Abstract
Flash
floods
are
largely
driven
by
high
rainfall
rates
in
convective
storms
that
projected
to
increase
frequency
and
intensity
a
warmer
climate
the
future.
However,
quantifying
changes
future
flood
flashiness
is
challenging
due
lack
of
high-resolution
simulations.
Here
we
use
outputs
from
continental
convective-permitting
numerical
weather
model
at
4-km
hourly
resolution
force
hydrologic
scale
depict
such
change.
As
results
indicate,
US
becoming
7.9%
flashier
end
century
assuming
high-emissions
scenario.
The
Southwest
(+10.5%)
has
greatest
among
historical
flash
hot
spots,
central
(+8.6%)
emerging
as
new
spot.
Additionally,
flood-prone
frontiers
advancing
northwards.
This
study
calls
on
implementing
climate-resilient
mitigation
measures
for
spots.
Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: May 16, 2023
Flooding
is
one
of
the
most
common
natural
hazards,
causing
disastrous
impacts
worldwide.
Stress-testing
global
human-Earth
system
to
understand
sensitivity
floodplains
and
population
exposure
a
range
plausible
conditions
strategy
identify
where
future
changes
flooding
or
might
be
critical.
This
study
presents
analysis
inundated
areas
varying
flood
event
magnitudes
globally
for
1.2
million
river
reaches.
Here
we
show
that
topography
drainage
correlate
with
sensitivities
as
well
societal
behaviour.
We
find
clear
settlement
patterns
in
which
sensitive
frequent,
low
magnitude
events,
reveal
evenly
distributed
across
hazard
zones,
suggesting
people
have
adapted
this
risk.
In
contrast,
extreme
events
tendency
populations
densely
settled
these
rarely
flooded
being
significant
danger
from
potentially
increasing
given
climate
change.
Geoderma,
Journal Year:
2023,
Volume and Issue:
440, P. 116713 - 116713
Published: Nov. 16, 2023
Assessing
root
sources
of
three
uncertainties
–
parameterization
soil
hydraulic
characteristics,
boundary
conditions,
and
estimation
source/sink
terms
is
a
significant
challenge
in
water
transport
modeling.
This
study
aims
to
evaluate
the
uncertainty
each
widely-used
parameter
methods
affecting
plot-scale
dynamics.
The
employs
HYDRUS,
process-based
hydrologic
model,
incorporate
these
compare
model
predictions
measured
values
semiarid
Inner
Mongolia
steppe,
China.
Soil
parameters
are
determined
using
two
direct
(laboratory-derived
approach
evaporation
method)
one
indirect
method
(neural
network).
While
generally
simulates
moisture
dynamics,
performed
better,
especially
under
dry
conditions.
suggests
that
measuring
intensity
properties,
such
as
unsaturated
conductivity,
with
crucial
for
reasonable
simulation.
also
demonstrates
impact
different
applied
conditions
on
simulated
moisture,
specifically
partitioning
reference
FAO
evapotranspiration
via
(soil
fraction
cover)
(leaf
area
index
crop
height).
cover
reflected
better
Additionally,
compares
uptake
function
growth
constant
depth
referenced
grass
pasture,
finds
no
difference
among
them.
Comparing
predicting
concludes
input
more
sensitive
than
or
representation
function.
Our
highlights
properties
can
reflect
effects
land
use
change,
compaction,
field
transports.
Hydrology and earth system sciences,
Journal Year:
2019,
Volume and Issue:
23(3), P. 1339 - 1354
Published: March 11, 2019
Abstract.
Alpine
catchments
show
a
high
sensitivity
to
climate
variation
as
they
include
the
elevation
range
of
snow
line.
Therefore,
correct
representation
variables
and
their
interdependence
is
crucial
when
describing
or
predicting
hydrological
processes.
When
using
model
simulations
in
impact
studies,
forcing
meteorological
data
are
usually
downscaled
bias
corrected,
most
often
by
univariate
approaches
such
quantile
mapping
individual
variables,
neglecting
relationships
that
exist
between
variables.
In
this
study
we
test
hypothesis
explicit
consideration
relation
air
temperature
precipitation
will
affect
modelling
snow-dominated
mountain
environment.
