Hydrology and earth system sciences,
Journal Year:
2023,
Volume and Issue:
27(17), P. 3221 - 3239
Published: Sept. 8, 2023
Abstract.
The
assessment
of
effective
hydraulic
properties
at
the
catchment
scale,
i.e.,
conductivity
(K)
and
transmissivity
(T),
is
particularly
challenging
due
to
sparse
availability
hydrological
monitoring
systems
through
stream
gauges
boreholes.
To
overcome
this
challenge,
we
propose
a
calibration
methodology
which
only
considers
information
from
digital
elevation
model
(DEM)
spatial
distribution
network.
built
on
assumption
that
groundwater
system
main
driver
controlling
density
extension,
where
perennial
network
reflects
intersection
table
with
topography.
Indeed,
seepage
surface
primarily
controlled
by
topography,
aquifer
thickness
dimensionless
parameter
K/R,
R
average
recharge
rate.
Here,
use
process-based
parsimonious
3D
flow
calibrate
K/R
minimizing
relative
distances
between
observed
simulated
generated
zones.
By
deploying
in
24
selected
headwater
catchments
located
northwestern
France,
demonstrate
method
successfully
predicts
extent
for
80
%
cases.
Results
show
high
sensitivity
extension
low-order
streams
limited
impacts
DEM
resolution
as
long
remains
consistent
observations.
assuming
an
rate,
found
K
values
vary
1.0×10-5
1.1×10-4
m
s−1,
agreement
local
estimates
derived
tests
independent
calibrated
model.
With
emergence
global
remote-sensing
databases
compiling
high-resolution
networks,
approach
provides
new
opportunities
assess
unconfined
aquifers
ungauged
basins.
BioScience,
Journal Year:
2022,
Volume and Issue:
73(1), P. 9 - 22
Published: Dec. 7, 2022
Abstract
Rivers
that
do
not
flow
year-round
are
the
predominant
type
of
running
waters
on
Earth.
Despite
a
burgeoning
literature
natural
intermittence
(NFI),
knowledge
about
hydrological
causes
and
ecological
effects
human-induced,
anthropogenic
(AFI)
remains
limited.
NFI
AFI
could
generate
contrasting
biological
responses
in
rivers
because
distinct
underlying
drying
evolutionary
adaptations
their
biota.
We
first
review
show
how
different
drivers
alter
timing,
frequency
duration
drying,
compared
with
NFI.
Second,
we
evaluate
possible
differences
biodiversity
responses,
functions,
ecosystem
services
between
AFI.
Last,
outline
gaps
management
needs
related
to
Because
hydrologic
characteristics
impacts
AFI,
ignoring
distinction
undermine
intermittent
ephemeral
streams
exacerbate
risks
ecosystems
societies
downstream.
Hydrology and earth system sciences,
Journal Year:
2022,
Volume and Issue:
26(6), P. 1527 - 1543
Published: March 22, 2022
Abstract.
In
a
warming
climate,
periods
with
lower
than
average
precipitation
will
increase
in
frequency
and
intensity.
During
such
periods,
known
as
meteorological
droughts,
the
decline
annual
runoff
may
be
proportionally
larger
corresponding
precipitation.
Reasons
behind
this
exacerbation
of
deficit
during
dry
remain
largely
unknown,
challenges
predictability
when
occur
future
how
intense
it
be.
work,
we
tested
hypothesis
that
droughts
is
common
feature
across
climates,
driven
by
evaporation
enhancement.
We
relied
on
multidecadal
records
streamflow
for
more
200
catchment
areas
various
European
which
distinctively
show
emergence
similar
exacerbated
identified
previous
studies,
i.e.
order
−20
%
to
−40
less
what
expected
from
deficits.
The
magnitude
two
three
times
basins
located
regions
wet
regions,
qualitatively
correlated
an
+11
+33
over
characterized
energy-limited
water-limited
regimes,
respectively.
Thus,
enhanced
atmospheric
vegetation
demand
moisture
induces
nonlinear
precipitation-runoff
relationship
low-flow
results
unexpectedly
large
decrease
already
low
water
availability.
Forecasting
onset,
magnitude,
duration
these
drops
have
paramount
societal
ecological
implications,
especially
given
their
supporting
role
safeguarding
water,
food,
energy.
outcome
are
prone
climates
regimes
makes
further
understanding
its
patterns
urgent
priority
water-resource
planning
management
drier
climate.
