Abstract.
Global
precipitation
change
in
response
to
climate
is
closely
related
surface
temperature,
the
forcing
agent,
and
atmospheric
dry
energy
budget,
but
regional
more
complex.
In
this
study,
we
use
experiments
from
Precipitation
Driver
Response
Model
Intercomparison
Project
(PDRMIP)
wherein
carbon
dioxide,
sulfate
aerosols,
black
aerosols
are
perturbed
study
global
contrast
with
over
India.
The
warming
dioxide
increases
both
globally
regionally,
whereas
cooling
aerosol
leads
a
reduction
cases.
however,
decrease
increase
of
mechanism
increased
heating
driving
stronger
monsoon
circulation
low-level
winds.
This
intensification
Indian
is,
somewhat
surprisingly,
for
emissions
than
when
limited
those
Asian
region.
Overall,
our
presents
heterogeneity
responses
at
levels
potential
underlying
physical
processes
under
variety
forcings
that
would
be
useful
designing
further
model
higher
spatial
resolution.
International Journal of Climatology,
Год журнала:
2025,
Номер
unknown
Опубликована: Апрель 23, 2025
ABSTRACT
The
largest
impact
of
future
climate
changes
on
societies
and
ecosystems
will
likely
come
from
precipitation
variability
change.
Using
the
ERA5
dataset,
this
global
study
examines
trends
using
many
parameters
across
five
main
components:
amount,
frequency,
type,
wet
dry
spells,
extremes.
Global
are
summarised
by
land
ocean
areas,
region,
then
zonally
averaged
to
identify
broader
patterns
interactions
that
may
not
be
apparent
in
local
regional
scale
studies,
especially
with
a
reanalysis
dataset.
We
find
dataset
was
able
reproduce
key
features
change:
near‐ubiquitous
increase
extreme
precipitation,
Arctic
transition
snowfall
rainfall
regime
mid‐to
high
latitudes,
contrasting
sign
change
amount
frequency
between
ocean.
Two
noteworthy
findings
(1)
spatial
intensification
around
warmest
locations
(equatorial
region)
is
matched
temporal
time
year
(summer
months)
northern
hemisphere,
(2)
Himalayas
show
altitudinal
stratification
phase
changes.
Finally,
consistent
other
we
synoptic
weather
types
influence
scaling
temperature
should
explored
research.
Additionally,
results
compared
those
GPCC,
GPCP,
MERRA‐2
datasets
evaluate
robustness
results.
Daily,
annual,
seasonal
means,
including
inter‐annual
estimates
align
strongly
three
validation
datasets;
however,
mixed
results,
minimal
moderate
agreement.
In
general,
GPCC
most
similar
ERA5.
Remote Sensing,
Год журнала:
2024,
Номер
16(8), С. 1381 - 1381
Опубликована: Апрель 13, 2024
This
study
addresses
the
imperative
to
comprehend
gravity
shifts
resulting
from
groundwater
storage
(GWS)
variations
in
Arabian
Peninsula.
Despite
critical
importance
of
water
resource
sustainability
and
its
relationship
with
gravity,
limited
research
emphasizes
need
for
expanded
exploration.
The
investigation
explores
impact
GWS
extraction
on
field,
utilizing
Gravity
Recovery
Climate
Experiment
(GRACE)
Global
Land
Data
Assimilation
System
(GLDAS)
data
addition
validation
using
WaterGAP
Hydrology
Model
(WGHM).
Spanning
April
2002
June
2023,
this
predicts
trends
over
next
decade
Seasonal
Autoregressive
Integrated
Moving
Average
(SARIMA)
model.
comprehensive
time-series
analysis
reveals
a
significant
GRACE-derived
trend
approximately
−4.90
±
0.32
mm/year
during
period.
has
notable
anomaly
(GA)
values,
as
observed
through
decomposition
analysis.
projected
indicates
depletion
rate
14.51
km3/year
decade.
correlation
between
GA
is
substantial
at
0.80,
while
rainfall
negligible
due
low
precipitation
rates.
Employing
multiple
linear
regression
explains
80.61%
variance
GWS,
precipitation,
evapotranspiration.
investigates
climate
change
factors—precipitation,
temperature,
evapotranspiration—providing
holistic
understanding
forces
shaping
variations.