Glacio-hydrological
were
performed
for
two
partly
glacierized
alpine
recently
developed
multivariate
correction
method
post-process
EURO-CORDEX
regional
outputs
1976
2099.
These
compared
those
obtained
common
correction.
As
both
methods
each
variable's
distribution
same
way,
marginal
distributions
no
differences.
Yet,
regarding
temperature,
clear
differences
notable
studied
catchments.
Simultaneous
based
on
approach
led
more
below
temperatures
0
∘C
therefore
simulated
snowfall
than
with
approach.
This
difference
translated
considerable
consequences
responses
The
bias-correction-forced
showed
distinctly
different
results
projected
cover
characteristics,
snowmelt-driven
streamflow
components,
expected
glacier
disappearance
dates.
all
aspects
–
fraction
above
∘C,
water
equivalents,
volumes,
regime
resulting
from
multivariate-corrected
corresponded
better
reference
Differences
total
due
may
be
considered
negligible
given
generally
large
spread
projections,
but
systematic
seasonally
delayed
components
snowmelt
particular
matter
planning
perspective.
While
does
not
allow
conclusive
evidence
preferable,
it
clearly
demonstrates
incorporating
ignoring
inter-variable
can
conclusions
drawn
change
studies
environments.
Water Resources Research,
Journal Year:
2016,
Volume and Issue:
52(10), P. 8343 - 8373
Published: Oct. 1, 2016
Understanding
hydrological
model
predictive
capabilities
under
contrasting
climate
conditions
enables
more
robust
decision
making.
Using
Differential
Split
Sample
Testing
(DSST),
we
analyze
the
performance
of
six
models
for
37
Irish
catchments
unlike
those
used
training.
Additionally,
consider
four
ensemble
averaging
techniques
when
examining
interperiod
transferability.
DSST
is
conducted
using
2/3
year
noncontinuous
blocks
(i)
wettest/driest
years
on
record
based
precipitation
totals
and
(ii)
with
a
more/less
pronounced
seasonal
regime.
Model
transferability
between
regimes
was
found
to
vary
depending
testing
scenario,
catchment,
evaluation
criteria
considered.
As
expected,
average
outperformed
most
individual
members.
However,
differed
considerably
in
number
times
they
surpassed
best
member.
Bayesian
Averaging
(BMA)
Granger-Ramanathan
(GRA)
method
were
outperform
simple
arithmetic
mean
(SAM)
Akaike
Information
Criteria
(AICA).
Here
GRA
performed
better
than
51%–86%
cases
(according
Nash-Sutcliffe
criterion).
When
assessing
skill
change
recommend
setting
up
select
available
analogues
expected
annual
conditions;
applying
multiple
criteria;
(iii)
diverse
set
catchments;
(iv)
multimodel
conjunction
an
appropriate
technique.
Given
computational
efficiency
relative
BMA,
former
recommended
as
preferred
technique
assessment.
Hydrology and earth system sciences,
Journal Year:
2019,
Volume and Issue:
23(11), P. 4471 - 4489
Published: Oct. 30, 2019
Extreme
low
and
high
flows
can
have
negative
economic,
social,
ecological
effects
are
expected
to
become
more
severe
in
many
regions
due
climate
change.
Besides
flows,
the
whole
flow
regime,
i.e.,Â
annual
hydrograph
comprised
of
monthly
mean
is
subject
changes.
Knowledge
on
future
changes
regimes
important
since
contain
information
both
extremes
conditions
prior
dry
wet
seasons.
Changes
individual
low-
high-flow
characteristics
as
well
under
been
thoroughly
studied.
In
contrast,
little
known
about
extreme
regimes.
We
here
propose
two
methods
for
estimation
apply
them
simulated
discharge
time
series
Switzerland.
The
first
method
relies
frequency
analysis
performed
duration
curves.
second
approach
performs
sums
a
large
set
stochastically
generated
hydrographs.
Both
approaches
were
found
produce
similar
100-year
regime
estimates
when
applied
data
19Â
hydrological
Our
results
show
that
rainfall-dominated
distinct
from
those
melt-dominated
regions.
regions,
minimum
low-flow
decreases
by
up
50
%,
whilst
reduction
25
%
maximum
increases
%.
point
other
direction
than
discharges
increase
100
decrease
less
respectively.
findings
provide
guidance
water
resource
planning
management
valuable
basis
impact
studies.
