Earth Surface Dynamics,
Journal Year:
2024,
Volume and Issue:
12(6), P. 1295 - 1313
Published: Nov. 25, 2024
Abstract.
Computing
hydrological
fluxes
at
the
Earth's
surface
is
crucial
for
landscape
evolution
models,
topographic
analysis,
and
geographic
information
systems.
However,
existing
formalisms,
like
single
or
multiple
flow
algorithms,
often
rely
on
ad
hoc
rules
based
local
slope
drainage
area,
neglecting
physics
of
water
flow.
While
more
physics-oriented
solutions
offer
accuracy
(e.g.
shallow-water
equations),
their
computational
costs
limit
use
in
terms
spatial
temporal
scales.
In
this
contribution,
we
introduce
GraphFlood,
a
novel
efficient
iterative
method
computing
river
depth
discharge
2D
with
digital
elevation
model
(DEM).
Leveraging
directed
acyclic
graph
structure
flow,
GraphFlood
iteratively
solves
equations.
This
algorithm
aims
to
find
correct
hydraulic
by
balancing
input
output
over
topography.
At
each
iteration,
employ
fast-graph-theory
algorithms
calculate
accumulation
surface,
approximating
input.
Discharge
then
computed
using
Manning
resistance
equation,
similar
River.lab
(Davy
Lague,
2009).
The
divergence
discharges
increments
until
reaching
stationary
state.
can
also
solve
flood
wave
propagation
function
immediate
upstream
neighbours.
We
validate
depths
obtained
solution
against
analytical
rectangular
channels
CAESAR-Lisflood
models
natural
DEMs.
demonstrates
significant
advantages
previous
hydrodynamic
an
approximately
10-fold
speed-up
compared
Additionally,
its
time
scales
slightly
than
linearly
number
cells,
making
it
suitable
large
DEMs
exceeding
106–108
cells.
demonstrate
versatility
integrating
realistic
hydrology
into
various
morphometric
analyses,
including
channel
width
measurement,
inundation
pattern
delineation,
floodplain
classification
hillslope,
colluvial,
fluvial
domains.
Furthermore,
discuss
integration
potential
highlighting
simplicity
implementation
efficiency.
Hydrology,
Journal Year:
2022,
Volume and Issue:
9(3), P. 50 - 50
Published: March 18, 2022
The
modelling
and
management
of
flood
risk
in
urban
areas
are
increasingly
recognized
as
global
challenges.
complexity
these
issues
is
a
consequence
the
existence
several
distinct
sources
risk,
including
not
only
fluvial,
tidal
coastal
flooding,
but
also
exposure
to
runoff
local
drainage
failure,
various
strategies
that
can
be
proposed.
high
degree
vulnerability
characterizes
such
expected
increase
future
due
effects
climate
change,
growth
population
living
cities,
densification.
An
increasing
awareness
socio-economic
losses
environmental
impact
flooding
clearly
reflected
recent
expansion
number
studies
related
sometimes
within
framework
adaptation
change.
goal
current
paper
provide
general
review
advances
flood-risk
management,
while
exploring
perspectives
fields
research.
Water,
Journal Year:
2021,
Volume and Issue:
13(21), P. 3115 - 3115
Published: Nov. 4, 2021
Detecting
effective
parameters
in
flood
occurrence
is
one
of
the
most
important
issues
that
has
drawn
more
attention
recent
years.
Remote
Sensing
(RS)
and
Geographical
Information
System
(GIS)
are
two
efficient
ways
to
spatially
predict
Flood
Risk
Mapping
(FRM).
In
this
study,
a
web-based
platform
called
Google
Earth
Engine
(GEE)
(Google
Company,
Mountain
View,
CA,
USA)
was
used
obtain
risk
indices
for
Galikesh
River
basin,
Northern
Iran.
With
aid
Landsat
8
satellite
imagery
Shuttle
Radar
Topography
Mission
(SRTM)
Digital
Elevation
Model
(DEM),
11
(Elevation
(El),
Slope
(Sl),
Aspect
(SA),
Land
Use
(LU),
Normalized
Difference
Vegetation
Index
(NDVI),
Water
(NDWI),
Topographic
Wetness
(TWI),
Distance
(RD),
Waterway
Density
(WRD),
Soil
Texture
(ST]),
Maximum
One-Day
Precipitation
(M1DP))
were
provided.
next
step,
all
these
imported
into
ArcMap
10.8
(Esri,
West
Redlands,
software
index
normalization
better
visualize
graphical
output.
