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.
Environmental Research Letters,
Journal Year:
2021,
Volume and Issue:
16(8), P. 084033 - 084033
Published: July 29, 2021
Abstract
Non-perennial
streams
are
widespread,
critical
to
ecosystems
and
society,
the
subject
of
ongoing
policy
debate.
Prior
large-scale
research
on
stream
intermittency
has
been
based
long-term
averages,
generally
using
annually
aggregated
data
characterize
a
highly
variable
process.
As
result,
it
is
not
well
understood
if,
how,
or
why
hydrology
non-perennial
changing.
Here,
we
investigate
trends
drivers
three
signatures
that
describe
duration,
timing,
dry-down
period
across
continental
United
States
(CONUS).
Half
gages
exhibited
significant
trend
through
time
in
at
least
one
signatures,
changes
no-flow
duration
were
most
pervasive
(41%
gages).
Changes
substantial
for
many
streams,
7%
annual
exceeding
100
days
during
study
period.
Distinct
regional
patterns
change
evident,
with
widespread
drying
southern
CONUS
wetting
northern
CONUS.
These
correlated
aridity,
though
spatiotemporal
variability
diverse
signatures.
While
timing
strongly
related
climate,
was
watershed
land
use
physiography.
Our
results
indicate
conditions
increasing
prevalence
over
much
binary
classifications
‘perennial’
‘non-perennial’
an
accurate
reflection
this
change.
Water
management
should
reflect
changing
nature
both
today
future.
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.
Earth system science data,
Journal Year:
2022,
Volume and Issue:
14(10), P. 4525 - 4550
Published: Oct. 17, 2022
Abstract.
The
geographic
distribution
of
streams
and
rivers
drives
a
multitude
patterns
processes
in
hydrology,
geomorphology,
geography,
ecology.
Therefore,
hydrographic
network
that
accurately
delineates
both
small
large
rivers,
along
with
their
topographic
topological
properties,
equal
precision
would
be
indispensable
the
earth
sciences.
Currently,
available
global
hydrographies
do
not
feature
headwater
great
detail.
However,
these
headwaters
are
vital
because
they
estimated
to
contribute
more
than
70
%
overall
stream
length.
We
aimed
fill
this
gap
by
using
MERIT
Hydro
digital
elevation
model
at
3
arcsec
(∼90
m
Equator)
derive
globally
seamless,
standardised
network,
“Hydrography90m”,
corresponding
information.
A
central
is
minimal
upstream
contributing
area,
i.e.
flow
accumulation,
0.05
km2
(or
5
ha)
initiate
channel,
which
allowed
us
extract
channels
By
employing
suite
GRASS
GIS
hydrological
modules,
we
calculated
range-wide
accumulation
direction
delineate
total
1.6
million
drainage
basins
extracted
726
unique
segments
sub-catchments.
In
addition,
computed
variables
comprising
slope,
gradient,
length,
curvature
attributes
as
well
allow
for
routing
various
order
classifications.
validated
spatial
accuracy
Hydrography90m
against
NHDPlus
HR,
an
independent,
national
high-resolution
dataset
United
States.
Our
validation
shows
newly
developed
has
highest
contains
compared
three
other
datasets.
This
comprehensive
approach
provides
long-overdue
baseline
assessing
actual
streamflow
opens
new
research
avenues
studies
surface
water
worldwide.
thus
offers
significant
potential
facilitate
assessment
freshwater
quantity
quality,
inundation
risk,
biodiversity,
conservation,
resource
management
objectives
manner.
layers
https://doi.org/10.18728/igb-fred-762.1
(Amatulli
et
al.,
2022a),
while
can
used
directly
standard
applications,
recommend
seamless
integration
modules
open-source
QGIS
software
further
customise
data
optimal
utility
from
it.
Ecosystems,
Journal Year:
2022,
Volume and Issue:
26(1), P. 1 - 28
Published: Feb. 7, 2022
Watershed
resilience
is
the
ability
of
a
watershed
to
maintain
its
characteristic
system
state
while
concurrently
resisting,
adapting
to,
and
reorganizing
after
hydrological
(for
example,
drought,
flooding)
or
biogeochemical
excessive
nutrient)
disturbances.
