Abstract.
Since
1950,
European
rivers
have
been
put
under
increasing
pressure
by
anthropogenic
activities,
resulting
in
changes
climate,
land
cover,
soil
properties
and
channel
morphologies.
These
evolving
environmental
conditions
can
translate
into
hydrological
conditions.
The
availability
of
consistent
estimates
river
flow
at
global
continental
level
is
a
necessity
to
assess
attribute
the
cycle.
To
overcome
limitations
posed
observations
(incomplete
records,
inhomogeneous
spatial
coverage),
we
simulate
discharge
for
Europe
period
1950–2020
using
state-of-the-art
modelling
approach.
We
use
new
set
up
LISFLOOD
model,
running
1
arcminute
(≈1.8
km)
with
six-hourly
time
steps.
model
forced
climate
reanalysis
data
(ERA5-land)
bias-corrected
downscaled
resolution
weather
observations.
also
ingests
72
surface
fields
maps
representing
catchment
morphology,
vegetation,
properties,
use,
water
demand,
lakes
reservoirs.
Inputs
related
human
activities
are
through
emulate
society.
Hydrological
ReAnalysis
(HERA),
provides
282
521
pixels
upstream
area
>
100
km2.
its
skill
2901
gauging
stations
distributed
across
Europe.
Overall,
HERA
delivers
satisfying
results,
general
weak
underestimation
observed
mean
variability.
find
that
performance
increases
between
1950
2020.
fine
temporal
result
an
enhanced
compared
other
small-to-medium-scale
catchments
(100–10
000
km2),
degraded
remaining
small
catchments.
first
long-term,
high-resolution
Despite
limitations,
it
enables
analysis
dynamics
extremes,
influences,
change
scale
while
keeping
local
relevance.
It
creates
opportunity
study
these
ungauged
Abstract.
Since
1950,
European
rivers
have
been
put
under
increasing
pressure
by
anthropogenic
activities,
resulting
in
changes
climate,
land
cover,
soil
properties
and
channel
morphologies.
These
evolving
environmental
conditions
can
translate
into
hydrological
conditions.
The
availability
of
consistent
estimates
river
flow
at
global
continental
level
is
a
necessity
to
assess
attribute
the
cycle.
To
overcome
limitations
posed
observations
(incomplete
records,
inhomogeneous
spatial
coverage),
we
simulate
discharge
for
Europe
period
1950–2020
using
state-of-the-art
modelling
approach.
We
use
new
set
up
LISFLOOD
model,
running
1
arcminute
(≈1.8
km)
with
six-hourly
time
steps.
model
forced
climate
reanalysis
data
(ERA5-land)
bias-corrected
downscaled
resolution
weather
observations.
also
ingests
72
surface
fields
maps
representing
catchment
morphology,
vegetation,
properties,
use,
water
demand,
lakes
reservoirs.
Inputs
related
human
activities
are
through
emulate
society.
Hydrological
ReAnalysis
(HERA),
provides
282
521
pixels
upstream
area
>
100
km2.
its
skill
2901
gauging
stations
distributed
across
Europe.
Overall,
HERA
delivers
satisfying
results,
general
weak
underestimation
observed
mean
variability.
find
that
performance
increases
between
1950
2020.
fine
temporal
result
an
enhanced
compared
other
small-to-medium-scale
catchments
(100–10
000
km2),
degraded
remaining
small
catchments.
first
long-term,
high-resolution
Despite
limitations,
it
enables
analysis
dynamics
extremes,
influences,
change
scale
while
keeping
local
relevance.
It
creates
opportunity
study
these
ungauged
Journal of Flood Risk Management,
Journal Year:
2025,
Volume and Issue:
18(1)
Published: Jan. 17, 2025
ABSTRACT
Devastating
flood
events
are
recurrently
impacting
West
Africa.
To
mitigate
impacts
and
reduce
the
vulnerability
of
populations,
a
better
knowledge
on
frequency
these
is
crucial.
The
lack
reliable
hydrometric
datasets
has
hitherto
been
major
limitation
in
analysis
at
scale
Utilising
recently
developed
African
database,
we
perform
annual
maximum
flow
(AMF)
time
series,
covering
246
river
basins
Africa,
between
1975
2018.
Generalized
extreme
value
(GEV)
Gumbel
probability
distributions
were
compared
to
fit
AMF
series
with
L‐moments,
Maximum
Likelihood
(MLE)
(GMLE)
methods.
Results
indicated
that
GEV
distribution
GMLE
method
provided
best
results.
Regional
envelope
curves
entire
region
unprecedented
data
coverage
have
generated
for
first‐time
providing
insights
estimation
quantiles
ungauged
basins.
correlation
watershed
properties
shows
significant
correlations
catchment
area,
groundwater
storage,
altitude
topographic
wetness
index.
findings
from
this
study
useful
risk
assessment
design
hydraulic
infrastructures
region,
first
step
prior
development
regional
approaches
transfer
information
gauged
sites
catchments.
