Journal of Hydrology X,
Journal Year:
2022,
Volume and Issue:
17, P. 100138 - 100138
Published: Oct. 20, 2022
The
presence
of
year-round
surface
water
in
streams
(i.e.,
streamflow
permanence)
is
an
important
factor
for
identifying
aquatic
habitat
availability,
determining
the
regulatory
status
streams,
managing
land
use
change,
allocating
resources,
and
designing
scientific
studies.
However,
accurate,
high
resolution,
dynamic
prediction
permanence
that
accounts
year-to-year
variability
at
a
regional
extent
major
gap
modeling
capability.
Herein,
we
expand
adapt
U.S.
Geological
Survey
(USGS)
PRObability
Streamflow
PERmanence
(PROSPER)
model
from
its
original
implementation
Pacific
Northwest
(PROSPERPNW)
to
upper
Missouri
River
basin
(PROSPERUM),
geographical
region
includes
mountain
prairie
ecosystems
northern
United
States.
PROSPERUM
empirical
used
estimate
probability
stream
channel
has
flow
response
climatic
conditions
(monthly
annual)
static
physiographic
predictor
variables
upstream
basin.
structure
approach
are
generally
consistent
with
PROSPERPNW
but
include
improved
spatial
resolution
(10
m)
longer
period.
Average
accuracy
was
81
%.
Drainage
area,
proportion
as
wetlands,
developed
cover
were
most
variables.
identifies
decreases
during
climatically
drier
years,
although
there
magnitude
across
basins
highlighting
geographically
varying
sensitivity
drought.
Variability
perennial
drought
among
study
area
also
observed.
Abstract
Non‐perennial
rivers
and
streams
are
ubiquitous
on
our
planet.
Although
several
metrics
have
been
used
to
statistically
group
or
compare
streamflow
characteristics,
there
is
currently
no
widely
definition
of
how
many
days
over
what
reach
length
surface
flow
must
cease
in
order
classify
a
river
as
non‐perennial.
At
the
same
time,
breadth
climate
geographic
settings
for
non‐perennial
leads
diversity
their
regimes,
such
often
quickly
they
go
dry.
These
rich
expanding
body
literature
addressing
ecologic
geomorphic
features,
but
said
be
ignored
by
hydrologists.
Yet
much
we
do
know
about
hydrology
terms
generation
processes,
water
losses,
variability
flow.
We
also
that
while
prevalent
arid
regions,
occur
across
all
types
experience
diverse
set
natural
anthropogenic
controls
streamflow.
Furthermore,
measuring
modeling
these
presents
distinct
challenges,
research
directions,
which
still
require
further
attention.
Therefore,
present
an
overview
current
understanding,
methodologic
knowledge
gaps,
directions
hydrologic
understanding
rivers;
critical
topics
light
both
growing
global
scarcity
ever‐changing
laws
policies
dictate
whether
environmental
protection
receive.
This
article
categorized
under:
Science
Water
>
Hydrological Processes,
Journal Year:
2019,
Volume and Issue:
33(24), P. 3056 - 3069
Published: July 26, 2019
Abstract
Solute
concentrations
in
streamflow
typically
vary
systematically
with
stream
discharge,
and
the
resulting
concentration–discharge
relationships
are
important
signatures
of
catchment
biogeochemical
processes.
Solutes
derived
from
mineral
weathering
often
exhibit
decreasing
increasing
flows,
suggesting
dilution
a
kinetically
limited
flux
by
variable
water.
However,
previous
work
showed
that
weathering‐derived
solutes
59
headwater
catchments
were
much
weaker
than
this
simple
model
would
predict.
Instead,
behaved
as
chemostats,
rates
solute
production
and/or
mobilization
nearly
proportional
to
water
fluxes,
on
both
event
interannual
timescales.
Here,
we
re‐examine
these
findings
using
data
for
wider
range
2,186
catchments,
ranging
~10
>1,000,000
km
2
drainage
area
spanning
wide
lithologic
climatic
settings.
Concentration–discharge
among
larger
set
broadly
consistent
previously
described
chemostatic
behaviour,
at
least
timescales
solutes.
Among
same
however,
site‐to‐site
variations
mean
strong
negative
correlations
long‐term
average
precipitation
reflecting
control
leaching
critical
zone.
We
use
multiple
regression
site
characteristics
including
discharge
identify
potential
controls
find
land
cover
significant
predictors
many
analytes.
The
picture
emerges
is
one
which,
timescales,
chemostatically
buffered
groundwater
storage
fast
chemical
reactions,
but
each
catchment's
“set
point”
reflects
differences
climatically
driven
evolution
In
contrast
products,
some
nutrients
particulates
near‐chemostatic
across
all
their
correlate
more
strongly
characteristics.