Precipitation
evapotranspiration
exhibit
nearly
equal
limiting
replenishment
opportunities.
holds
significance
studying
extensive
withdrawal
Peninsula,
particularly
concerning
crust
mass
stability.
Atmospheric chemistry and physics,
Год журнала:
2023,
Номер
23(22), С. 14187 - 14218
Опубликована: Ноя. 15, 2023
Abstract.
Atmospheric
water
vapor
plays
a
crucial
role
in
the
global
energy
balance,
hydrological
cycle,
and
climate
system.
High-quality
consistent
data
from
different
sources
are
vital
for
weather
prediction
research.
This
study
assesses
consistency
between
Formosa
Satellite
Mission
3–Constellation
Observing
System
Meteorology,
Ionosphere,
Climate
(FORMOSAT-3/COSMIC)
radio
occultation
(RO)
European
Centre
Medium-Range
Weather
Forecasts
(ECMWF)
Reanalysis
Model
5
(ERA5)
datasets.
Comparisons
made
across
atmospheric
pressure
levels
(300,
500,
850
hPa)
2007
to
2018.
Generally,
two
datasets
show
good
spatial
temporal
agreement.
COSMIC's
retrieval
is
slightly
lower
than
ERA5's
at
500
hPa,
with
distinct
latitudinal
differences
hemispheres.
COSMIC
exhibits
increasing
trends
of
3.47
±
1.77
%
per
decade,
3.25
1.25
2.03
0.65
decade
300,
respectively.
Significant
regional
variability
trends,
encompassing
notable
decreasing
patterns,
observable
tropical
subtropical
regions.
At
strong
noted
equatorial
Pacific
Ocean
Laccadive
Sea,
while
evident
Indo-Pacific
region
Arabian
Sea.
Over
land,
substantial
hPa
observed
southern
United
States,
contrasting
Africa
Australia.
The
ERA5
primarily
negative
regions
hPa.
However,
estimated
significantly
higher
ones
derived
low-height
stratocumulus-cloud-rich
ocean
west
South
America.
These
trend
located
Intertropical
Convergence
Zone
(ITCZ)
area
frequent
occurrences
convection,
such
as
deep
clouds.
difference
characterizing
distribution
RO
cloud
may
cause
differences.
assessment
spatiotemporal
RO-derived
reanalysis
helps
ensure
quality
these
studies.
Geophysical Research Letters,
Год журнала:
2024,
Номер
51(6)
Опубликована: Март 18, 2024
Abstract
The
high
latitude
Southern
Hemisphere
(SH)
is
an
important
region
for
Earth's
climate.
Ocean
heat
content,
cryosphere
interactions,
Antarctic
bottom
water
development
and
the
cloud‐albedo
feedbacks
need
to
be
understood
form
a
complete
picture
of
climate
system.
However,
SH
one
most
under‐observed
regions
due
its
remoteness.
advent
satellites
reanalyses
have
improved
our
monitoring
this
region.
Some
previous
studies
observed
increase
in
precipitation
over
latitudes,
however
we
argue
that
some
trends
commonly
used
data
sets
may
artifacts.
We
use
regression
analysis
Annular
Mode
contrast
these
relationships
satellite
reanalysis
products,
evaluate
SH.
suggest
sensor
changes
lack
situ
available
calibration
responsible
unusual
patterns
especially
around
65°S.
Atmosphere,
Год журнала:
2024,
Номер
15(5), С. 535 - 535
Опубликована: Апрель 27, 2024
In
this
paper,
the
global
distribution
of
precipitation
for
2023,
in
terms
totals
and
regional
anomaly
patterns,
is
analyzed
using
information
from
new
Global
Precipitation
Climatology
Project
(GPCP)
V3.2
Monthly
product,
including
how
amounts
patterns
2023
fit
into
longer
record
1983–2023.
The
tropical
pattern
anomalies
dominated
by
effect
El
Nino
which
began
during
Northern
Hemisphere
spring,
after
three
plus
years
La
Nina
conditions.
transition
conditions
through
2022
shows
rapid
change
many
features
positive
to
negative
or
reverse.
Comparison
observed
trend
maps
with
climate
model
results
indicates
similarity
between
observations
forced
SSTs,
while
“free-running”
ensemble
only
a
broad
general
agreement
over
large
regions.
total
about
3%
range
span
data,
prominent
as
features,
showing
small
anomaly.