Vulnerable
waters
include
non-floodplain
wetlands
headwater
streams,
abundant
components
representing
most
distal
extent
freshwater
aquatic
network.
are
hydrologically
dynamic
biogeochemically
reactive
systems,
storing,
processing,
releasing
water
entrained
(that
is,
dissolved
particulate)
materials
along
expanding
contracting
networks.
The
functions
emerging
from
these
processes
affect
magnitude,
frequency,
timing,
duration,
storage,
rate
change
material
energy
fluxes
among
downstream
waters,
thereby
maintaining
states
imparting
resilience.
We
present
here
conceptual
framework
for
understanding
how
vulnerable
confer
demonstrate
individual
cumulative
vulnerable-water
modifications
reduced
extent,
altered
connectivity)
watershed-scale
disturbance
response
recovery,
which
decreases
can
trigger
transitions
across
thresholds
alternative
conducive
increased
flood
frequency
nutrient
concentrations).
subsequently
describe
resilient
watersheds
require
spatial
heterogeneity
temporal
variability
in
interactions
between
terrestrial
systems
down-gradient
necessitates
attention
conservation
restoration
their
connectivity
gradients.
To
conclude,
we
provide
actionable
principles
articulate
research
needs
further
science
management.
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.
Nature Water,
Journal Year:
2025,
Volume and Issue:
unknown
Published: March 31, 2025
Abstract
To
manage
water
resources
and
forecast
river
flows,
hydrologists
seek
to
understand
how
moves
from
precipitation,
through
watersheds,
into
channels.
However,
we
lack
fundamental
information
on
the
spatial
distribution
physical
controls
global
hydrologic
processes.
This
is
needed
provide
theoretical
support
for
large-domain
model
simulations.
Here,
address
this
issue,
present
a
global,
searchable
database
of
400
research
watersheds
with
published
descriptions
dominant
flow
pathways.
knowledge
synthesis
approach
leverages
decades
grant
funding,
fieldwork
effort
local
expertise.
We
use
test
longstanding
hypotheses
about
roles
climate,
biomes
landforms
in
controlling
show
that
aridity
predicts
depth
pathways
terrain
predict
prevalence
lateral
These
new
data
search
capabilities
efficient
hypothesis
testing
investigate
emergent
patterns
relate
landscape
organization
function.
Freshwater Science,
Journal Year:
2022,
Volume and Issue:
41(2), P. 167 - 182
Published: March 25, 2022
Nonperennial
streams
dominate
global
river
networks
and
are
increasing
in
occurrence
across
space
time.
When
surface
flow
ceases
or
the
water
dries,
moisture
can
be
retained
subsurface
sediments
of
hyporheic
zone,
supporting
aquatic
communities
ecosystem
processes.
However,
hydrological
ecological
definitions
zone
have
been
developed
perennial
rivers
emphasize
mixing
organisms
from
both
stream
groundwater.
The
adaptation
such
to
include
humid
dry
unsaturated
conditions
could
promote
characterization
how
biogeochemical
variability
shape
within
nonperennial
zones,
advancing
our
understanding
structure
function
these
habitats.
To
conceptualize
zones
for
streams,
we
review
sources
influence
physicochemical
conditions.
We
consider
extent
this
biogeochemistry
ecology
might
vary
with
states.
then
link
components
composition
communities.
Next,
examine
literature
identify
priorities
research
exploring
zones.
Lastly,
by
integrating
hydrology,
biogeochemistry,
ecology,
recommend
a
multidisciplinary
conceptualization
as
porous
streambed
that
shift
between
lotic,
lentic,
humid,
time
support
aquatic–terrestrial
biodiversity.
As
drying
increases
because
change,
call
holistic,
interdisciplinary
terrestrial
sciences
apply
characterize
full
spectrum