Geophysical Research Letters,
Journal Year:
2021,
Volume and Issue:
48(2)
Published: Jan. 26, 2021
Abstract
Over
half
of
global
rivers
and
streams
lack
perennial
flow,
understanding
the
distribution
drivers
their
flow
regimes
is
critical
for
hydrologic,
biogeochemical,
ecological
functions.
We
analyzed
nonperennial
using
540
U.S.
Geological
Survey
watersheds
across
contiguous
United
States
from
1979
to
2018.
Multivariate
analyses
revealed
regional
differences
in
no‐flow
fraction,
date
first
no
duration
dry‐down
period,
with
further
divergence
between
natural
human‐altered
watersheds.
Aridity
was
a
primary
driver
metrics
at
continental
scale,
while
unique
combinations
climatic,
physiographic
anthropogenic
emerged
scales.
Dry‐down
showed
stronger
associations
nonclimate
compared
fraction
timing.
Although
sparse
gages
limits
our
such
streams,
examined
here
suggest
important
role
aridity
land
cover
change
modulating
future
stream
drying.
Abstract
Intermittent
rivers
and
ephemeral
streams
(IRES)
are
now
recognized
to
support
specific
freshwater
biodiversity
ecosystem
services
represent
approximately
half
of
the
global
river
network,
a
fraction
that
is
likely
increase
in
context
changes.
Despite
large
research
efforts
on
IRES
during
past
few
decades,
there
need
for
developing
systemic
approach
considers
their
hydrological,
hydrogeological,
hydraulic,
ecological,
biogeochemical
properties
processes,
as
well
interactions
with
human
societies.
Thus,
we
assert
interdisciplinary
promoted
by
critical
zone
sciences
socio‐ecology
relevant.
These
approaches
rely
infrastructure—Critical
Zone
Observatories
(CZO)
Long‐Term
Socio‐Ecological
Research
(LTSER)
platforms—that
representative
diversity
(e.g.,
among
climates
or
types
geology.
We
illustrate
this
within
French
CZO
LTSER,
including
socio‐ecosystems,
detail
IRES.
networks
also
specialized
long‐term
observations
required
detect
measure
responses
climate
forcings
despite
delay
buffering
effects
ecosystems.
The
LTSER
platforms
development
innovative
techniques
data
analysis
methods
can
improve
characterization
IRES,
particular
monitoring
flow
regimes,
groundwater‐surface
water
flow,
biogeochemistry
rewetting.
provide
scientific
methodological
perspectives
which
its
associated
infrastructure
would
relevant
original
insights
help
fill
knowledge
gaps
about
This
article
categorized
under:
Water
Life
>
Stresses
Pressures
Ecosystems
Science
Hydrological
Processes
Conservation,
Management,
Awareness
Biological reviews/Biological reviews of the Cambridge Philosophical Society,
Journal Year:
2021,
Volume and Issue:
97(2), P. 481 - 504
Published: Nov. 10, 2021
ABSTRACT
Landscape
perspectives
in
riverine
ecology
have
been
undertaken
increasingly
the
last
30
years,
leading
aquatic
ecologists
to
develop
a
diverse
set
of
approaches
for
conceptualizing,
mapping
and
understanding
‘riverscapes’.
Spatiotemporally
explicit
rivers
their
biota
nested
within
socio‐ecological
landscape
now
provide
guiding
principles
inland
fisheries
watershed
management.
During
two
decades,
scientific
literature
on
riverscapes
has
increased
rapidly,
indicating
that
term
associated
are
serving
an
important
purpose
freshwater
science
We
trace
origins
theoretical
foundations
riverscape
examine
trends
published
assess
state
demonstrate
how
they
being
applied
address
recent
challenges
management
ecosystems.
focus
studying
visualizing
streams
with
remote
sensing,
modelling
sampling
designs
enable
pattern
detection
as
seen
from
above
(e.g.
river
channel,
floodplain,
riparian
areas)
but
also
into
water
itself
organisms
aqueous
environment).
Key
concepts
central
heterogeneity,
scale
(resolution,
extent
scope)
connectivity
(structural
functional),
which
underpin
spatial
temporal
aspects
study
design,
data
collection
analysis.
Mapping
physical
biological
characteristics
floodplains
high‐resolution,
spatially
intensive
techniques
improves
causes
ecological
consequences
patterns
at
multiple
scales.
This
information
is
crucial
managing
ecosystems,
especially
successful
implementation
conservation,
restoration
monitoring
programs.
Recent
advances
field‐sampling
geospatial
technology
making
it
feasible
collect
high‐resolution
over
larger
scales
space
time.
highlight
opportunities
discuss
future
avenues
research
emerging
tools
can
potentially
help
overcome
obstacles
collecting,
analysing
displaying
these
data.
synthesis
intended
researchers
resource
managers
understand
apply
real‐world
problems
Hydrological Processes,
Journal Year:
2020,
Volume and Issue:
34(26), P. 5704 - 5711
Published: Nov. 18, 2020
It
has
been
12
years
since
Bishop
et
al.
