Soil Systems,
Journal Year:
2023,
Volume and Issue:
7(2), P. 33 - 33
Published: April 8, 2023
The
salinity
of
estuarine
areas
in
arid
or
semi-arid
environments
can
reach
high
values,
conditioning
the
distribution
vegetation
and
soil
surface
characteristics.
While
many
studies
focused
on
prediction
as
a
function
numerous
parameters,
few
attempted
to
explain
role
its
within
profile
pattern
landscape
units.
In
wadi
estuary
northern
Morocco,
units
derived
from
satellite
imagery
naturalistic
environmental
analysis
are
compared
with
systematic
survey
by
means
apparent
electrical
conductivity
(Eca)
measurements.
comparison
is
based
allocation
measurement
points
an
area
Eca
measurements
alone,
using
linear
discriminant
four
machine
learning
methods.
results
show
that
between
57
66%
well-classified,
highlighting
major
factor
discrimination
zones.
mainly
result
interaction
capillary
rise
flooding
tides
wadi.
location
misclassified
analysed
discussed,
well
possible
causes
confusions.
EarthArXiv (California Digital Library),
Journal Year:
2024,
Volume and Issue:
unknown
Published: June 12, 2024
With
sea-level
rise,
flooding
in
coastal
communities
is
now
common
during
the
highest
high
tides.
Floods
also
occur
at
normal
tidal
levels
when
rainfall
overcomes
stormwater
infrastructure
that
partially
submerged
by
Data
describing
this
type
of
compound
scarce
and,
therefore,
it
unclear
how
often
these
floods
and
whether
there
are
other
non-tidal
factors
contribute
to
flooding.
We
combine
measurements
on
roads
within
storm
drains
with
a
numerical
model
examine
processes
Carolina
Beach,
NC,
USA
–
community
chronically
outside
extreme
storms
despite
flood
mitigation
combat
Of
43
non-storm
we
measured
year-long
study
period,
one-third
were
unexpected
because
forecasted
tide
was
below
their
monitoring
threshold.
introduce
novel
coupling
between
an
ocean-scale
hydrodynamic
(ADCIRC)
community-scale
surface
water
pipe
flow
(3Di)
quantify
contributions
from
multiple
drivers.
find
setup
sustained
(non-storm)
winds
modulates
extents
depth:
wind
causes
deeper,
longer,
more
extensive
tides
can
cause
days
would
not
have
occurred
due
alone.
Rainfall
contributes
floods;
submerge
outfalls
daily
basis,
even
minor
rainstorms
lead
as
runoff
has
nowhere
drain.
As
particularly
low-lying
community,
Beach
provides
glimpse
into
future
challenges
worldwide
will
face
predicting,
preparing
for,
adapting
increasingly
frequent
compounding
drivers
atop
rise.
Authorea (Authorea),
Journal Year:
2024,
Volume and Issue:
unknown
Published: June 13, 2024
Using
a
recently
developed
1/12th
degree
regional
ocean
model,
we
establish
link
between
U.S.
East
Coast
sea
level
variability
and
offshore
upper-ocean
heat
content
change.
This
manifests
as
cross-shore
mass
redistribution
driven
by
an
thermosteric
response
to
subsurface
warming
or
cooling.
Approximately
50\%
of
simulated
monthly
inter-annual
coastal
variance
south
Cape
Hatteras
can
be
statistically
accounted
for
this
mechanism,
realized
function
hypsometry,
gyre
scale
warming,
the
depth-dependence
density
explains
non-stationarity
coast
covariance,
specifically
observed
modeled
behavior
after
$\sim$
2010.
Since
approximately
2010,
elevated
rates
rise
partly
explained
result
shore-ward
due
sub-surface
within
North
Atlantic
subtropical
gyre.
These
results
reveal
mechanism
that
connects
local
broader
region
identifies
influence
changes
on
level.
analysis
presents
framework
identifying
new
regions
may
susceptible
enhanced
helps
bridge
gap
quantifying
large
change
anticipating
impacts
like
flooding
storm
surge.
Water Research,
Journal Year:
2024,
Volume and Issue:
266, P. 122339 - 122339
Published: Aug. 28, 2024
With
sea-level
rise,
flooding
in
coastal
communities
is
now
common
during
the
highest
high
tides.
Floods
also
occur
at
normal
tidal
levels
when
rainfall
overcomes
stormwater
infrastructure
that
partially
submerged
by
Data
describing
this
type
of
compound
scarce
and,
therefore,
it
unclear
how
often
these
floods
and
extent
to
which
non-tidal
factors
contribute
flooding.