Journal of Hydrology Regional Studies,
Journal Year:
2022,
Volume and Issue:
44, P. 101251 - 101251
Published: Oct. 26, 2022
Upper
Blue
Nile
River
Basin,
Ethiopia
This
study
aims
to
determine
possible
trends
in
monthly,
seasonal
and
annual
precipitation
streamflow
series.
The
Discrete
Wavelet
Transform
(DWT)
was
used
obtain
detailed
information
about
the
time-frequency
conditions
of
six
meteorological
five
stations
during
1984–2014.
Mann-Kendall
test
also
applied
original
DWT
components
which
periodicities
are
dominant
reproducing
observed
trends.
combined
has
not
been
explored
UBNRB
context.
We
three
criteria
a
suitable
wavelet,
decomposition
level,
signal
extension
mode.
From
these
criteria,
bias
ratio
between
wavelet
approximation
series
time
proposed
this
study.
Results
show
that
almost
all
experience
an
insignificant
but
increasing
trend,
whereas
exhibit
trend
at
5%
significance
level.
use
periodic
events
up
4
years
more
influential
affecting
Climate,
Journal Year:
2023,
Volume and Issue:
11(5), P. 95 - 95
Published: April 28, 2023
The
ever-increasing
need
for
water,
the
alteration
in
climate,
and
its
observed
changes
over
recent
years
have
triggered
a
lot
of
research
studies
associated
with
phenomenon
drought.
Within
wider
geographical
region
Mediterranean,
relevant
scientific
subject
seems
to
be
great
interest,
since
it
is
undoubtedly
related
number
severe
socio-economic
consequences.
This
present
effort
focuses
on
evolution
this
particular
time,
within
borders
nine
different
countries
Eastern
Mediterranean
(Athens,
Greece—Europe;
Constantinople,
Turkey—Asia;
Nicosia,
Cyprus—Europe;
Jerusalem,
Israel—Asia;
Amman,
Jordan—Asia;
Damascus,
Syria—Asia;
Beirut,
Lebanon—Asia;
Cairo,
Egypt—Africa;
Tripoli
Libya—Africa).
By
applying
Standard
Precipitation
Index
(SPI),
examining
precipitation
data
at
month
level
(January
1901
December
2020),
utilizing
Inverse
Distance
Weighted
(IDW)
method,
spatio–temporal
variability
drought
events
area
was
studied.
In
long-term
droughts
presented
higher
than
usual
volume,
accordance
12-
24-month
SPI,
starting
from
mid-20th
century.
Similarly,
Damascus
similar
pattern
those
Jerusalem.
An
upward
trend
frequency
extreme
last
thirty
years.
same
true
terms
duration
dry
periods.
Drought
also
been
central,
southern,
eastern
regions
Turkey.
A
downward
Cairo
based
analysis
monthly
precipitation.
Climatic Change,
Journal Year:
2024,
Volume and Issue:
177(3)
Published: Feb. 26, 2024
Abstract
The
Nile
basin
is
the
second
largest
in
Africa
and
one
of
regions
experiencing
high
climatic
diversity
with
variability
precipitation
deteriorating
water
resources.
As
climate
change
affecting
most
hydroclimatic
variables
across
world,
this
study
assesses
whether
historical
changes
river
flow
sediment
loads
at
selected
gauges
can
be
attributed
to
change.
An
impact
attribution
approach
employed
by
constraining
a
process-based
model
set
factual
counterfactual
forcing
data
for
69
years
(1951–2019),
from
setup
Inter-Sectoral
Impact
Model
Intercomparison
Project
(ISIMIP3a).
To
quantify
role
change,
we
use
non-parametric
Mann-Kendall
test
identify
trends
calculate
differences
long-term
mean
annual
load
simulations
between
using
data.
Results
stations
Lake
Victoria
show
reasonable
evidence
increase
flows
(two
stations)
(one
station),
largely
climate.
In
contrast,
within
Blue
Main
basins,
there
slight
decrease
four
under
climate,
which
but
no
significant
station).
These
findings
spatial
impacts
on
area
period.
Journal of Hydrology,
Journal Year:
2024,
Volume and Issue:
640, P. 131679 - 131679
Published: July 14, 2024
Sub-Saharan
Africa
(SSA)
is
strongly
affected
by
flood
hazards,
endangering
human
lives
and
economic
stability.
However,
the
role
of
internal
climate
modes
variability
in
driving
fluctuations
SSA
occurrence
remains
poorly
documented
understood.
To
address
this
gap,
we
quantify
relative
combined
contribution
large-scale
drivers
to
seasonal
regional
using
a
new
65-year
daily
streamflow
dataset,
sea-surface
temperatures
derived
from
observations,
12
Single
Model
Initial-condition
Large
Ensembles
(SMILEs)
Coupled
Intercomparison
Project
Phases
5
6.