(2008)
wrote
the
Invited
Commentary
"Aqua
Incognita:
unknown
headwaters".They
highlighted
that
"In
most
regions,
overwhelming
majority
of
stream
length
lies
beyond
frontiers
any
systematic
documentation
and
would
have
to
be
represented
as
a
blank
space
on
assessment
map.This
means
for
streams
support
aquatic
life,
understanding
is
lacking
water
quality,
habitat,
biota,
specific
discharge,
or
even
how
many
kilometers
such
are
there.This
so
vast
it
deserves
name
help
us
at
least
remember
there.We
propose
calling
'Aqua
Incognita'"
(Bishop
al.,
2008;
p.
1239).We
continue
agree
with
this
statement
need
understand
headwater
better.In
commentary,
we
want
draw
attention
particular
type
less
frequently
examined:
flow
intermittently,
i.e.,
Aqua
Temporaria
Incognita.Question
3
23
unsolved
problems
in
hydrology
(Blöschl
2019)
focuses
ephemeral
dryland
streams.We
argue
focus
needs
broadening
temporary
because
they
ubiquitous
all
climates.Headwater
feed
larger
perennial
particularly
sensitive
climate
change
other
human
influences
(Jaeger
2014;Reynolds
2015;Pumo
2016).Their
effective
management
protection,
therefore,
requires
an
both
natural
artificial
causes
intermittence.Temporary
among
hydrologically
variable
systems
(Wohl,
2017).They
include
intermittent
seasonally,
only
response
rainfall
snowmelt
events,
episodic
contain
flowing
during
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.
Science Advances,
Journal Year:
2023,
Volume and Issue:
9(3)
Published: Jan. 18, 2023
The
riverine
dissolved
organic
carbon
(DOC)
flux
is
of
similar
magnitude
to
the
terrestrial
sink
for
atmospheric
CO2,
but
factors
controlling
it
remain
poorly
determined
and
are
largely
absent
from
Earth
system
models
(ESMs).
Here,
we
show,
a
range
European
headwater
catchments,
that
electrolyte
solubility
theory
explains
how
declining
precipitation
ionic
strength
(IS)
has
increased
dissolution
thermally
moderated
pools
soluble
soil
matter
(OM),
while
hydrological
conditions
govern
proportion
this
OM
entering
aquatic
system.
Solubility
will
continue
rise
exponentially
with
IS
until
pollutant
ion
deposition
fully
flattens
out
under
clean
air
policies.
Future
DOC
export
increasingly
depend
on
rates
warming
any
directional
changes
intensity
seasonality
marine
deposition.
Our
findings
provide
firm
foundation
incorporating
processes
dominating
change
in
component
global
cycle
ESMs.
npj Biodiversity,
Journal Year:
2024,
Volume and Issue:
3(1)
Published: Feb. 7, 2024
Rivers
are
an
important
component
of
the
global
carbon
cycle
and
contribute
to
atmospheric
exchange
disproportionately
their
total
surface
area.
Largely,
this
is
because
rivers
efficiently
mobilize,
transport
metabolize
terrigenous
organic
matter
(OM).
Notably,
our
knowledge
about
magnitude
globally
relevant
fluxes
strongly
contrasts
with
lack
understanding
underlying
processes
that
transform
OM.
Ultimately,
OM
processing
en
route
oceans
results
from
a
diverse
assemblage
consumers
interacting
equally
pool
resources
in
spatially
complex
network
heterogeneous
riverine
habitats.
To
understand
interaction
between
OM,
we
must
therefore
account
for
spatial
configuration,
connectivity,
landscape
context
at
scales
ranging
local
ecosystems
entire
networks.
Building
such
explicit
framework
fluvial
across
may
also
help
us
better
predict
poorly
understood
anthropogenic
impacts
on
cycling,
instance
human-induced
fragmentation
changes
flow
regimes,
including
intermittence.
Moreover,
current
unprecedented
human-driven
loss
biodiversity.
This
least
partly
due
mechanisms
operating
scales,
as
interference
migration
habitat
homogenization,
comes
largely
unknown
functional
consequences.
We
advocate
here
comprehensive
networks
connecting
two
aware
but
disparate
lines
research
(i)
metacommunities
biodiversity,
(ii)
biogeochemistry
contribution
cycle.
argue
agenda
focusing
regional
scale-that
is,
river
network-to
enable
deeper
mechanistic
naturally
arising
biodiversity-ecosystem
functioning
coupling
major
driver
biogeochemically
fluxes.