Abstract.
Despite
the
importance
of
temporary
streams
for
provision
key
ecosystem
services,
their
experimental
monitoring
remains
challenging
because
practical
difficulties
in
performing
accurate
high-frequency
surveys
flowing
portion
river
networks.
In
this
study,
about
30
electrical
resistance
(ER)
sensors
were
deployed
a
high
relief
2.6
km2
catchment
Italian
Alps
to
monitor
spatio-temporal
dynamics
active
network
during
fall
2019.
The
set-up
ER
was
personalized
make
them
more
flexible
deployment
field
and
under
low
flow
conditions.
Available
data
analyzed,
compared
based
estimates
nodes'
persistency
then
used
generate
sequence
maps
representing
reaches
stream
with
sub-daily
temporal
resolution.
This
allowed
proper
estimate
joint
variations
length
(L)
discharge
(Q)
entire
study
period.
Our
analysis
revealed
cross-correlation
between
statistics
individual
signals
persistencies
cross
sections
where
placed.
observed
spatial
actively
channels
also
diversity
hydrological
behaviour
distinct
zones
catchment,
which
attributed
differences
geology
stream-bed
composition.
pronounced
responsiveness
total
small
precipitation
events
as
led
important
hysteresis
L
vs.
Q
relationship,
thereby
impairing
performances
power-law
model
frequently
literature
relate
these
two
quantities.
Consequently,
our
site
adoption
unique
L-Q
relationship
infer
variability
from
discharges
would
underestimate
actual
by
40%.
work
emphasizes
potential
analysing
streams,
discussing
major
limitations
type
technology
emerging
specific
application
presented
herein.
Annual Review of Earth and Planetary Sciences,
Journal Year:
2023,
Volume and Issue:
51(1), P. 277 - 299
Published: Jan. 10, 2023
Landscapes
receive
water
from
precipitation
and
then
transport,
store,
mix,
release
it,
both
downward
to
streams
upward
vegetation.
How
they
do
this
shapes
floods,
droughts,
biogeochemical
cycles,
contaminant
the
health
of
terrestrial
aquatic
ecosystems.
Because
many
key
processes
occur
invisibly
in
subsurface,
our
conceptualization
them
has
often
relied
heavily
on
physical
intuition.
In
recent
decades,
however,
much
intuition
been
overthrown
by
field
observations
emerging
measurement
methods,
particularly
involving
isotopic
tracers.
Here
we
summarize
surprises
that
have
transformed
understanding
hydrological
at
scale
hillslopes
drainage
basins.
These
forced
a
shift
perspective
process
conceptualizations
are
relatively
static,
homogeneous,
linear,
stationary
ones
predominantly
dynamic,
heterogeneous,
nonlinear,
nonstationary.
▪Surprising
novel
measurements
transforming
functioning
landscapes.▪Even
during
storm
peaks,
streamflow
is
composed
mostly
stored
landscape
for
weeks,
months,
or
years.▪Streamflow
tree
uptake
originate
different
subsurface
storages
seasons’
precipitation.▪Stream
networks
dynamically
extend
retract
as
wets
dries,
stream
reaches
lose
flow
into
underlying
aquifers.
Journal of Hydrology,
Journal Year:
2024,
Volume and Issue:
632, P. 130728 - 130728
Published: Jan. 24, 2024
Fluvial
landscape
analysis
represents
an
essential
component
in
geomorphology,
hydrology,
ecology
and
cartography.
It
is
traditionally
focused
on
the
transition
between
hillslopes
channel
domain,
which
network
drainage
represented
by
static
flow
lines.
However,
natural
fluctuations
of
processes
occurring
watershed
induce
lateral
longitudinal
expansions
contractions
patterns
variations
stream
surface
area.
These
can
be
better
understood
introducing
a
two-dimensional
(2D)
view
catchment
hydrography,
river
width
floodplain
are
included
analysis.
The
novelty
introduced
this
work
development
hydrodynamic
hierarchical
framework
(HHF)
to
analyse
transitions
among
geomorphic
hydrographic
features
fluvial
landscape,
distinguishing
hillslope,
unchanneled
valleys,
floodplains,
single/multithreads
channels.
HHF
based
estimation
nested
inundation
pattern
domains
(IPDs)
from
digital
elevation
models
2D
modeling.
IPDs
defined
scaling
laws
that
characterize
log–log
relations
density
unit
discharge
thresholds
extracted
direct
rainfall
method
(DRM)
approach
under
steady
state
solutions.
physical
significance
analysed
within
context
both
physiographic
rates
employed
as
input
for
modeling
approach.
Initially,
spatial
heterogeneity
initially
used
derive
metrics
function
rate.
Then,
index,
representative
IPDs'
heterogeneity,
measure
susceptibility
area
expand/contract.
Finally,
consistency
results
assessed
comparison
another
hydrodynamic-based
recently
proposed
literature.
using
challenging
mountain
low-relief
environments,
characterized
multithread
channels,
meander
cut-offs,
oxbow
lakes,
extreme
landscapes
feature
glacial
outwash,
permafrost,
peatlands.
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.
Scientific Reports,
Journal Year:
2021,
Volume and Issue:
11(1)
Published: Nov. 2, 2021
Abstract
Looking
across
a
landscape,
river
networks
appear
deceptively
static.
