Water Resources Research,
Journal Year:
2024,
Volume and Issue:
60(12)
Published: Dec. 1, 2024
Abstract
Artificial
intelligence
(AI)
methods
have
created
insurmountable
performance
in
prediction
tasks
for
geoscientific
problems
yet
are
unable
to
derive
process
insights
and
answer
specific
scientific
questions.
The
geoscience
community
faces
a
dilemma
of
reconciling
comprehension
with
high
predictive
accuracy.
Here
we
introduce
deep
learning
(DPL)
approach
empowering
neural
networks
deduce
intrinsic
processes
from
observable
data,
wherein
the
intuitive
physics
geosystems
is
directly
coupled
within
(DL)
architecture
as
structural
prior.
We
aim
incorporate
raw
common
concepts
possible
macroscopic
guidance:
on
one
hand,
reduce
interference
DL's
data
adaptability.
On
other
allow
information
flow
model
converge
along
paths
toward
target
output,
thus
enabling
potential
gain
limited
supervision.
Illustrating
its
application
precipitation‐runoff
modeling
across
USA,
DPL
yields
an
ensemble
median
Nash‐Sutcliffe
efficiency
0.758
Kling‐Gupta
0.778
robust
transferability,
compared
0.762
0.751
state‐of‐the‐art
DL
model.
good
match
between
internal
representations
independent
sets
snow
water
equivalent
evapotranspiration,
superior
capability
catchment
budget
closures,
demonstrates
proficient
mastery.
study
also
highlights
beneficial
synergies
large‐scale
collaboration,
promoting
organic
unity
understanding
performance.
This
work
shows
promising
avenue
big
will
benefit
domains
that
remain
concerned
clarity
era
AI.
Earth s Future,
Journal Year:
2024,
Volume and Issue:
12(7)
Published: July 1, 2024
Abstract
Interpretable
Machine
Learning
(IML)
has
rapidly
advanced
in
recent
years,
offering
new
opportunities
to
improve
our
understanding
of
the
complex
Earth
system.
IML
goes
beyond
conventional
machine
learning
by
not
only
making
predictions
but
also
seeking
elucidate
reasoning
behind
those
predictions.
The
combination
predictive
power
and
enhanced
transparency
makes
a
promising
approach
for
uncovering
relationships
data
that
may
be
overlooked
traditional
analysis.
Despite
its
potential,
broader
implications
field
have
yet
fully
appreciated.
Meanwhile,
rapid
proliferation
IML,
still
early
stages,
been
accompanied
instances
careless
application.
In
response
these
challenges,
this
paper
focuses
on
how
can
effectively
appropriately
aid
geoscientists
advancing
process
understanding—areas
are
often
underexplored
more
technical
discussions
IML.
Specifically,
we
identify
pragmatic
application
scenarios
typical
geoscientific
studies,
such
as
quantifying
specific
contexts,
generating
hypotheses
about
potential
mechanisms,
evaluating
process‐based
models.
Moreover,
present
general
practical
workflow
using
address
research
questions.
particular,
several
critical
common
pitfalls
use
lead
misleading
conclusions,
propose
corresponding
good
practices.
Our
goal
is
facilitate
broader,
careful
thoughtful
integration
into
science
research,
positioning
it
valuable
tool
capable
enhancing
current
Water Resources Research,
Journal Year:
2024,
Volume and Issue:
60(4)
Published: April 1, 2024
Abstract
While
deep
learning
(DL)
models
exhibit
superior
simulation
accuracy
over
traditional
distributed
hydrological
(DHMs),
their
main
limitations
lie
in
opacity
and
the
absence
of
underlying
physical
mechanisms.
The
pursuit
synergies
between
DL
DHMs
is
an
engaging
research
domain,
yet
a
definitive
roadmap
remains
elusive.
In
this
study,
novel
framework
that
seamlessly
integrates
process‐based
model
encoded
as
neural
network
(NN),
additional
NN
for
mapping
spatially
physically
meaningful
parameters
from
watershed
attributes,
NN‐based
replacement
representing
inadequately
understood
processes
developed.
