Abstract.
Improving
the
consistency
of
hydrological
models,
i.e.
their
ability
to
reproduce
observed
system
dynamics,
is
required
increase
predictive
power.
As
use
streamflow
data
for
calibration
necessary
but
not
sufficient
constrain
model
and
warrant
consistency,
other
strategies
must
be
considered,
in
particular
additional
sources.
The
aim
this
study
test
whether
simultaneous
dissolved
organic
carbon
(DOC)
nitrate
(NO3-)
concentrations
along
with
improves
a
parsimonious
solute-transport
model.
A
multi-objective
multi-variable
approach
was
used
evaluate
an
intensive
agricultural
headwater
catchment.
Our
results
showed
that
using
daily
stream
DOC
NO3-
together
during
did
improve
model's
accurately
predict
or
evaluation
periods.
However,
internal
improved
simulation
low
flows,
groundwater
storage
upstream
soil
storage,
riparian
storage.
Parameter
uncertainty
decreased
when
calibrated
solute
concentrations,
except
parameters
related
fast
slow
reservoir
flow.
This
shows
added
value
multiple
sources
addition
calibration,
models
better
representation
states
With
increasing
availability
from
catchment
monitoring,
provides
objective
way
can
confidence
scenario
evaluation.
The Science of The Total Environment,
Journal Year:
2022,
Volume and Issue:
849, P. 157398 - 157398
Published: July 21, 2022
Dissolved
organic
carbon
(DOC)
in
surface
waters
is
an
important
component
of
the
boreal
landscape
budget
and
a
critical
variable
water
quality.
A
dominant
terrestrial
DOC
source
riparian
zone.
These
near
stream
areas
play
key
role
regulating
transport
between
land
aquatic
ecosystems.
The
groundwater
dynamics
at
this
interface
have
been
considered
major
controlling
for
export
to
streams.
This
study
focuses
on
levels
mean
travel
times
(MTT)
concentrations
and,
subsequently,
DOC.
done
by
comparing
them
as
explanatory
variables
capture
spatial
intra-annual
variability
We
used
physically
based
3D
hydrological
model,
Mike
SHE,
simulate
zones
14
sub-catchments
within
Krycklan
catchment
(Sweden).
model
concept
assumes
that
will
be
higher
moving
through
shallow
flow
paths.
In
can
linked
position
table
point
observation
or
time,
which
generally
shorter
has
travelled
more
conductive
soil
layers.
compared
results
with
both
observed
concentrations.
analysis
revealed
correlation
modelled
annual
averages
increased
from
r
=
0.08
0.87
using
MTT
instead
level.
also
better
captured
successfully
represented
seasonal
We,
therefore,
suggest
predictor
than
level
concentration
because
it
greater
variety
heterogeneities,
such
variation
properties,
size,
input
deep
sources.
Hydrology and earth system sciences,
Journal Year:
2023,
Volume and Issue:
27(16), P. 3083 - 3114
Published: Aug. 24, 2023
Abstract.
Stable
isotopes
(δ18O)
and
tritium
(3H)
are
frequently
used
as
tracers
in
environmental
sciences
to
estimate
age
distributions
of
water.
However,
it
has
previously
been
argued
that
seasonally
variable
tracers,
such
δ18O,
generally
systematically
fail
detect
the
tails
water
therefore
substantially
underestimate
ages
compared
radioactive
3H.
In
this
study
for
Neckar
River
basin
central
Europe
based
on
a
>20-year
record
hydrological,
δ18O
3H
data,
we
scrutinized
above
postulate
together
with
potential
role
spatial
aggregation
effects
exacerbating
underestimation
ages.
This
was
done
by
comparing
inferred
from
total
21
different
model
implementations,
including
time-invariant,
lumped-parameter
sine-wave
(SW)
convolution
integral
(CO)
models
well
StorAge
Selection
(SAS)-function
(P-SAS)
integrated
hydrological
combination
SAS
functions
(IM-SAS).
We
found
that,
indeed,
commonly
SW
CO
mean
transit
times
(MTTs)
∼
1–2
years
lower
than
those
obtained
same
models,
reaching
MTTs
∼10
years.
contrast,
several
implementations
P-SAS
IM-SAS
not
only
allowed
simultaneous
representations
storage
variations
streamflow
stream
signals,
but
these
were,
11–17
years,
also
much
higher
similar
3H,
which
suggested
11–13
Characterized
parameter
posterior
distributions,
particular
parameters
control
age,
individually
constrained
or
observations
exhibited
limited
differences
magnitudes
parts
temporal
variability
time
(TTDs)
response
changing
wetness
conditions.
suggests
both
lead
comparable
descriptions
how
is
routed
through
system.
These
findings
provide
evidence
us
reject
hypothesis
tracer
“cannot
see
older
about
4
years”
truncates
corresponding
leading
underestimations
Instead,
our
results
broad
equivalence
systems
characterized
at
least
15–20
The
question
degree
heterogeneity
can
further
adversely
affect
estimates
remains
unresolved
lumped
distributed
provided
inconclusive
results.