ITCZ
(Inter-Tropical
Convergence
Zone)
latitude
band,
0–10°
N,
sets
high
mean
rain
rate
steady
upward
decades,
probably
response
related
warming.
npj Climate and Atmospheric Science,
Год журнала:
2024,
Номер
7(1)
Опубликована: Ноя. 20, 2024
Climate
models
exhibit
errors
in
their
simulation
of
historical
trends
variables
including
sea
surface
temperature,
winds,
and
precipitation,
with
important
implications
for
regional
global
climate
projections.
Here,
we
show
that
the
same
trend
are
also
present
a
suite
initialised
seasonal
re-forecasts
years
1993–2016.
These
produced
by
operational
similar
to
Coupled
Model
Intercomparison
Project
(CMIP)-class
share
external
forcings
(e.g.
CO2/aerosols).
The
errors,
which
often
well-developed
at
very
short
lead
times,
represent
roughly
linear
change
model
mean
biases
over
1993–2016
re-forecast
record.
similarity
both
simulations
suggests
likewise
result
from
evolving
biases,
responding
changing
radiative
forcings,
instead
being
an
erroneous
long-term
response
forcing.
Therefore,
these
may
be
investigated
examining
short-lead
development
forecasts/re-forecasts,
suggest
should
made
all
CMIP
models.
Atmosphere,
Год журнала:
2023,
Номер
14(8), С. 1276 - 1276
Опубликована: Авг. 12, 2023
Extreme
precipitation
events
are
becoming
increasingly
frequent
and
intense
in
southeastern
Brazil,
leading
to
socio-economic
problems.
While
it
is
not
possible
control
these
events,
providing
accurate
weather
forecasts
can
help
society
be
better
prepared.
In
this
study,
we
assess
the
performance
of
Weather
Research
Forecasting
(WRF)
model
simulating
a
period
extreme
from
31
December
2021
2
January
2022
southern
region
Minas
Gerais
(SMG)
state
Brazil.
We
conducted
five
simulations
using
two
nested
grids:
12
km
grid
(coarse
resolution)
3
(high
resolution).
For
coarse
resolution,
tested
cumulus
convection
parameterization
schemes:
Kain–Fritsch,
Betts–Miller–Janjic,
Grell–Freitas,
Grell–Devenyi,
New
Tiedke.
evaluated
impact
on
driving
high-resolution
simulations.
To
simulations,
compared
them
with
satellite
estimates,
situ
measurements
thirteen
meteorological
stations,
other
variables
ERA5
reanalysis.
Based
results,
found
that
Grell–Freitas
scheme
has
spatial
pattern
intensity
for
studied
when
four
analyzed
schemes.
Water,
Год журнала:
2023,
Номер
15(20), С. 3675 - 3675
Опубликована: Окт. 20, 2023
The
Gravity
Recovery
and
Climate
Experiment
(GRACE)
provided
valuable
insights
into
variations
in
Groundwater
Storage
(GWS).
However,
the
sensitivity
of
utilizing
Global
Positioning
System
(GPS)
time
series
displacement
data
for
detecting
changes
GWS
remains
a
subject
ongoing
discussion.
In
order
to
estimate
spatiotemporal
GWS,
we
selected
vertical
from
65
GPS
stations
located
Main
Karoo
Aquifer
(MKA).
We
performed
total
water
storage
(TWS)
inversion
on
components;
after
that,
deducted
surface
components
based
Land
Data
Assimilation
(GLDAS)
January
2013
December
2021.
Additionally,
validation,
compared
our
estimates
with
GRACE-derived
observed
values
derived
WaterGAP
Hydrology
Model
(WGHM)
compartments.
discovered
that
TWS
trends
GRACE
exhibited
similar
behaviors
trend
overestimated
by
WGHM.
Our
findings
demonstrate
relatively
typical
behavior
between
first
second
principal
component
(PCs)
empirical
orthogonal
function
(EOF)
loadings
(or
spatial
patterns).
With
contribution
71.83%
GPS-derived
variability
68.92%
variability,
EOF-1
is
potent
factor.
For
Principal
Components
PC1
PC2,
PCs
have
correlation
coefficients
0.75
0.84,
respectively.
Finally,
higher
temporal
resolution,
can
perform
same
task
as
hydrological
applications.
addition,
add
important
information
assess
regional
change.