Multi‐source
observations
are
used
training
data,
fully
differentiable,
enabling
fast
parameter
tuning
by
backpropagation.
A
hybrid
Amazon
Basin
(∼6
×
10
6
km
2
)
was
established
based
on
framework,
HydroPy,
global‐scale
DHM,
its
backbone.
Trained
simultaneously
with
streamflow
Gravity
Recovery
Climate
Experiment
satellite
yielded
median
Nash‐Sutcliffe
efficiencies
0.83
0.77
dynamic
simulations
total
water
storage,
respectively,
41%
35%
higher
than
those
original
HydroPy
model.
Replacing
Penman‒Monteith
formulation
produces
more
plausible
potential
evapotranspiration
(PET)
estimates,
unravels
spatial
pattern
PET
giant
basin.
parameterization
interpreted
to
identify
factors
controlling
variability
key
parameters.
Overall,
study
lays
out
feasible
technical
modeling
big
data
era.
Science Advances,
Journal Year:
2024,
Volume and Issue:
10(13)
Published: March 27, 2024
Estimating
river
flood
risks
under
climate
change
is
challenging,
largely
due
to
the
interacting
and
combined
influences
of
various
flood-generating
drivers.
However,
a
more
detailed
quantitative
analysis
such
compounding
effects
implications
their
interplay
remains
underexplored
on
large
scale.
Here,
we
use
explainable
machine
learning
disentangle
between
drivers
quantify
importance
for
different
magnitudes
across
thousands
catchments
worldwide.
Our
findings
demonstrate
ubiquity
in
many
floods.
Their
often
increases
with
magnitude,
but
strength
this
increase
varies
basis
catchment
conditions.
Traditional
might
underestimate
extreme
hazards
where
contribution
strongly
magnitude.
Overall,
our
study
highlights
need
carefully
incorporate
risk
assessment
improve
estimates
Nature Geoscience,
Journal Year:
2024,
Volume and Issue:
17(11), P. 1100 - 1107
Published: Oct. 21, 2024
Abstract
In
2022,
Europe
faced
an
extensive
summer
drought
with
severe
socioeconomic
consequences.
Quantifying
the
influence
of
human-induced
climate
change
on
such
extreme
event
can
help
prepare
for
future
droughts.
Here,
by
combining
observations
and
model
outputs
hydrological
land-surface
simulations,
we
show
that
Central
Southern
experienced
highest
observed
total
water
storage
deficit
since
satellite
began
in
2002,
probably
representing
most
widespread
soil
moisture
past
six
decades.
While
precipitation
deficits
primarily
drove
drought,
global
warming
contributed
to
over
30%
intensity
its
spatial
extent
via
enhanced
evaporation.
We
identify
14–41%
contribution
was
mediated
warming-driven
drying
occurred
before
year
indicating
importance
considering
lagged
effects
avoid
underestimating
associated
risks.
Human-induced
had
qualitatively
similar
extremely
low
river
discharges.
These
results
highlight
droughts
are
already
underway,
long
lasting,
risk
may
escalate
further
future.
Hydrology and earth system sciences,
Journal Year:
2023,
Volume and Issue:
27(15), P. 2973 - 2987
Published: Aug. 11, 2023
Abstract.
Floods
are
a
major
natural
hazard
in
the
Mediterranean
region,
causing
deaths
and
extensive
damages.
Recent
studies
have
shown
that
intense
rainfall
events
becoming
more
extreme
this
region
but,
paradoxically,
without
leading
to
an
increase
severity
of
floods.
Consequently,
it
is
important
understand
how
flood
changing
explain
absence
trends
magnitude
despite
increased
extremes.
A
database
98
stations
southern
France
with
average
record
50
years
daily
river
discharge
data
between
1959
2021
was
considered,
together
high-resolution
reanalysis
product
providing
precipitation
simulated
soil
moisture
classification
weather
patterns
associated
over
France.