We
combine
measurements
on
roads
within
storm
drains
with
a
numerical
model
examine
processes
Carolina
Beach,
NC,
USA
-
community
chronically
outside
extreme
storms
despite
flood
mitigation
combat
Of
43
non-storm
we
measured
year-long
study
period,
one-third
were
unexpected
based
threshold
used
for
monitoring.
introduce
novel
coupling
between
an
ocean-scale
hydrodynamic
(ADCIRC)
community-scale
surface
water
pipe
flow
(3Di)
quantify
contributions
from
multiple
drivers.
Accounting
compounding
effects
tides,
wind,
rain
increases
up
0.4
m
compared
simulations
include
only
Setup
sustained
(non-storm)
regional
winds
causes
deeper,
longer,
more
extensive
tides
can
cause
days
would
not
have
occurred
due
alone.
Rainfall
contributes
floods;
because
submerge
outfalls
daily
basis,
even
minor
rainstorms
lead
as
runoff
has
nowhere
drain.
As
particularly
low-lying
community,
Beach
provides
glimpse
into
future
challenges
worldwide
will
face
predicting,
preparing
for,
adapting
increasingly
frequent
drivers
atop
rise.
Abstract
Tidal
flooding
occurs
when
coastal
water
levels
exceed
impact-based
flood
thresholds
due
to
tides
alone,
under
average
weather
conditions.
Transitions
tidal
regimes
are
already
underway
for
nuisance
severities
in
harbours
and
bays
expected
higher
coming
decades.
In
the
first
such
regional
assessment,
we
show
that
same
transition
tidally
forced
floods
can
also
be
occur
Australian
estuaries
with
less
than
0.1
m
further
sea-level
rise.
Flood
historically
used
only
exceeded
combined
effects
of
riverine
(freshwater)
(salt
water)
influences
will
then
high
alone.
Once
this
emerges,
it
is
projected
become
chronic
within
two
Locations
most
at-risk
emergence
subsequent
establishment
those
just
inside
estuary
entrances.
These
locations
exemplified
by
low
freeboard,
vertical
distance
between
a
threshold
typical
tide
level.
We
use
freeboard-based
analysis
estimate
rise
required
impacts
associated
official
The
resultant
tide-only
frequency
estimates
provide
lower
bound
future
rates.
Journal of Geophysical Research Oceans,
Journal Year:
2024,
Volume and Issue:
129(12)
Published: Dec. 1, 2024
Abstract
Using
a
recently
developed
1/12th
degree
regional
ocean
model,
we
establish
link
between
U.S.
East
Coast
sea
level
variability
and
offshore
upper
heat
content
change.
This
manifests
as
cross‐shore
mass
redistribution
driven
by
an
thermosteric
response
to
subsurface
warming
or
cooling.
Approximately
50%
of
simulated
monthly
interannual
coastal
variance
south
Cape
Hatteras
can
be
statistically
accounted
for
this
mechanism,
realized
function
hypsometry,
gyre
scale
warming,
the
depth
dependence
density
explains
nonstationarity
covariance,
specifically
observed
modeled
behavior
after
2010.
Since
approximately
2010,
elevated
rates
rise
partly
explained
result
shoreward
due
within
North
Atlantic
subtropical
gyre.
These
results
reveal
mechanism
that
connects
local
broader
region
identifies
influence
changes
on
level.
analysis
presents
framework
identifying
new
regions
may
susceptible
enhanced
helps
bridge
gap
quantifying
large
change
anticipating
impacts
make
flooding
storm
surge
more
acutely
damaging.
Soil Systems,
Journal Year:
2023,
Volume and Issue:
7(2), P. 33 - 33
Published: April 8, 2023
The
salinity
of
estuarine
areas
in
arid
or
semi-arid
environments
can
reach
high
values,
conditioning
the
distribution
vegetation
and
soil
surface
characteristics.
While
many
studies
focused
on
prediction
as
a
function
numerous
parameters,
few
attempted
to
explain
role
its
within
profile
pattern
landscape
units.
In
wadi
estuary
northern
Morocco,
units
derived
from
satellite
imagery
naturalistic
environmental
analysis
are
compared
with
systematic
survey
by
means
apparent
electrical
conductivity
(Eca)
measurements.
comparison
is
based
allocation
measurement
points
an
area
Eca
measurements
alone,
using
linear
discriminant
four
machine
learning
methods.
results
show
that
between
57
66%
well-classified,
highlighting
major
factor
discrimination
zones.
mainly
result
interaction
capillary
rise
flooding
tides
wadi.
location
misclassified
analysed
discussed,
well
possible
causes
confusions.