Overall,
demonstrates
reported
most
likely
result
use
other
per
se.
Rather,
largely
be
attributed
choices
approaches
complexity
considering
transient
conditions
next
aspects.
Given
additional
vulnerability
due
potentially
still
unknown
effects,
advocate
avoiding
type
if
possible
instead
adopting
SAS-based
time-variant
formulations
models.
ABSTRACT
During
the
last
decade,
tracer‐aided
hydrological
models
(TAMs)
have
been
applied
in
numerous
studies
and
successfully
evolved
for
different
purposes.
Such
confirmed
value
of
tracer
data
modeling,
offering
insights
into
internal
storages,
water
sources,
flow
pathways,
mixing
processes,
ages,
which
cannot
be
derived
from
hydrometric
alone.
The
direct
coupling
tracers
flux
tracking
balance
can
reduce
model
uncertainty
through
increased
biogeochemical
process
knowledge.
More
specifically,
such
simultaneously
capture
celerity
responses
with
velocities
(and
age)
particles.
As
a
result
availability
high‐resolution
characterizing
functioning
across
Critical
Zone
entire
landscapes,
together
rapid
improvement
computing
capacity,
four
major
advances
reshaped
capability
TAMs,
we
review
this
paper:
(1)
enhanced
representation
spatial
heterogeneity,
(2)
more
explicit
conceptualization
ecohydrological
partitioning,
(3)
application
to
larger
catchment
scales,
(4)
incorporation
non‐conservative
coupled
quality
modeling.
However,
persistent
challenges
also
emerged,
particularly
relation
acquisition,
mismatches
between
information
content
scale
application,
uncertainties
structures,
as
well
adaptation
multi‐criteria
calibration.
In
review,
recent
remaining
TAMs
summarized
discussed
particular
focus
on
conservative
models.
Global Change Biology,
Journal Year:
2020,
Volume and Issue:
26(10), P. 5899 - 5913
Published: July 20, 2020
Abstract
The
magnitude
of
the
terrestrial
carbon
(C)
sink
may
be
overestimated
globally
due
to
difficulty
accounting
for
all
C
losses
across
heterogeneous
landscapes.
More
complete
assessments
net
landscape
balances
(NLCB)
are
needed
that
integrate
both
emissions
by
fire
and
transfer
aquatic
systems,
two
key
loss
pathways
C.
These
can
particularly
significant
in
wet–dry
tropics,
where
plays
a
fundamental
part
ecosystems
intense
rainfall
seasonal
flooding
result
considerable
export
(ΣF
aq
).
Here,
we
determined
NLCB
lowland
catchment
(~140
km
2
)
tropical
Australia
over
years
evaluating
productivity
(NEP),
fire‐related
ΣF
(comprising
downstream
transport
gaseous
evasion)
main
components,
is,
savanna
woodland
wetlands.
We
found
was
large
(NLCB
334
Mg
−2
year
−1
),
wetland
areas
contributed
84%
16%
this
sink,
respectively.
Annually,
(−56
(−28
reduced
NEP
13%
7%,
Savanna
burning
shifted
source
several
months
during
dry
season,
while
significantly
offset
wet
with
disproportionate
contribution
single
major
monsoonal
events—up
39%
annual
exported
one
event.
hypothesize
wetter
hotter
conditions
tropics
future
will
increase
emissions,
potentially
further
reducing
current
region.
long‐term
studies
upscale
first
estimate
less
productive,
yet
hydrologically
dynamic
regions
our
indicating
not
hold.
Frontiers in Earth Science,
Journal Year:
2020,
Volume and Issue:
8
Published: Nov. 6, 2020
Tropical
regions
cover
approximately
36%
of
the
Earth's
landmass.
These
are
home
to
40%
world's
population,
which
is
projected
increase
over
50%
by
2030
under
a
remarkable
climate
variability
scenario
often
exacerbated
El
Niño
Southern
Oscillation
(ENSO)
and
other
teleconnections.
In
tropics,
ecohydrological
conditions
typically
influence
complex
land-ocean-atmosphere
interactions
that
produce
dynamic
cycling
mass
energy
reflected
in
clear
partition
water
fluxes.
Here,
we
present
review
seven
years
concerted
continuous
stable
isotope
monitoring
across
Costa
Rica,
including
key
insights
learned,
main
methodological
advances
limitations
(both
experimental
designs
data
analysis),
potential
gaps,
future
research
opportunities
with
humid
tropical
perspective.
The
uniqueness
geographic
location
Rica
within
mountainous
Central
America
Isthmus,
receiving
moisture
inputs
from
Caribbean
Sea
(windward)
Pacific
Ocean
(complex
leeward
topography),
experiencing
strong
ENSO
events,
poses
advantage
for
use
isotopic
variations
underpin
drivers
responses.
sequential
approach,
analyzed
transport,
rainfall
generation,
groundwater/surface
connectivity
Bayesian
rainfall-runoff
modeling.
overarching
goal
this
provide
robust
example
progressive
escalation
common
observations
more
modeling
outputs
applications
enhance
resource
management
tropics.
