF1
region-wide
uniform
spatial
pattern
whereas
EOF2
exhibits
north–south
dipole
pattern.
Further
indicated
two
EOF
modes
are
related
distinct
atmospheric
circulation
external
forcings.
Specifically,
linked
wave
train
from
Central
Siberia
toward
Japan,
while
connected
an
similar
Western
Pacific
Variations
mid–high
latitude
sea
surface
temperatures,
ice,
snow
potential
factors
influencing
EOF1.
close
relationship
tropical
SST
anomalies.