Afterward,
an
intelligent
learning
machine
(Random
Forest
(RF)),
which
robust
data
mining
technique,
compute
importance
degree
each
hazard
map.
According
results,
WRD,
RD,
M1DP,
El
accounted
about
68.27
percent
total
risk.
Among
indices,
WRD
containing
23.8
greatest
impact
on
floods.
FRM
mapping,
21
18
areas
stood
at
higher
highest
areas,
respectively.
Journal of Hydrology,
Journal Year:
2022,
Volume and Issue:
612, P. 128182 - 128182
Published: July 11, 2022
Modelling
hydrological
processes
with
fully
distributed
models
based
on
the
shallow
water
equations
implies
a
high
computational
cost,
which
often
limits
resolution
of
mesh.
Therefore,
in
practice,
modellers
need
to
find
compromise
between
spatial
resolution,
numerical
accuracy
and
cost.
Moreover,
this
balance
is
probably
related
underlying
Digital
Terrain
Model
(DTM).
In
work,
it
studied
effect
DTM
size
mesh
results
runtime
model
2D
equations.
Seven
rainfall
events
four
different
basins
have
been
modelled
using
3
DTMs
resolutions.
The
obtained
highlight
relevance
vertical
versus
horizontal
DTMs.
Furthermore,
has
observed
that
resolutions
greater
than
25
m,
together
LiDAR-based
provide
comparable
outflow
hydrographs.
Water Resources Research,
Journal Year:
2023,
Volume and Issue:
59(10)
Published: Oct. 1, 2023
Abstract
In
our
era,
the
rapid
increase
of
parallel
programming
coupled
with
high‐performance
computing
(HPC)
facilities
allows
for
use
two‐dimensional
shallow
water
equation
(2D‐SWE)
algorithms
simulating
floods
at
“hydrological”
catchment
scale,
rather
than
just
“hydraulic”
fluvial
scale.
This
approach
paves
way
development
new
operational
systems
focused
on
impact‐based
flash‐floods
nowcasting,
wherein
hydrodynamic
simulations
directly
model
spatial
and
temporal
variability
measured
or
predicted
rainfall
impacts
even
a
street
Specifically,
main
goal
this
research
is
to
make
step
move
toward
implementation
an
effective
flash
flood
nowcasting
system
in
which
timely
accurate
impact
warnings
are
provided
by
including
weather
radar
products
HPC
2D‐SWEs
modelling
framework
able
integrate
watershed
hydrology,
flow
hydrodynamics,
river
urban
flooding
one
model.
The
timing,
location,
intensity
street‐level
evolution
some
key
elements
risk
(people,
vehicles,
infrastructures)
also
discussed
considering
both
calibration
issues
role
played
resolution.
All
these
analyzed
having
as
starting
point
event
hit
Mandra
town
(Athens,
Greece)
15
November
2017,
highlighting
feasibility
accuracy
overall
providing
insights
field.
Geoscientific model development,
Journal Year:
2023,
Volume and Issue:
16(3), P. 977 - 1008
Published: Feb. 8, 2023
Abstract.
The
Simulation
EnviRonment
for
Geomorphology,
Hydrodynamics,
and
Ecohydrology
in
Integrated
form
(SERGHEI)
is
a
multi-dimensional,
multi-domain,
multi-physics
model
framework
environmental
landscape
simulation,
designed
with
an
outlook
towards
Earth
system
modelling.
At
the
core
of
SERGHEI's
innovation
its
performance-portable
high-performance
parallel-computing
(HPC)
implementation,
built
from
scratch
on
Kokkos
portability
layer,
allowing
SERGHEI
to
be
deployed,
fashion,
graphics
processing
unit
(GPU)-based
heterogeneous
systems.
In
this
work,
we
explore
combinations
MPI
using
OpenMP
CUDA
backends.
contribution,
introduce
present
detail
first
operational
module
solving
shallow-water
equations
(SERGHEI-SWE)
HPC
implementation.
This
applicable
hydrological
problems
including
flooding
runoff
generation,
Its
applicability
demonstrated
by
testing
several
well-known
benchmarks
large-scale
problems,
which
SERGHEI-SWE
achieves
excellent
results
different
types
problems.
Finally,
scalability
performance
evaluated
TOP500
systems,
very
good
scaling
range
over
20
000
CPUs
up
256
state-of-the
art
GPUs.
