Authorea (Authorea),
Journal Year:
2023,
Volume and Issue:
unknown
Published: Dec. 21, 2023
Knowing
where
and
when
rivers
cease
to
flow
provides
an
important
basis
for
evaluating
riverine
biodiversity,
biogeochemistry
ecosystem
services.
We
present
a
novel
modeling
approach
estimate
monthly
time
series
of
streamflow
intermittence
at
high
spatial
resolution
the
continental
scale.
Streamflow
is
quantified
more
than
1.5
million
river
reaches
in
Europe
as
number
no-flow
days
grouped
into
five
classes
(0,
1-5,
6-15,
16-29,
30-31
days)
each
month
from
1981
2019.
Daily
observed
3706
gauging
stations
were
used
train
validate
two-step
Random
Forest
approach.
Important
predictors
derived
73
15
arc-sec
(~500
m)
grid
cells
that
computed
by
downscaling
0.5
arc-deg
(~55
km)
output
global
hydrological
model
WaterGAP,
which
accounts
human
water
use.
Of
perennial
intermittent
station-months,
97.8%
86.4%,
respectively,
are
correctly
predicted.
Interannual
variations
months
satisfactorily
simulated,
with
median
Pearson
correlation
0.5.
While
prevalence
underestimated,
overestimated
dry
regions
artificial
storage
abounds.
Our
estimates
3.8%
all
European
reach-months
17.2%
during
1981-2019,
predominantly
days.
Although
estimation
uncertainty
high,
our
study
provides,
first
time,
information
on
continent-wide
dynamics
streams.
Water Resources Research,
Journal Year:
2024,
Volume and Issue:
60(2)
Published: Feb. 1, 2024
Abstract
Understanding
the
spatio‐temporal
dynamics
of
runoff
generation
in
headwater
catchments
is
challenging,
due
to
intermittent
and
fragmented
nature
surface
flows.
The
active
stream
network
non‐perennial
rivers
contracts
expands,
with
a
dynamic
behavior
that
depends
on
complex
interplay
among
climate,
topography,
geology.
In
this
work,
CATchment
HYdrology,
an
integrated
surface–subsurface
hydrological
model
(ISSHM),
used
simulate
two
virtual
same,
spatially
homogeneous,
subsurface
characteristics
(hydraulic
conductivity,
porosity,
water
retention
curves)
but
different
morphology.
We
run
sets
simulations
reproduce
sequence
steady‐states
at
catchment
wetness
levels
transient
conditions
analyze
joint
variations
length
(
L
)
discharge
outlet
Q
high
resolutions.
shape
curves
differs
does
not
depend
climate
forcing,
as
it
mainly
controlled
by
underlying
topography.
then
analyzed
suitability
topographic
index
contributing
area
identify
spatial
configuration
maximum
catchments.
These
morphometric
parameters
provided
good
estimate
distribution
flowing
both
study
Our
numerical
indicate
ISSHMs
have
potential
accurately
describe
networks
processes
driving
such
that,
overall,
they
can
be
useful
tools
gain
insights
into
main
physical
drivers
streams.
Water Resources Research,
Journal Year:
2024,
Volume and Issue:
60(8)
Published: July 31, 2024
Abstract
Knowing
where
and
when
rivers
cease
to
flow
provides
an
important
basis
for
evaluating
riverine
biodiversity,
biogeochemistry
ecosystem
services.
We
present
a
novel
modeling
approach
estimate
monthly
time
series
of
streamflow
intermittence
at
high
spatial
resolution
the
continental
scale.
Streamflow
is
quantified
more
than
1.5
million
river
reaches
in
Europe
as
number
no‐flow
days
grouped
into
five
classes
(0,
1–5,
6–15,
16–29,
30–31
days)
each
month
from
1981
2019.
Daily
observed
3706
gauging
stations
were
used
train
validate
two‐step
random
forest
approach.
Important
predictors
derived
73
15
arc‐sec
(∼500
m)
grid
cells
that
computed
by
downscaling
0.5
arc‐deg
(∼55
km)
output
global
hydrological
model
WaterGAP,
which
accounts
human
water
use.
Of
perennial
non‐perennial
station‐months,
97.8%
86.4%,
respectively,
correctly
predicted.
Interannual
variations
months
satisfactorily
simulated,
with
median
Pearson
correlation
0.5.
