Climate Dynamics,
Journal Year:
2023,
Volume and Issue:
62(2), P. 1077 - 1106
Published: Sept. 27, 2023
Abstract
This
study
assesses
the
ability
of
climate
models
to
represent
rainy
season
(RS)
dependent
indices
relevant
for
agriculture
and
crop-specific
agricultural
in
eleven
African
subregions.
For
this,
we
analyze
model
ensembles
build
from
Regional
Climate
Models
(RCMs)
CORDEX-CORE
(RCM_hist)
their
respective
driving
General
Circulation
(GCMs)
CMIP5
(GCM_hist).
Those
are
compared
with
gridded
reference
data
including
reanalyses
at
high
spatio-temporal
resolution
(≤
0.25°,
daily)
over
climatological
period
1981–2010.
Furthermore,
ensemble
RCM-evaluation
runs
forced
by
ERA-Interim
(RCM_eval)
is
considered.
Beside
precipitation
like
sum
or
number
days
annually
during
RS,
examine
three
(crop
water
need
(CWN),
irrigation
requirement,
availability),
depending
on
RS’
onset.
The
agricultural-relevant
as
simulated
models,
CORDEX-CORE,
assessed
first
time
several
All
simulate
general
characteristics
well.
However,
performance
strongly
depends
subregion.
We
show
that
can
RS
subregions
one
adequately
yet
struggle
reproducing
two
RSs.
Precipitation
based
also
variable
errors
among
representation
CWN
affected
family
(GCM,
RCM)
forcing
ERA-Interim).
Nevertheless,
too
coarse
GCMs
hinders
such
specific
they
not
able
consider
land
surface
features
related
processes
smaller
scale.
Additionally,
daily
scale
usage
complex
variables
(e.g.,
latent
heat
flux
CWN)
preconditions
RS-onset
its
spatial
representation)
add
uncertainty
index
calculation.
Mostly,
RCMs
a
higher
skill
representing
value
models.
Sustainable Cities and Society,
Journal Year:
2023,
Volume and Issue:
101, P. 105072 - 105072
Published: Nov. 21, 2023
This
study
examines
the
effect
of
land
cover,
vegetation
health,
climatic
forcings,
elevation
heat
loads,
and
terrain
characteristics
(LVCET)
on
surface
temperature
(LST)
distribution
in
West
Africa
(WA).
We
employ
fourteen
machine-learning
models,
which
preserve
nonlinear
relationships,
to
downscale
LST
other
predictands
while
preserving
geographical
variability
WA.
Our
results
showed
that
random
forest
model
performs
best
downscaling
predictands.
is
important
for
sub-region
since
it
has
limited
access
mainframes
power
multiplex
algorithms.
In
contrast
northern
regions,
southern
regions
consistently
exhibit
healthy
vegetation.
Also,
areas
with
unhealthy
coincide
hot
clusters.
The
positive
Normalized
Difference
Vegetation
Index
(NDVI)
trends
Sahel
underscore
rainfall
recovery
subsequent
Sahelian
greening.
southwesterly
winds
cause
upwelling
cold
waters,
lowering
WA
highlighting
cooling
influence
water
bodies
LST.
Identifying
elevated
paramount
prioritizing
greening
initiatives,
our
underscores
importance
considering
LVCET
factors
urban
planning.
Topographic
slope-facing
angles,
diurnal
anisotropic
all
contribute
variations
LST,
emphasizing
need
a
holistic
approach
when
designing
resilient
sustainable
landscapes.
Scientific Data,
Journal Year:
2023,
Volume and Issue:
10(1)
Published: Sept. 28, 2023
Regional
climate
models
can
be
used
to
examine
how
past
weather
events
might
unfold
under
different
conditions
by
simulating
analogue
versions
of
those
with
modified
thermodynamic
(i.e.,
warming
signals).
Here,
we
apply
this
approach
dynamically
downscaling
a
40-year
sequence
from
1980-2019
driven
atmospheric
re-analysis,
and
then
repeating
total
8
times
using
range
time-evolving
signals
that
follow
4
80-year
future
trajectories
2020-2099.