However,
flowing
streams
expand
and
contract
following
ever-changing
hydrological
conditions
of
the
surrounding
environment.
Despite
ecological
biogeochemical
value
rivers
with
discontinuous
flow,
deciphering
temporary
nature
quantifying
their
extent
remains
challenging.
Using
unique
observational
dataset
spanning
diverse
geomorphoclimatic
settings,
we
demonstrate
existence
general
hierarchical
structuring
network
dynamics.
Specifically,
stream
activation
follows
fixed
repeatable
sequence,
in
which
least
persistent
sections
activate
only
when
most
ones
are
already
flowing.
This
phenomenon
not
facilitates
monitoring
activities,
but
enables
development
mathematical
framework
that
elucidates
how
climate
drives
temporal
variations
active
length.
As
gets
drier,
average
fraction
decreases
while
its
relative
variability
increases.
Our
study
provides
novel
conceptual
basis
for
characterizing
impacts.
Water Resources Research,
Journal Year:
2024,
Volume and Issue:
60(1)
Published: Jan. 1, 2024
Abstract
Non‐perennial
streams
have
a
global
prevalence,
but
quantitative
knowledge
of
the
temporal
dynamics
their
flowing
length—namely
extent
wet
portion
stream
network—remains
limited,
as
monitoring
spatiotemporal
configuration
channels
is
challenging
in
most
settings.
This
work
combines
high
spatial
resolution
visual
surveys
and
camera‐based
approaches
to
reconstruct
space‐time
network
3.7
km
2
Mediterranean
catchment
central
Italy.
Information
on
hydrological
status
derived
from
40
field
sub‐hourly
images
collected
with
21
stage‐cameras
are
combined
exploiting
hierarchical
principle.
The
latter
postulates
existence
Bayesian
chain,
defined
local
persistence
nodes
that
dictates
wetting/drying
order
during
expansion/retraction
cycles
network.
Our
results
highlight
complexity
study
area:
while
number
decreases
dry
season
increases
season,
persistency
exhibits
highly
heterogeneous
non‐monotonic
pattern,
originating
dynamically
disconnected
Despite
this
heterogeneity,
model
well
approximates
evolution
state
nodes,
an
accuracy
exceeds
99%.
Crucially,
allows
reconstruction
even
cases
which
part
was
not
observed.
provides
novel
conceptual
approach
for
poorly
accessible
sites.
Water Resources Research,
Journal Year:
2022,
Volume and Issue:
58(4)
Published: April 1, 2022
In
spite
of
the
prevalence
temporary
rivers
over
a
wide
range
climatic
conditions,
they
represent
relatively
understudied
fraction
global
river
network.
Here,
we
exploit
well-established
hydrological
model
and
derived
distribution
approach
to
develop
coupled
probabilistic
description
for
dynamics
catchment
discharge
corresponding
active
network
length.
Analytical
expressions
flow
duration
curve
(FDC)
stream
length
(SLDC)
were
used
provide
consistent
classification
streamflow
regimes
in
rivers.
Two
distinct
(persistent
erratic)
three
different
types
(ephemeral,
perennial,
ephemeral
de
facto)
identified
depending
on
value
two
dimensionless
parameters.
These
key
parameters,
which
are
related
underlying
fluctuations
sensitivity
changes
(here
quantified
by
scaling
exponent
b),
originate
seven
behavioral
classes
characterized
contrasting
shapes
SLDCs
FDCs.
The
analytical
was
tested
using
data
gathered
study
catchments
located
Italy
USA,
with
satisfactory
performances
most
cases.
Our
empirical
results
show
existence
structural
relationship
between
regimes,
is
chiefly
modulated
b.
proposed
framework
represents
promising
tool
analysis
streams.
Water Resources Research,
Journal Year:
2023,
Volume and Issue:
59(9)
Published: Aug. 16, 2023
Abstract
Growth
and
contraction
of
headwater
stream
networks
determine
habitat
extent,
open
a
window
to
the
hyporheic
zone.
A
fundamental
challenge
is
observation
this
process:
wetted
channel
extent
dynamic
in
space
time,
with
length
varying
by
orders
magnitude
over
course
single
storm
event
catchments.
To
date,
observational
data
sets
are
produced
from
boots‐on‐the‐ground
campaigns,
drone
imaging,
or
flow
presence
sensors,
which
often
laborious
limited
their
spatial
temporal
extents.
Here,
we
evaluate
satellite
imagery
as
means
detect
via
machine
learning
methods
trained
on
local
surveys
extent.
Even
where
features
smaller
than
imagery's
resolution,
surface
water
may
be
imprinted
upon
spectral
signature
an
individual
pixel.
For
two
catchments
northern
California
minimal
riparian
canopy
cover
highly
train
random
forest
model
RapidEye
captured
contemporaneously
existing
predict
(accuracy
>91%).
The
used
produce
length‐discharge
(L‐Q)
relations
calculate
spatially
distributed
estimates
capacity
exchange.
sharp
break
occurs
main
stem
channels
lower
order
tributaries,
resulting
stepped
L‐Q
relationship
that
cannot
traditionally
power
law
models.
Remotely
sensed
powerful
tool
for
mapping
at
high
resolution.