Journal of Hydrology,
Год журнала:
2024,
Номер
634, С. 131105 - 131105
Опубликована: Март 24, 2024
Understanding
the
fluctuations
in
groundwater
levels
response
to
meteorological
conditions
is
challenging,
especially
given
slow
transit
time
associated
with
reservoirs
and
short
duration
of
series
for
levels.
Nevertheless,
this
knowledge
crucial
water
resource
management,
that
global
warming
will
drastically
impact
hydrological
dynamics
cold
humid
climates.
The
objective
work
was
quantify
how
standardized
indexes
contribute
understanding
level
climates
(10
23
years).
relationships
between
precipitation
index
(SPI),
temperature
(STI),
climate
indexes,
(SGI)
were
analyzed.
reactivity
examined
2000
2022
using
measurements
from
152
wells
located
46°N
52°N
province
Quebec
(Canada).
results
showed
available
sufficient
provide
new
insights
into
role
on
fluctuations,
demonstrating
usefulness
indexes.
One
main
contributions
study
hydrogeological
systems
go
through
an
annual
reset
due
prolonged
freezing
period.
This
one
drivers
isolating
year-to-year
conditions,
contributing
short-duration
droughts.
Geophysical Research Letters,
Год журнала:
2022,
Номер
49(18)
Опубликована: Сен. 13, 2022
Abstract
Understanding
how
groundwater
storage
(GWS)
responds
to
climate
change
is
essential
for
water
resources
management
and
future
availability
in
the
Tibetan
Plateau
(TP).
However,
dominant
factor
controlling
long‐term
GWS
changes
remains
unclear
its
responses
are
not
well
understood.
Here
we
combined
multi‐source
datasets
including
in‐situ
measurements,
satellite
observations,
global
models,
reanalysis
products
reveal
that
increased
at
5.59
±
1.44
Gt/yr
during
2003–2016
while
showing
spatial
heterogeneities
with
increasing
trends
northern
TP
glacial
regions
declining
central
southern
TP.
The
accelerated
transformation
from
solid
(glaciers,
snow,
permafrost;
−17.72
1.53
Gt/yr)
into
liquid
provide
more
recharge
groundwater,
dominating
total
increase.
This
study
contributes
a
better
understanding
of
hydrological
cycle
under
provides
key
information
projecting
different
scenarios
Journal of Hydrology,
Год журнала:
2023,
Номер
626, С. 130294 - 130294
Опубликована: Окт. 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.
New Phytologist,
Год журнала:
2023,
Номер
240(3), С. 968 - 983
Опубликована: Авг. 25, 2023
Summary
Accounting
for
water
limitation
is
key
to
determining
vegetation
sensitivity
drought.
Quantifying
effects
on
evapotranspiration
(ET)
challenged
by
the
heterogeneity
of
types,
climate
zones
and
vertically
along
rooting
zone.
Here,
we
train
deep
neural
networks
using
flux
measurements
study
ET
responses
progressing
drought
conditions.
We
determine
a
stress
factor
(fET)
that
isolates
reductions
from
atmospheric
aridity
other
covarying
drivers.
regress
fET
against
cumulative
deficit,
which
reveals
control
whole‐column
moisture
availability.
find
variety
stress.
Responses
range
rapid
declines
10%
its
water‐unlimited
rate
at
several
savannah
grassland
sites,
mild
in
most
forests,
despite
substantial
deficits.
Most
sensitive
are
found
arid
warm
sites.
A
combination
regulation
stomatal
hydraulic
conductance
access
belowground
reservoirs,
whether
groundwater
or
soil
moisture,
could
explain
different
behaviors
observed
across
This
not
captured
standard
land
surface
model,
likely
reflecting
simplifications
representation
storage.
Ground Water,
Год журнала:
2023,
Номер
62(1), С. 15 - 33
Опубликована: Июнь 24, 2023
Abstract
Effective
groundwater
management
is
critical
to
future
environmental,
ecological,
and
social
sustainability
requires
accurate
estimates
of
withdrawals.
Unfortunately,
these
are
not
readily
available
in
most
areas
due
physical,
regulatory,
challenges.
Here,
we
compare
four
different
approaches
for
estimating
withdrawals
agricultural
irrigation.
We
apply
methods
a
groundwater‐irrigated
region
the
state
Kansas,
USA,
where
high‐quality
withdrawal
data
evaluation.
The
represent
broad
spectrum
approaches:
(1)
hydrologically‐based
Water
Table
Fluctuation
method
(WTFM);
(2)
demand‐based
SALUS
crop
model;
(3)
based
on
satellite‐derived
evapotranspiration
(ET)
from
OpenET;
(4)
landscape
hydrology
model
which
integrates
hydrologic‐
approaches.
applicability
each
approach
varies
availability,
spatial
temporal
resolution,
accuracy
predictions.