Journal of Hydrology,
Journal Year:
2023,
Volume and Issue:
621, P. 129667 - 129667
Published: May 16, 2023
Data
assimilation
(DA)
in
physically-based
hydrodynamic
models
is
conditioned
by
the
difference
temporal
and
spatial
scales
of
observed
data
resolution
model
itself.
In
order
to
use
remote
sensing
small-scale
modelling,
it
necessary
explore
innovative
DA
methods
that
can
lead
a
more
plausible
representation
variability
parameters
processes
involved.
present
study,
satellite-derived
soil
moisture
situ-observed
streamflow
were
jointly
assimilated
into
high-resolution
hydrological-hydrodynamic
based
on
Iber
software,
using
Tempered
Particle
Filter
(TPF)
for
dual
estimation
state
variables
parameters.
Twelve
storm
events
occurring
199
km2
catchment
located
NW
Spain
used
testing
proposed
approach.
A
3-step
procedure
was
followed:
(1)
sensitivity
analysis
parameters;
(2)
joint
discharge
estimate
correlations
between
observations
(3)
an
initial
set
particles
parameter
standard
deviations
derived
from
prior
information.
The
numerical
correctly
reproduces
data,
with
average
Nash-Sutcliffe
efficiency
(NSE)
value
0.74
over
12
when
information
used.
approach
described
shown
be
most
efficient
produce
isolated
peak
discharges.
Journal of Hydrology,
Journal Year:
2024,
Volume and Issue:
632, P. 130728 - 130728
Published: Jan. 24, 2024
Fluvial
landscape
analysis
represents
an
essential
component
in
geomorphology,
hydrology,
ecology
and
cartography.
It
is
traditionally
focused
on
the
transition
between
hillslopes
channel
domain,
which
network
drainage
represented
by
static
flow
lines.
However,
natural
fluctuations
of
processes
occurring
watershed
induce
lateral
longitudinal
expansions
contractions
patterns
variations
stream
surface
area.
These
can
be
better
understood
introducing
a
two-dimensional
(2D)
view
catchment
hydrography,
river
width
floodplain
are
included
analysis.
The
novelty
introduced
this
work
development
hydrodynamic
hierarchical
framework
(HHF)
to
analyse
transitions
among
geomorphic
hydrographic
features
fluvial
landscape,
distinguishing
hillslope,
unchanneled
valleys,
floodplains,
single/multithreads
channels.
HHF
based
estimation
nested
inundation
pattern
domains
(IPDs)
from
digital
elevation
models
2D
modeling.
IPDs
defined
scaling
laws
that
characterize
log–log
relations
density
unit
discharge
thresholds
extracted
direct
rainfall
method
(DRM)
approach
under
steady
state
solutions.
physical
significance
analysed
within
context
both
physiographic
rates
employed
as
input
for
modeling
approach.
Initially,
spatial
heterogeneity
initially
used
derive
metrics
function
rate.
Then,
index,
representative
IPDs'
heterogeneity,
measure
susceptibility
area
expand/contract.
Finally,
consistency
results
assessed
comparison
another
hydrodynamic-based
recently
proposed
literature.
using
challenging
mountain
low-relief
environments,
characterized
multithread
channels,
meander
cut-offs,
oxbow
lakes,
extreme
landscapes
feature
glacial
outwash,
permafrost,
peatlands.
Journal of Hydrology,
Journal Year:
2024,
Volume and Issue:
632, P. 130778 - 130778
Published: Jan. 26, 2024
Badlands
are
often
the
source
of
a
significant
fraction
sediment
reaching
river
network
due
to
exposure
bare
soil
impact
rain
drops
and
bed
shear
stress
generated
by
surface
runoff.
Hence,
correct
understanding
erosion
transport
processes
inside
badlands
can
help
better
characterisation
suspended
production
at
catchment
scale.
In
this
work
we
study
suitability
two-dimensional
(2D)
physically-based
event-scale
model
as
tool
represent
in
seasonal
The
solves
2D
shallow
water
equations,
including
infiltration
rainfall,
order
compute
generation
routing
runoff
within
badland.
Coupled
hydrodynamic
equation
with
terms
that
account
for
rainfall-
runoff-driven
deposition.
Based
on
model,
an
overall
procedure
was
developed
tested
considering,
case
study,
badland
located
El
Soto
(central
Pyrenees,
Iberian
Peninsula).
For
analysed
badland,
several
high-resolution
topography
surveys
were
available,
which
allowed
estimation
loss
spatial
distribution
patterns
periods
3-4
months
over
two
years.
These
data
sets
used
calibrate
validate
proposed
modelling
approach,
analyse
its
capabilities
limitations
assessment