Warming
two
emission
scenarios
(SSP585
SSP245)
are
derived
groups
global
based
on
whether
they
exhibit
relatively
high
or
low
sensitivity.
The
resulting
dataset,
which
contains
25
hourly
over
200
3-hourly
variables
at
12
km
spatial
resolution,
plausible
in
direct
reference
previously
observed
enables
systematic
exploration
the
ways
change
influences
characteristics
historical
extreme
events.
Earth s Future,
Journal Year:
2023,
Volume and Issue:
11(4)
Published: April 1, 2023
Abstract
Understanding
how
droughts
are
characterized,
propagated,
and
projected,
particularly
multivariate
droughts,
is
necessary
to
explain
the
variability
changes
in
drought
characteristics.
This
study
aims
understand
multimodel
global
monitoring,
propagation,
projection
by
utilizing
a
standardized
index
(MSDI)
during
historical
(1959–2014)
future
(2045–2100)
periods
under
two
socioeconomic
pathways
SSPs
(370
585),
derived
from
bias‐corrected
Coupled
Model
Intercomparison
Project
Phase
6
(CMIP6).
Based
on
energy
metrics,
bias
correction
method
outperformed
other
techniques
correcting
biases
CMIP6
representation.
The
indicators
demonstrate
distinct
categories
for
meteorological,
hydrological,
droughts.
There
were
significant
high
cross
correlations
between
Heatwave
Total
Length
(HWTL)
MSDI
Africa
South
America
all
lagged
times.
Europe
North
generally
saw
maximum
duration
(228
months)
period.
For
projections,
recorded
(197
months),
while
witnessed
minimum
SSP
370
(171
(149
585.
Furthermore,
period
tropical
Africa,
propagation
of
meteorological
hydrological
was
slower
wet
months
than
dry
months.
Under
projection,
there
shift
long
meteorological‐hydrological
middle
late
beginning
Africa.
Therefore,
tracking
projecting
characteristics
vital
understanding
risk
drought‐related
consequences.
One Earth,
Journal Year:
2024,
Volume and Issue:
7(1), P. 72 - 87
Published: Jan. 1, 2024
Global
water
scarcity
threatens
agriculture,
food
security,
and
human
sustainability.
Hence,
understanding
changes
in
terrestrial
storage
(WS)
is
crucial.
By
utilizing
climate
models,
reanalysis,
satellite
data,
we
demonstrate
the
effectiveness
of
multivariate
bias
correction
technique
facilitating
precise
WS
representation
while
ensuring
robust
budget
closure.
Historical
data
indicate
seasonal
changes,
where
forested
basins
exhibit
a
surplus
December-January-February
season,
with
reversal
June-July-August-September
season.
Non-forested
display
varied
patterns
influenced
by
geographical
location
land
use
type.
Future
projections
increased
deficits
most
Southern
Hemisphere
under
middle-road
(SSP
245)
scenario
wetter
conditions
regional
rivalry
370)
scenario.
Weather
systems
governing
vary
season
basin,
resulting
inconsistent
moisture
intake
into
basins.
These
findings
underscore
intricate
interplay
between
transport,
characteristics,
WS,
highlighting
need
to
understand
these
complex
interactions
for
effective
resource
management
strategies
changing
climates.
Environmental Research Letters,
Journal Year:
2024,
Volume and Issue:
19(7), P. 074009 - 074009
Published: June 5, 2024
Abstract
Precipitation
plays
a
crucial
role
in
Africa’s
agriculture,
water
resources,
and
economic
stability,
assessing
its
potential
changes
under
future
warming
is
important.
In
this
study,
we
demonstrate
that
the
latest
generation
of
coupled
climate
models
(CMIP6)
robustly
project
substantial
wetting
over
western,
central,
eastern
Africa.
contrast,
southern
Africa
Madagascar
tend
toward
drying.