Highlights
Estimation
using
curves
will
change
conditions.
but
Scientific Reports,
Journal Year:
2019,
Volume and Issue:
9(1)
Published: Sept. 16, 2019
Abstract
Climate
change
impacts
are
non
uniformly
distributed
over
the
globe.
Mountains
have
a
peculiar
response
to
large
scale
variations,
documented
by
elevation
gradients
of
surface
temperature
increase
observed
many
mountain
ranges
in
last
decades.
Significant
changes
precipitation
expected
changing
climate
and
orographic
effects
important
determining
amount
rainfall
at
given
location.
It
thus
becomes
particularly
understand
how
responds
global
warming
anthropogenic
forcing.
Here,
using
rain
gauge
dataset
European
Alpine
region,
we
show
that
distribution
annual
among
lowlands
mountains
has
varied
time,
with
an
high
elevations
compared
low
starting
mid
20
century
peaking
1980s.
The
simultaneous
peak
aerosol
load
is
discussed
as
possible
source
for
this
interdecadal
change.
These
results
provide
new
insights
further
our
understanding
improve
predictions
anthropic
on
precipitations,
which
fundamental
water
security
management.
Journal of Hydrology X,
Journal Year:
2021,
Volume and Issue:
11, P. 100074 - 100074
Published: Jan. 27, 2021
Society
and
the
environment
in
arid
southwestern
United
States
depend
on
reliable
water
availability,
yet
current
use
outpaces
supply.
Water
demand
is
projected
to
grow
future
climate
change
expected
reduce
To
adapt,
managers
need
robust
estimates
of
regional
supply
support
management
decisions.
address
this
need,
we
estimate
streamflow
seven
resource
regions
U.S.
using
a
new
SPAtially
Referenced
Regressions
On
Watershed
attributes
(SPARROW)
model.
We
present
projections
corresponding
input
data
from
models
two
greenhouse
gas
Representative
Concentration
Pathways
(RCP4.5
8.5)
for
three,
thirty-year
intervals
centered
2030s,
2050s,
2080s,
historical
thirty
year
interval
1990s.
Across
regions,
about
half
RCP4.5
(51%)
thirds
RCP8.5
(67%)
indicate
decreases
2080s
relative
period.
Models
project
maximum
36–80%
all
periods
RCPs
streamflow,
up
20–45%
at
sites
along
Colorado
River
used
measuring
compliance
with
interstate
international
agreements.
Headwaters
are
experience
greatest
declines,
substantial
downstream
implications.
Among
these
estimates,
streamflows
forced
tend
be
lower
than
those
RCP4.5.
Not
models,
times,
widespread
declines.
The
most
ubiquitous
increases
occur
2030s
under
Later
time
enhanced
forcings
smaller
increase
accumulated
streamflows,
suggesting
that
limiting
or
reducing
concentrations
could
availability.
Although
some
possible
promising,
modest
spatially
limited
later
still
unlikely
sufficient
meet
demand.
These
results
inform
likelihood
agreement
compliance,
developing
strategies
balance
Hydrology and earth system sciences,
Journal Year:
2021,
Volume and Issue:
25(5), P. 2685 - 2703
Published: May 20, 2021
Abstract.
A
deep
learning
rainfall–runoff
model
can
take
multiple
meteorological
forcing
products
as
input
and
learn
to
combine
them
in
spatially
temporally
dynamic
ways.
This
is
demonstrated
with
Long
Short-Term
Memory
networks
(LSTMs)
trained
over
basins
the
continental
US,
using
Catchment
Attributes
Meteorological
data
set
for
Large
Sample
Studies
(CAMELS).
Using
from
different
(North
American
Land
Data
Assimilation
System,
NLDAS,
Maurer,
Daymet)
a
single
LSTM
significantly
improved
simulation
accuracy
relative
only
individual
products.
sensitivity
analysis
showed
that
combines
precipitation
ways,
depending
on
location,
also
ways
of
parts
hydrograph.