Hydrology and earth system sciences,
Journal Year:
2024,
Volume and Issue:
28(4), P. 851 - 871
Published: Feb. 23, 2024
Abstract.
Rivers
are
rich
in
biodiversity
and
act
as
ecological
corridors
for
plant
animal
species.
With
climate
change
increasing
anthropogenic
water
demand,
more
frequent
prolonged
periods
of
drying
river
systems
expected,
endangering
ecosystems.
However,
understanding
predicting
the
hydrological
mechanisms
that
control
periodic
rewetting
rivers
is
challenging
due
to
a
lack
studies
observations,
particularly
non-perennial
rivers.
Within
framework
Horizon
2020
DRYvER
(Drying
River
Networks
Climate
Change)
project,
modelling
study
flow
intermittence
being
carried
out
three
European
catchments
(Spain,
Finland,
France)
characterised
by
different
climate,
geology,
use.
The
objective
this
represent
spatio-temporal
dynamics
at
reach
level
mesoscale
networks
(between
120
350
km2).
daily
spatially
distributed
condition
(flowing
or
dry)
predicted
using
J2000
model
coupled
with
random
forest
classification
model.
Observed
data
from
sources
(water
measurements,
photo
traps,
citizen
science
applications)
used
build
predictive
This
aims
evaluate
impact
observed
dataset
(sample
size,
spatial
temporal
representativity)
on
performance
Results
show
hybrid
approach
developed
allows
patterns
be
accurately
catchments,
sensitivity
criterion
above
0.9
prediction
dry
events
Finnish
French
case
0.65
Spanish
study.
shows
value
combining
reduce
uncertainty
intermittence.
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.
Hydrological Sciences Journal,
Journal Year:
2022,
Volume and Issue:
68(2), P. 276 - 289
Published: Dec. 6, 2022
Non-perennial
rivers
and
streams
are
ubiquitous.
Nonetheless,
our
understanding
of
their
hydrological
patterns
is
minimal.
Hydrological
models
powerful
tools
to
study
characterize
patterns,
but
few
can
simulate
extremes
such
as
non-flow
events.
We
aimed
capture
accurately
the
flow
intermittency
spatial
temporal
in
a
Mediterranean
river
basin
with
restructured
Soil
Water
Assessment
Tool
(SWAT+).
calibrated
model
using
multi-objective
optimization
algorithm
data
from
two
gauging
stations
mainstream
for
period
2000–2020.
Furthermore,
we
validated
simulations
against
stage
series
at
14
stations.
The
results
indicated
that
simulates
low
flows
period.
observed
significant
variation
both
space
time
remarkable
inter-annual
variability.
also
an
increase
over
Water Resources Research,
Journal Year:
2023,
Volume and Issue:
59(9)
Published: Sept. 1, 2023
Abstract
The
western
U.S.
is
experiencing
increasing
rain
to
snow
ratios
due
climate
change,
and
scientists
are
uncertain
how
changing
recharge
patterns
will
affect
future
groundwater‐surface
water
connection.
We
examined
watershed
topography
streambed
hydraulic
conductivity
impact
groundwater
age
stream
discharge
at
eight
sites
along
a
headwater
within
the
Manitou
Experimental
Forest,
CO
USA.
To
do
so,
we
measured:
(a)
continuous
discharge/level
specific
from
April
November
2021;
(b)
biweekly
chemistry;
(c)
chlorofluorocarbons
tritium
in
spring
fall;
(d)
conductivity;
(e)
local
slope.
used
chemistry
data
calculate
fluorite
saturation
states
that
were
inform
end‐member
mixing
analysis
of
streamflow
source.
then
combined
chlorofluorocarbon
estimate
composition
riparian
groundwater.
Our
suggest
drying
more
probable
where
slope
steep
high.
In
these
areas,
source
shifted
seasonally,
as
indicated
by
increases,
observed
high
fraction
streamflow,
primarily
interflow
adjacent
hillslopes.
contrast,
flat
low,
likely
persist
was
seasonally
constant
buffered
storage
alluvial
sediments.
Groundwater
paired
with
characterization
subsurface
characteristics
enabled
identification
controls
on
patterns.
Ecosystems,
Journal Year:
2022,
Volume and Issue:
26(4), P. 873 - 892
Published: Dec. 12, 2022
Abstract
Streams
and
rivers
act
as
landscape-scale
bioreactors
processing
large
quantities
of
terrestrial
particulate
organic
matter
(POM).