We
find
significant
relationships
between
floods
across
SSA,
with
climatic
accounting
for
30–90
%
floods.
Notably,
western,
central,
summer-rain
region
southern
display
stronger
teleconnections
comparison
East
winter-rain
South
Africa,
where
circulation
patterns
activities
may
play
more
important
role.
In
eastern
are
mainly
influenced
Pacific
Indian
Oceans,
while
western
central
Atlantic
Ocean
Mediterranean
Sea
larger
also
that
number
projected
fluctuate
±
10–50
during
21st
century
response
different
sequences
key
variability.
note
contributions
future
risks
generally
consistent
all
SMILEs.
Our
findings
thus
provide
valuable
information
long-term
disaster
risk
reduction
management.
International Journal of Climatology,
Journal Year:
2024,
Volume and Issue:
44(7), P. 2462 - 2483
Published: April 16, 2024
Abstract
In
this
study,
hindcasts
from
eight
Copernicus
Climate
Change
Service
(C3S)
and
three
North
American
Multi‐Model
Ensemble
(NMME)
operational
seasonal
forecast
systems,
based
on
dynamical
climate
models,
are
employed
to
investigate
the
influence
of
South
Atlantic
Ocean
Dipole
(SAOD)
predictive
skill
Central
Africa
(CA)
rainfall.
The
focus
is
primarily
June–July–August
season
for
1993–2016.
findings
reveal
that,
when
regionally
averaged,
all
models
exhibit
positive
in
predicting
CA
rainfall,
except
Geophysical
Fluid
Dynamics
Laboratory
(GFDL‐SPEAR)
model.
Notably,
there
significant
spatial
variations
across
different
regions.
Model
performance
particularly
low
(high)
African
Republic
Congo
Basin
(Gabon
Chad)
tends
deteriorate
with
increasing
lead‐time.
Models
that
demonstrate
a
strong
connection
between
SAOD
rainfall
tend
better
skills
forecasting
contrast
weaker
connections.
This
leads
in‐phase
relationship
strength
SAOD–rainfall
among
models.
Furthermore,
atmospheric
circulation
responding
SST
forcing
associated
El
Niño–Southern
Oscillation
exerts
robust
climatological
mean
over
SAO.
suggests
state
bias
SAO/equatorial
Pacific
region
plays
role
modulating
simulated
SAOD–CA
and,
consequently,
prediction
general,
both
NMME
C3S
appear
be
valuable
tools
capable
providing
essential
information
several
months
advance.
These
insights
can
aid
decision‐makers
making
informed
decisions
regarding
adaptation
mitigation
measures.
Earth system science data,
Journal Year:
2025,
Volume and Issue:
17(1), P. 293 - 316
Published: Jan. 30, 2025
Abstract.
Since
1950,
anthropogenic
activities
have
altered
the
climate,
land
cover,
soil
properties,
channel
morphologies,
and
water
management
in
river
basins
of
Europe.
This
has
resulted
significant
changes
hydrological
conditions.
The
availability
consistent
estimates
flow
at
global
continental
levels
is
a
necessity
for
assessing
cycle.
To
overcome
limitations
posed
by
observations
(incomplete
records,
inhomogeneous
spatial
coverage),
we
simulate
discharge
Europe
period
1951–2020
using
state-of-the-art
modelling
approach.
We
use
new
European
set-up
OS
LISFLOOD
model,
running
1
arcmin
(≈1.8
km)
with
6-hourly
time
steps.
model
forced
climate
reanalysis
data
(ERA5-Land)
that
are
bias-corrected
downscaled
to
resolution
gridded
weather
observations.
also
incorporates
72
surface
field
maps
representing
catchment
morphology,
vegetation,
use,
demand,
lakes,
reservoirs.
Inputs
related
human
evolving
through
emulate
societal
changes.
resulting
Hydrological
ReAnalysis
(HERA)
provides
282
521
pixels
an
upstream
area
>100
km2.
assess
its
skill
2448
gauging
stations
distributed
across
Overall,
HERA
delivers
satisfying
results
(median
KGE′=0.55),
despite
general
underestimation
observed
mean
discharges
(mean
bias=-13.1
%),
demonstrates
capacity
reproduce
statistics
extreme
flows.
performance
increases
size,
it
varies
space
depending
on
reservoir
influence
calibration.
fine
temporal
enhanced
compared
previous
based
small-
medium-scale
catchments
(100–10
000
km2).
first
publicly
available
long-term,
high-resolution
Despite
limitations,
enables
analysis
dynamics
extremes,
influences,
change
scale
while
maintaining
local
relevance.
It
creates
opportunity
study
these
ungauged
dynamic
socio-economic
inputs
via
JRC
catalogue:
https://doi.org/10.2905/a605a675-9444-4017-8b34-d66be5b18c95
(Tilloy
et
al.,
2024).