EarthArXiv (California Digital Library),
Journal Year:
2023,
Volume and Issue:
unknown
Published: July 10, 2023
Large-scale,
high-resolution
hydrologic
modeling
is
an
important
tool
to
address
questions
of
water
quantity,
availability,
and
recharge.
Continental-to-Global
scale
models,
particularly
those
that
include
groundwater,
are
growing
in
number.
However,
many
these
approaches
simplify
aspects
the
system
connections
between
e.g.,
surface
groundwater.
The
ParFlow
CONUS
platform
a
large-scale,
hyper-resolution,
model
relies
on
integrated
solution
3D
partial
differential
equations
describe
soil,
flow.
prior
version,
1.0,
was
first
large-scale
included
explicit
treatment
lateral
groundwater
flow
for
contiguous
US.
Here,
we
present
2.0
model.
This
extends
coastlines
contributing
basins
United
States
(i.e.,
CONUS)
consistent
with
NOAA
National
Water
Model.
Here
document
roughly
five
years
technical
development
this
platform,
steady-state
simulation
results,
rigorously
compare
results
1.0
simulations,
evaluate
performance
based
observations.
Simulated
table
depth
streamflow
were
evaluated
using
more
than
635K
observations
from
USGS
monitoring
wells
gauges.
Our
demonstrate
improvement
both
simulations
over
generation
all
Hydrologic
Unit
Code
(HUC)
basins.
These
also
suggest
current
has
good
excellent
entire
CONUS,
almost
half
HUC
subbasins
exhibiting
normalized
root-square
error
(RSR).
metric
not
usually
compared
directly
at
studies,
good-to-excellent
exhibited
some
regions.
Frontiers in Science,
Journal Year:
2024,
Volume and Issue:
1
Published: March 5, 2024
Climate
change
is
profoundly
affecting
the
global
water
cycle,
increasing
likelihood
and
severity
of
extreme
water-related
events.
Better
decision-support
systems
are
vital
to
accurately
predict
monitor
environmental
disasters
optimally
manage
resources.
These
must
integrate
advances
in
remote
sensing,
situ
,
citizen
observations
with
high-resolution
Earth
system
modeling,
artificial
intelligence
(AI),
information
communication
technologies,
high-performance
computing.
Digital
Twin
(DTE)
models
a
ground-breaking
solution
offering
digital
replicas
simulate
processes
unprecedented
spatiotemporal
resolution.
Advances
observation
(EO)
satellite
technology
pivotal,
here
we
provide
roadmap
for
exploitation
these
methods
DTE
hydrology.
The
4-dimensional
Hydrology
datacube
now
fuses
EO
data
advanced
modeling
soil
moisture,
precipitation,
evaporation,
river
discharge,
report
latest
validation
Mediterranean
Basin.
This
can
be
explored
forecast
flooding
landslides
irrigation
precision
agriculture.
Large-scale
implementation
such
will
require
further
assess
products
across
different
regions
climates;
create
compatible
multidimensional
datacubes,
retrieval
algorithms,
that
suitable
multiple
scales;
uncertainty
both
models;
enhance
computational
capacity
via
an
interoperable,
cloud-based
processing
environment
embodying
open
principles;
harness
AI/machine
learning.
We
outline
how
various
planned
missions
facilitate
hydrology
toward
benefit
if
scientific
technological
challenges
identify
addressed.
Earth system science data,
Journal Year:
2024,
Volume and Issue:
16(4), P. 2007 - 2032
Published: April 29, 2024
Abstract.
Earth
system
models
(ESMs)
are
progressively
advancing
towards
the
kilometer
scale
(“k-scale”).
However,
surface
parameters
for
land
(LSMs)
within
ESMs
running
at
k-scale
typically
derived
from
coarse-resolution
and
outdated
datasets.
This
study
aims
to
develop
a
new
set
of
global
with
resolution
1
km
multiple
years
2001
2020,
utilizing
latest
most
accurate
available
Specifically,
datasets
consist
related
use
cover,
vegetation,
soil,
topography.
Differences
between
newly
developed
conventional
emphasize
their
potential
higher
accuracy
due
incorporation
advanced
data
sources.
To
demonstrate
capability
these
parameters,
we
conducted
simulations
using
E3SM
Land
Model
version
2
(ELM2)
over
contiguous
United
States.
Our
results
that
contribute
significant
spatial
heterogeneity
in
ELM2
soil
moisture,
latent
heat,
emitted
longwave
radiation,
absorbed
shortwave
radiation.
On
average,
about
31
%
54
information
is
lost
by
upscaling
12
resolution.
Using
eXplainable
Machine
Learning
(XML)
methods,
influential
factors
driving
variability
loss
were
identified,
highlighting
substantial
impact
various
as
well
mean
climate
conditions.