This
function
is
linked
to
their
flow
regime,
which
governs
residence
times,
shapes
reactivity
controls
the
amount
carbon
(C)
exported
atmosphere
coastal
oceans.
Climate
change
impacts
regimes
by
increasing
both
flash
floods
droughts.
Here,
we
used
a
modelling
approach
explore
consequences
lateral
hydrological
contraction,
that
is,
reduction
wet
portion
streambed,
for
POM
decomposition
transport
at
river
network
scale.
Our
model
integrates
seasonal
leaf
litter
input
generator
POM,
transient
storage
on
dry
streambed
portions
with
associated
ensuing
changes
in
reactivity,
dynamics
through
dendritic
network.
Simulations
showed
from
its
average
increased
due
combination
(1)
low
while
stored
streambeds,
(2)
shunting
during
flashy
events.
The
sensitivity
analysis
further
supported
high
contraction
leads
higher
export
regardless
coefficient
values,
fresh
differences
between
under
conditions.
study
incorporates
areas
into
pulse-shunt
concept
(Raymond
others
Ecology
97(1):5–16,
2016.
https://doi.org/10.1890/14-1684.1
),
providing
mechanistic
framework
testable
predictions
about
storage,
fluvial
networks.
Hydrological Processes,
Journal Year:
2022,
Volume and Issue:
36(8)
Published: Aug. 1, 2022
Abstract
A
limited
number
of
gauging
stations,
especially
for
nested
catchments,
hampers
a
process
understanding
the
interaction
between
streamflow,
groundwater
and
water
usage
during
drought.
Non‐commercial
measurement
devices
can
help
overcome
this
lack
monitoring,
but
they
need
to
be
thoroughly
tested.
The
Dreisam
River
in
South‐West
Germany
was
affected
by
several
hydrological
drought
events
from
2015
2020
which
parts
main
stream
tributaries
fell
dry.
Therefore
it
provided
useful
case
study
area
flexible
longitudinal
quality
quantity
monitoring
network.
Among
other
measurements
setup
employs
an
image‐based
method
with
QR
codes
as
fiducial
marker.
In
order
assess
under
conditions
QR‐code
based
level
loggers
(WLL)
deliver
data
according
scientific
standards,
we
compared
its
performance
conventional
capacitive
WLL.
results
20
stations
reveal
that
riverbed
dry
>50%
at
locations
even
>70%
most
severely
July
August
2020,
north
western
catchment
being
concerned.
Highly
variable
drying
patterns
reaches
emerged
monitoring.
found
valuable
identification
validation
zero
occurrences.
Nevertheless,
simple
image
processing
approach
(based
on
automatic
thresholding
algorithm)
did
not
compensate
errors
due
natural
technical
setup.
Our
findings
highlight
complexity
environments
is
major
challenge
when
working
methods.
Hydrology and earth system sciences,
Journal Year:
2023,
Volume and Issue:
27(3), P. 703 - 722
Published: Feb. 9, 2023
Abstract.
Transmission
losses
are
the
loss
in
flow
volume
of
a
river
as
water
moves
downstream.
These
provide
crucial
ecosystem
services,
particularly
ephemeral
and
intermittent
systems.
can
be
quantified
at
many
scales
using
different
measurement
techniques.
One
most
common
methods
is
differential
gauging
two
locations.
An
alternative
method
for
non-perennial
rivers
to
replace
downstream
location
by
visual
assessments
wetted
length
on
satellite
images.
The
transmission
then
calculated
gauged
upstream
divided
length.
We
used
this
approach
estimate
Selwyn
River
(Canterbury,
New
Zealand)
147
images
collected
between
March
2020
May
2021.
drying
front
was
verified
field
six
occasions
seven
campaigns
were
conducted
ground-truth
estimated
from
point
data
obtained
lengths
train
an
ensemble
random
forest
models
predict
continuous
hourly
time
series
their
uncertainties.
Our
results
show
that
ranged
0.25
0.65
m3s-1km-1
during
1-year
study
period.
However,
shortly
after
flood
peak
could
reach
up
1.5
m3s-1km-1.
enabled
us
improve
our
understanding
groundwater–surface
interactions
valuable
support
management.
argue
framework
easily
adapted
other
longer
series.