Flood
events,
corresponding
occurrence
1
event
per
year
(5317
total),
were
extracted
classified
into
excess-rainfall,
short-rainfall,
long-rainfall
types.
Several
characteristics
been
also
analyzed:
durations,
base
flow
contribution
floods,
runoff
coefficient,
total
maximum
rainfall,
antecedent
moisture.
The
evolution
through
time
these
seasonality
analyzed.
Results
indicated
that,
most
basins,
floods
tend
occur
earlier
during
year,
mean
date
being,
on
average,
advanced
by
month
1959–1990
1991–2021.
This
seasonal
shift
could
be
attributed
frequency
southern-circulation
types
spring
summer.
An
extreme-event
has
observed,
decrease
before
events.
majority
excess
saturated
soils,
but
their
relative
proportion
decreasing
time,
notably
spring,
concurrent
short
rain
For
basins
there
positive
correlation
coefficients
remaining
stable
dryer
soils
producing
less
lower
In
context
increasing
aridity,
relationship
likely
cause
magnitudes
observed
change
These
changes
quite
homogeneous
domain
studied,
suggesting
they
rather
linked
regional
climate
than
catchment
characteristics.
study
shows
even
trends,
properties
may
need
accounted
for
when
analyzing
long-term
hazards.
Water,
Journal Year:
2024,
Volume and Issue:
16(15), P. 2199 - 2199
Published: Aug. 2, 2024
Machine
learning
models’
performance
in
simulating
monthly
rainfall–runoff
subtropical
regions
has
not
been
sufficiently
investigated.
In
this
study,
we
evaluate
the
of
six
widely
used
machine
models,
including
Long
Short-Term
Memory
Networks
(LSTMs),
Support
Vector
Machines
(SVMs),
Gaussian
Process
Regression
(GPR),
LASSO
(LR),
Extreme
Gradient
Boosting
(XGB),
and
Light
(LGBM),
against
a
model
(WAPABA
model)
streamflow
across
three
sub-basins
Pearl
River
Basin
(PRB).
The
results
indicate
that
LSTM
generally
demonstrates
superior
capability
than
other
five
models.
Using
previous
month
as
an
input
variable
improves
all
When
compared
with
WAPABA
model,
better
two
sub-basins.
For
simulations
wet
seasons,
shows
slightly
model.
Overall,
study
confirms
suitability
methods
modeling
at
scale
basins
proposes
effective
strategy
for
improving
their
performance.
The Science of The Total Environment,
Journal Year:
2023,
Volume and Issue:
891, P. 164626 - 164626
Published: June 5, 2023
Hydrometeorological
variability,
such
as
changes
in
extreme
precipitation,
snowmelt,
or
soil
moisture
excess,
Poland
can
lead
to
fluvial
flooding.
In
this
study
we
employed
the
dataset
covering
components
of
water
balance
with
a
daily
time
step
at
sub-basin
level
over
country
for
1952-2020.
The
data
set
was
derived
from
previously
calibrated
and
validated
Soil
&
Water
Assessment
Tool
(SWAT)
model
4000
sub-basins.
We
applied
Mann
Kendall
test
circular
statistics-based
approach
on
annual
maximum
floods
various
potential
flood
drivers
estimate
trend,
seasonality,
relative
importance
each
driver.
addition,
two
sub-periods
(1952-1985
1986-2020)
were
considered
examine
mechanism
recent
decades.
show
that
northeast
decreasing,
while
south
trend
showed
positive
behavior.
Moreover,
snowmelt
is
primary
driver
flooding
across
country,
followed
by
excess
precipitation.
latter
seemed
be
dominant
only
small,
mountain-dominated
region
south.
gained
mainly
northern
part,
suggesting
spatial
pattern
generation
mechanisms
also
governed
other
features.
found
strong
signal
climate
change
large
parts
Poland,
where
losing
second
sub-period
favor
which
explained
temperature
warming
diminishing
role
snow
processes.