Under
shared
socioeconomic
pathways
(defined
by
Shared
Socioeconomic
Pathways
SSP2-4.5
SSP5-8.5),
our
results
suggest
most
parts
Africa,
except
for
Madagascar,
will
experience
very
wet
years
five
times
more
often
2050–2100,
according
to
multi-model
median.
Conversely,
dry
twice
as
end
21st
century.
Furthermore,
find
increasing
risk
extreme
annual
rainfall
accompanied
shift
days
with
heavier
rainfall.
Our
findings
provide
important
insights
into
inter-hemispheric
precipitation
characteristics
underscore
need
serious
mitigation
adaptation
strategies.
Meteorological Applications,
Journal Year:
2024,
Volume and Issue:
31(3)
Published: May 1, 2024
Abstract
We
assess
the
impact
of
three
bias
correction
approaches
on
present
day
means
and
extremes,
climate
change
signal,
for
six
variables
(precipitation,
minimum
maximum
temperature,
radiation,
vapour
pressure
mean
sea
level
pressure)
from
dynamically
downscaled
simulations
over
Queensland,
Australia.
Results
show
that
all
bias‐correction
methods
are
effective
at
removing
systematic
model
biases,
however
results
variable
season‐dependent.
Importantly,
our
based
fully
independent
cross‐validation,
an
advantage
similar
studies.
Linear
scaling
preserves
signals
while
quantile
mapping
distribution‐based
transfer
function
modify
signal
patterns
change.
The
Perkins
score
values
above
95th
percentile
below
5th
was
used
to
evaluate
how
well
matches
observational
data.
Bias
improved
extremes
some
seasons.
rank
Kling–Gupta
efficiency
(KGE)
calculated
during
validation
period.
find
linear
empirical
best
Queensland
climatology.
On
average,
led
improvement
in
KGE
23%
annually.
However,
terms
extreme
values,
statistical
perform
best,
tends
worst.
Our
that,
except
scaling,
signal.
Comptes Rendus Géoscience,
Journal Year:
2023,
Volume and Issue:
355(S1), P. 411 - 438
Published: Jan. 12, 2023
In
this
study,
the
Soil
and
Water
Assessment
Tool
(SWAT)
model
is
used
to
assess
changes
in
surface
runoff
between
baseline
(1995–2014)
future
(2031–2050)
periods
Tougou
watershed
(37km
2
)
Burkina
Faso.
The
study
uses
a
combination
of
land
use
maps
(for
current
periods)
bias-corrected
ensemble
9
CMIP6
climate
models,
under
two
warming
scenarios.
An
increase
rainfall
(13.7%
18.8%)
projected,
which
major
contributor
(24.2%
34.3%).
change
narrative
(i.e.
conversion
bare
areas
croplands)
expected
decrease
runoff,
albeit
minor
comparison
effect
change.
Similar
findings
are
observed
for
annual
maximum
runoff.
This
sheds
light
on
need
consider
simultaneously
framing
water
management
policies.
Dans
cette
étude,
le
modèle
agro-éco-hydrologique
SWAT
est
utilisé
pour
évaluer
les
changements
dans
l’écoulement
de
entre
la
période
référence
1995–2014
et
2031–2050
sur
bassin
versant
au
Cette
étude
utilise
une
combinaison
cartes
d’états
(pour
actuelle
future)
un
corrigé
modèles
climatiques
issus
des
simulations
CMIP6,
sous
deux
scénarios
réchauffement.
Une
augmentation
précipitations
(de
13,7
%
à
18,8
%)
prévue,
ce
qui
principal
facteur
contribuant
l’augmentation
écoulements
(24,2
34,3
%).
Les
projetés
états
(principalement
surfaces
dégradées
en
sols
cultivés)
devrait
entraîner
diminution
surface,
toutefois
proportions
plus
faibles
comparaison
effets
du
climat
futur.
Des
résultats
similaires
sont
observés
lécoulement
maximal
annuel.
met
lumière
nécessité
prendre
compte
simultanément
futur
l’élaboration
politiques
futures
gestion
l’eau.