Global Change Biology,
Journal Year:
2021,
Volume and Issue:
28(7), P. 2360 - 2380
Published: Dec. 2, 2021
Despite
their
size
and
contribution
to
the
global
carbon
cycle,
we
have
limited
understanding
of
tropical
savannas
current
trajectory
with
climate
change
anthropogenic
pressures.
Here
examined
interannual
variability
externally
forced
long-term
changes
in
water
exchange
from
a
high
rainfall
savanna
site
seasonal
tropics
north
Australia.
We
used
an
18-year
flux
data
time
series
(2001-2019)
detect
trends
drivers
fluxes
water.
Significant
positive
gross
primary
productivity
(GPP,
15.4
g
C
m2
year-2
),
ecosystem
respiration
(Reco
,
8.0
net
(NEE,
7.4
)
use
efficiency
(WUE,
0.0077
kg
H2
O-1
year-1
were
computed.
There
was
weaker,
non-significant
trend
latent
energy
(LE,
0.34
W
m-2
).
Rainfall
nearby
increased
statistically
over
45-year
period
during
observation
period.
To
examine
dominant
GPP
WUE,
random
forest
approach
terrestrial
biosphere
model
conduct
attribution
experiment.
Radiant
driver
wet
season
fluxes,
whereas
soil
content
dominated
dry
fluxes.
The
suggested
that
[CO2
],
precipitation
Tair
accounting
for
90%
modelled
WUE.
Positive
largest
implying
tree
components
larger
contributor
than
grassy
understorey.
Fluxes
environmental
not
significant
season,
when
grasses
are
active.
is
potentially
still
recovering
cyclone
45
years
ago
regrowth
this
event
may
also
be
contributing
observed
sequestration,
highlighting
need
understand
sub-diurnal
decadal
scales.
Hydrology and earth system sciences,
Journal Year:
2025,
Volume and Issue:
29(1), P. 127 - 158
Published: Jan. 14, 2025
Abstract.
The
consistency
of
hydrological
models,
i.e.
their
ability
to
reproduce
observed
system
dynamics,
needs
be
improved
increase
predictive
power.
As
using
streamflow
data
alone
calibrate
models
is
not
sufficient
constrain
them
and
render
consistent,
other
strategies
must
considered,
in
particular
additional
types
data.
aim
this
study
was
test
whether
simultaneous
calibration
dissolved
organic
carbon
(DOC)
nitrate
(NO3-)
concentrations
along
with
the
a
parsimonious
solute-transport
model.
A
multi-objective
approach
four
scenarios
used
evaluate
model's
predictions
for
an
intensive
agricultural
headwater
catchment.
After
calibration,
model
reasonably
simultaneously
reproduced
dynamics
discharge
DOC
NO3-
stream
catchment
from
2008–2016.
Evaluation
independent
datasets
indicated
that
usually
groundwater
level
soil
moisture
upslope
riparian
zones
correctly
all
scenarios.
Using
daily
did
improve
its
predict
or
evaluation
periods.
significantly
representation
storage
lesser
extent
zone
but
zone.
Parameter
uncertainty
decreased
when
calibrated
solute
concentrations,
except
parameters
related
fast
slow
reservoir
flow.
This
shows
added
value
multiple
streamflow,
internal
states
flows.
With
increasing
availability
monitoring,
provides
objective
way
can
confidence
Hydrological Processes,
Journal Year:
2025,
Volume and Issue:
39(4)
Published: April 1, 2025
ABSTRACT
The
tracer‐aided
modelling
has
gained
widespread
attention
in
recent
years
as
a
crucial
approach
for
investigating
watershed
hydrological
functions.
However,
errors
model
inputs,
such
precipitation,
evapotranspiration
(ET)
and
isotopes
can
lead
to
uncertainty
physically
meaningful
parameters,
which,
turn,
affects
the
accurate
depiction
of
In
this
study,
we
focused
on
Hemuqiao
watershed,
typical
humid
mountainous
region
southeast
China,
equipped
with
intensive
isotopic
monitoring.
Two
Reservoirs
StorAge
Selection
(TRSAS)
was
adopted
explore
impact
input
data
understanding
connectivity
preferential
flow.
results
show
that
observation
precipitation
ET
do
not
significantly
reduce
performance
(with
optimal
NSE
value
decreasing
by
up
0.05).
they
increase
simulation
primarily
due
associated
large
events.
contrast,
observed
particularly
during
extreme
events,
meanwhile
significant
differences
some
parameters
compared
no
error
data.
Although
proportion
young
water
fraction
streamflow
does
noticeable
difference,
proportions
lateral
subsurface
flow
tend
be
overestimated
(i.e.,
approximately
0.14
0.08,
respectively,
average
over
long
term).
This
an
overestimation
between
soil
streamflow.
These
findings
suggest
models,
improving
accuracy
is
more
critical
accurately
processes
than
enhancing
spatial
observations
ET.