The
comparison
against
four
benchmark
indicates
ELM
generally
performs
simulating
moisture
energy
fluxes.
tailored
meet
emerging
needs
LSM
ESM
modeling
implications
our
understanding
water,
carbon,
cycles
under
change.
publicly
https://doi.org/10.5281/zenodo.10815170
(Li
et
al.,
2024).
Journal of Hydrology,
Journal Year:
2024,
Volume and Issue:
633, P. 130901 - 130901
Published: Feb. 15, 2024
Integrated
Hydrological
Models
(IHMs)
dynamically
couple
surface
and
groundwater
processes
across
the
unsaturated
zone
domain.
IHMs
are
data
intensive
computationally
demanding
but
can
provide
physically
realistic
output,
particularly
if
sufficient
input
of
high
quality
is
available.
In-situ
observations
often
have
a
small
footprint
time
cost-demanding.
Satellite
remote
sensing
observations,
with
their
long
series
archives
spatially
semi-continuous
gridded
format,
as
well
hydrogeophysical
flexible,
'on-demand'
high-resolution
coverage,
perfectly
complement
in-situ
observations.
We
review
contribution
various
satellite
products
for
IHM:
(1)
climate
forcings,
(2)
parameters,
(3)
boundary
conditions
(4)
constraining
model
calibration
assimilation.
Our
hydrogeophysics
focuses
on
four
mentioned
IHM
contributions,
we
analyze
them
per
acquisition
platform,
i.e.,
surface,
drone-borne
airborne
hydrogeophysics.
Finally,
includes
discussion
optimal
use
in
IHMs,
vision
further
improvements
data-driven,
integrated
hydrological
modelling.
Journal of Hydrology,
Journal Year:
2023,
Volume and Issue:
626, P. 130294 - 130294
Published: Oct. 13, 2023
Large-scale,
high-resolution
hydrologic
modeling
is
an
important
tool
to
address
questions
of
water
quantity,
availability,
and
potential
recharge.
Continental-to-Global
scale
models,
particularly
those
that
include
groundwater,
are
growing
in
number.
However,
many
these
approaches
simplify
aspects
the
system
connections
between
surface
groundwater.
The
ParFlow
CONUS
platform
a
large-scale,
hyper-resolution,
model
relies
on
integrated
solution
3D
partial
differential
equations
describe
soil,
2D
flow.
prior
version,
1.0,
was
first
large-scale
included
explicit
treatment
lateral
groundwater
flow
for
contiguous
US
(CONUS).
Here,
we
present
2.0
model.
This
extends
coastlines
contributing
basins
consistent
with
NOAA
National
Water
Model.
Here
document
roughly
five
years
technical
development
this
platform,
steady-state
simulation
results,
rigorously
compare
results
1.0
simulations,
evaluate
performance
based
observations.
Simulated
table
depth
streamflow
were
evaluated
using
more
than
635K
observations
from
USGS
monitoring
wells,
other
compiled
datasets,
NHD
gauges.
Our
demonstrate
improvement
both
simulations
over
generation
all
Hydrologic
Unit
Code
(HUC)
basins.
These
suggest
current
has
good
excellent
entire
CONUS,
almost
half
HUC
subbasins
exhibiting
normalized
root-square
error
(RSR).
metric
not
usually
compared
directly
at
studies,
good-to-excellent
exhibited
some
regions.
We
also
delineate
two
regions
influence
performance,
one
where
microtopography
around
streams
dominates
(D2),
another
mix
subsurface
heterogeneity
topographic
gradients
dominate
(D1).
Improvements
topography
CONUS1
CONUS2
generally
result
better
performances.
Advancements
structure
produce
estimates.
Water Resources Research,
Journal Year:
2024,
Volume and Issue:
60(3)
Published: March 1, 2024
Abstract
Coupled
simulations
of
surface
and
variably
saturated
subsurface
flow,
termed
integrated
hydrologic
models
(IHMs),
can
provide
powerful
insights
into
the
complex
dynamics
watersheds.
The
system
governing
equations
solved
by
an
IHM
is
non‐linear,
making
them
a
significant
computational
burden
challenging
to
accurately
parameterize.
Consequently,
large
fraction
studies
date
have
been
“numerical
hypothesis
testing”
studies,
but,
as
parallel
computing
continues
improve,
IHMs
are
approaching
point
where
they
might
also
be
useful
predictive
tools.
For
this
become
reality,
uncertainty
such
highly
parameterized
must
considered.
However,
seldom
considered
in
literature,
likely
due
long
runtimes
simulations.
questions
herein
how
much
there
for
common
watershed
simulation
scenario,
it
that
any
one
realization
will
give
same
relative
change
other
perturbation
recharge?
A
stochastic
ensemble
250
permeability
field
realizations
was
used
show
high‐mountain
headwaters
systems
dominated
subsurface.
Recharge
scenarios
echo
these
results,
but
changes
streamflow
or
groundwater
pressure
heads
were
significantly
smaller
than
their
base‐case
values.
main
finding
do
confident,
estimates
watersheds,
even
when
specific
outputs
may
high.