While
prevalence
underestimated,
overestimated
dry
regions
artificial
storage
abounds.
Our
estimates
3.8%
all
European
reach‐months
17.2%
during
1981–2019,
predominantly
days.
Although
estimation
uncertainty
high,
our
study
provides,
first
time,
information
on
continent‐wide
dynamics
streams.
Journal of Hydrology,
Journal Year:
2024,
Volume and Issue:
632, P. 130686 - 130686
Published: Feb. 3, 2024
Multi-criteria
model
calibration
can
lead
to
a
better
representation
of
hydrological
processes
and
reduce
parameter
uncertainty
compared
on
streamflow
data
alone.
However,
the
additional
may
be
difficult
collect
or
aggregate
into
representative
catchment
average
value
that
used
calibrate
lumped
model.
Temporary
streams
are
highly
dynamic,
their
flow
state
observed
visually.
temporary
still
uncommon
rarely
in
modelling.
In
this
study,
we
unique
dataset
with
discrete
observations
for
France
evaluated
how
informative
these
calibrating
lumped,
bucket-type
We
calibrated
HBV
92
catchments
using
discharge
stream-level
at
different
temporal
resolutions
(daily,
one
daily
per
month,
season)
as
proxy
groundwater
storage.
stream
generally
did
not
result
overall
simulation
validation
period.
which
performance
based
only
was
poor,
it
more
likely
an
improvement
performance.
The
use
combination
reduced
uncertainties
low-flow
simulations
up
half
catchments.
This
caused
by
better-constrained
storage
coefficient
slowest
reservoir
elimination
sets
led
substantial
variations
improvements
due
inclusion
were
related
characteristics.
Thus,
remains
unclear
help
improve
uncertainty.
Hydrological Processes,
Journal Year:
2024,
Volume and Issue:
38(6)
Published: June 1, 2024
Abstract
Non‐perennial
streams
play
a
crucial
role
in
ecological
communities
and
the
hydrological
cycle.
However,
key
parameters
processes
involved
stream
intermittency
remain
poorly
understood.
While
climatic
conditions,
geology
land
use
are
well
identified,
assessment
modelling
of
groundwater
controls
on
streamflow
intermittence
challenge.
In
this
study,
we
explore
new
opportunities
to
calibrate
process‐based
3D
flow
models
designed
simulate
hydrographic
network
dynamics
groundwater‐fed
headwaters.
Streamflow
measurements
maps
considered
together
constrain
effective
hydraulic
properties
aquifer
hydrogeological
models.
The
simulations
were
then
validated
using
visual
observations
water
presence/absence,
provided
by
national
monitoring
France
(ONDE).
We
tested
methodology
two
pilot
unconfined
shallow
crystalline
catchments,
Canut
Nançon
catchments
(Brittany,
France).
found
that
both
expansion/contraction
required
simultaneously
estimate
conductivity
porosity
with
low
uncertainties.
calibration
allowed
good
prediction
intermittency,
terms
spatial
extent.
For
studied,
Nançon,
is
close
reaching
1.5
×
10
−5
m/s
4.5
m/s,
respectively.
they
differ
more
their
storage
capacity,
estimated
at
0.1%
2.2%,
Lower
capacity
leads
higher
level
fluctuations,
shorter
response
times,
an
increase
proportion
intermittent
reduction
perennial
flow.
This
framework
for
predicting
headwater
can
be
deployed
improve
our
understanding
different
geomorphological,
geological
contexts.
It
will
benefit
from
advances
remote
sensing
crowdsourcing
approaches
generate
observational
data
products
high
temporal
resolution.
Limnology and Oceanography,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Oct. 7, 2024
Abstract
River
network
connectivity
(RC)
describes
the
hydrologic
exchange
of
water,
nutrients,
sediments,
and
pollutants
between
river
channel
other
“sites”
via
heterogenous
flowpaths
along
corridor.
As
water
moves
downstream
it
carries
these
constituents,
creating
a
stream‐to‐ocean
continuum
that
regulates
global
carbon,
nutrient
cycling.
models
have
developed
over
many
decades,
culminating
in
recent
years
with
network‐scale
RC
explicitly
simulate
transport
elements
from
headwaters
to
coasts,
sometimes
requiring
contain
tens
millions
reaches.
These
advances
provide
transformative
insights
into
aggregate
effects
on
material
across
scales
local
global.