In
general,
our
results
indicate
that
all
reasonably
estimate
region,
however,
type
amount
required
computational
requirements
vary
among
For
example,
WTFM
levels,
specific
yield,
recharge
data,
whereas
adequate
information
about
type,
land
use,
weather.
This
variability
highlights
difficulty
identifying
what
how
much,
necessary
reasonable
estimate,
suggests
availability
should
drive
choice
approach.
Overall,
findings
will
help
practitioners
evaluate
strengths
weaknesses
select
appropriate
their
application.
Hydrology and earth system sciences,
Год журнала:
2023,
Номер
27(6), С. 1383 - 1401
Опубликована: Март 31, 2023
Abstract.
The
quest
for
hydrological
hyper-resolution
modelling
has
been
on-going
more
than
a
decade.
While
global
models
(GHMs)
have
seen
reduction
in
grid
size,
they
thus
far
never
consistently
applied
at
(<=1
km)
the
large
scale.
Here,
we
present
first
application
of
GHM
PCR-GLOBWB
1
km
over
Europe.
We
thoroughly
evaluated
simulated
discharge,
evaporation,
soil
moisture,
and
terrestrial
water
storage
anomalies
against
long-term
observations
subsequently
compared
results
with
established
10
50
resolutions
PCR-GLOBWB.
Subsequently,
could
assess
added
value
this
version
scale
dependencies
model
forcing
resolution.
Eventually,
these
insights
can
help
us
understanding
current
challenges
opportunities
from
formulating
data
requirements
future
improvements.
found
that,
most
variables,
epistemic
uncertainty
is
still
large,
issues
commensurability
exist
respect
to
yet
coarse
used.
Merely
confidently
state
that
output
improves
coarser
due
better
representation
river
network
km.
However,
currently
available
are
not
widely
or
lack
sufficiently
long
time
series,
which
makes
it
difficult
performance
other
variables
hyper-resolution.
additional
validation
efforts
needed.
On
side,
applications
require
careful
revisiting
parameterization
possibly
implementation
physical
processes
be
able
resemble
dynamics
spatial
heterogeneity
With
km,
contribute
meeting
grand
challenge
modelling.
Even
though
was
only
assessed
continental
scale,
valuable
gained
validity.
As
such,
should
as
modest
milestone
on
longer
journey
towards
locally
relevant
output.
This,
however,
requires
community
effort
domain
experts,
developers,
research
software
engineers,
providers.
Data
assimilation
applications
in
integrated
surface-subsurface
hydrological
models
(ISSHMs)
are
generally
limited
to
scales
ranging
from
the
hillslope
local
or
meso-scale
catchments.
This
is
because
ISSHMs
resolve
processes
detail
and
a
physics-based
fashion
therefore
typically
require
intensive
computational
efforts
rely
on
ground-based
observations
with
small
spatial
support.
At
other
end
of
spectrum,
there
vast
body
literature
remote
sensing
data
for
land
surface
(LSMs)
at
continental
even
global
scale.
In
LSMs,
some
usually
represented
coarse
resolution
empirical
ways,
especially
groundwater
lateral
flows,
which
may
be
very
important
yet
often
neglected.
Starting
review
recent
progress
multiple
scales,
we
stress
need
find
common
ground
between
LSMs
suggest
possible
ways
forward
advance
use
models.
Water,
Год журнала:
2023,
Номер
15(17), С. 3118 - 3118
Опубликована: Авг. 30, 2023
The
development
of
civilization
and
the
preservation
environmental
ecosystems
are
strongly
dependent
on
water
resources.
Typically,
an
insufficient
supply
surface
resources
for
domestic,
industrial,
agricultural
needs
is
supplemented
with
groundwater
However,
a
natural
resource
that
must
accumulate
over
many
years
cannot
be
recovered
after
short
period
recharge.
Therefore,
long-term
management
important
issue
sustainable
development.
accurate
prediction
levels
first
step
in
evaluating
total
their
allocation.
process
data
collection,
may
lost
due
to
various
factors.
Filling
missing
main
problem
any
research
field
address.
It
well
known
maintain
integrity,
one
effective
approach
value
imputation
(MVI).
In
addition,
it
has
been
demonstrated
machine
learning
better
tool.
purpose
this
study
was
utilize
generative
adversarial
network
(GAN)
consists
model
discriminative
imputation.
Although
GAN
could
not
capture
level
endpoints
every
section,
overall
simulation
performance
still
excellent
some
extent.
Our
results
show
can
improve
accuracy
evaluations.
current
study,
two
interdisciplinary
deep
methods,
univariate
Seq2val
(sequence-to-value),
were
used
estimation.
addition
addressing
significance
parameter
conditions,
advantages
disadvantages
these
models
hydrological
simulations
also
discussed
compared.
Regarding
selection,
analysis
than
those
analysis.
Finally,
employed
examine
limits
simulations.
suggest
CNNs
better,
while
LSTM
multistep
prediction.
beneficial
providing
evaluation