Yet,
reviews
pointed
several
challenges
need
be
overcome
continue
advancing
modeling.
In
service
goals,
I
summarize
maps
identify
similarities
differences
large‐scale
modeling
landscape.
Although
our
computational
upscaling
abilities
significantly
improved
revealed
new
insights,
current
are
still
limited
by
quantity,
quality,
resolution,
lack
standardization
available
situ
databases
source
data
necessary
for
This
suggests
we
can
extend
if
keep
improving
datasets,
while
continuously
revisiting
physics
theory
explain
those
data.
doing
so,
will
expand
role
informing
quality
management
future.
Hydrological Processes,
Journal Year:
2023,
Volume and Issue:
37(12)
Published: Dec. 1, 2023
Abstract
Headwater
streams
often
experience
intermittent
flow.
Consequently,
the
flowing
drainage
network
expands
and
contracts
density
(DD)
varies
over
time.
Monitoring
DD
dynamics
is
essential
to
understand
processes
controlling
it.
However,
our
knowledge
of
event‐scale
limited
because
high
spatial
temporal
resolution
data
on
remain
sparse.
Therefore,
team
monitored
hydrologic
variables
in
two
5‐ha
headwater
catchments
Swiss
pre‐Alps
summer
2021,
through
mapping
surveys
flow
state
a
wireless
streamwater
level
sensor
network.
We
combined
sources
calculate
at
event‐time
scale.
Our
so‐called
CEASE
method
assumes
that
channel
reach
occurs
above
set
water
thresholds,
it
determined
DDs
with
accuracies
>94%.
responses
events
differed
for
catchments,
despite
their
proximity
similar
size.
ranged
from
2.7
32.2
km
−2
flatter
catchment
(average
slope:
15°).
For
this
catchment,
discharge‐DD
relationship
became
steeper
when
exceeded
20
increased
substantially
relatively
small
increases
discharge.
rainfall
during
dry
conditions,
showed
counterclockwise
hysteresis,
likely
due
initially
groundwater
discharge
area
near
outlet;
once
stopped,
remained
streamflow
recession
rising
levels
throughout
catchment.
wet
responded
synchronously.
In
24°),
varied
only
7.8
14.6
there
was
no
hysteresis
or
threshold
behaviour
relationship,
multiple
springs
maintained
monitoring
period.
These
results
highlight
variability
its
across
catchments.
Freshwater Science,
Journal Year:
2023,
Volume and Issue:
42(3), P. 247 - 267
Published: June 5, 2023
Streamflow-duration
assessment
methods
(SDAMs)
are
rapid,
indicator-based
tools
for
classifying
streamflow
duration
(e.g.,
intermittent
vs
perennial
flow)
at
the
reach
scale.
Indicators
easily
assessed
stream
properties
used
as
surrogates
of
flow
duration,
which
is
too
resource
intensive
to
measure
directly
many
reaches.
Invertebrates
commonly
SDAM
indicators
because
not
highly
mobile,
and
different
species
have
life
stages
that
require
durations
times
year.
The
objectives
this
study
were
1)
identify
invertebrate
taxa
can
be
distinguish
between
reaches
having
flow,
2)
compare
indicator
strength
across
taxonomic
numeric
resolutions,
3)
assess
relative
importance
season
habitat
type
on
ability
invertebrates
predict
streamflow-duration
class.
We
2
methods,
random
forest
models
analysis,
analyze
aquatic
terrestrial
data
(presence/absence,
density,
biomass)
family
genus
levels
from
370
samples
collected
both
erosional
depositional
habitats
during
wet
dry
seasons.
In
total,
36
53
sampled
along
31
forested
headwater
streams
in
4
level
II
ecoregions
United
States.
Random
family-
genus-level
datasets
had
classification
accuracy
ranging
88.9
93.2%,
with
slightly
higher
density
than
presence/absence
biomass
datasets.
Season
(wet/dry)
tended
a
stronger
predictor
class
(erosional/depositional).
Many
(58.8%)
(61.6%)
reaches,
most
exclusive
1
rarely
collected.
However,
23
family-level
or
(20
3
terrestrial)
44
genera
identified
potential
streams.
utility
varied
part
representation
dataset
but
also
variable
ecological
responses
drying
among
species.
Aquatic
been
an
important
field
existing
SDAMs,
our
findings
highlight
how
including
further
maximize
classifications.