The
coastal
sinking
of
land
in
many
low-lying
regions
the
world
has
a
greater
potential
risk
flooding-inundation
hazards
due
to
relative
sea
level
rise.
Kerala,
being
known
for
its
varied
geographical
features,
sharing
long
coastline
590
km
southern
part
India,
been
affected
by
several
floods
past
few
decades.
To
develop
an
effective
subsidence
monitoring
system
and
predict
hazard
risk,
this
study
makes
use
Multi-Temporal
Synthetic
Aperture
Radar
(MT-InSAR)
technique
using
Sentinel-1
data
obtain
Vertical
Land
Motion
(VLM)
over
Kerala
coast
projects
till
2100.
VLM
results
derived
from
InSAR
reveal
large
more
than
20mm/year
Kuttanad
region
Alappuzha
district.
Further,
we
incorporate
VLM,
future
projection
Intergovernmental
Panel
on
Climate
Change
(IPCC)
AR6
report,
high
spatial
resolution
Digital
Elevation
Model
(DEM)
map
fast
subsiding
zones
that
are
prone
flood
inundation
We
derive
maps
years
2030,
2050,
2070,
2100
considering
various
socio-economic
scenarios.
Earth s Future,
Journal Year:
2025,
Volume and Issue:
13(4)
Published: April 1, 2025
Abstract
High‐tide
flooding—minor,
disruptive
coastal
inundation—is
expected
to
become
more
frequent
as
sea
levels
rise.
However,
quantifying
just
how
quickly
high‐tide
flooding
rates
are
changing,
and
whether
some
places
experience
than
others,
is
challenging.
To
quantify
trends
in
from
tide‐gauge
observations,
flood
thresholds—elevations
above
which
begins—must
be
specified.
Past
studies
of
the
United
States
have
used
different
data
sets
approaches
for
specifying
thresholds,
only
directly
relate
impacts,
has
lead
sometimes
conflicting
ambiguous
results.
Here
we
present
a
novel
method
quantifying,
with
uncertainty,
thresholds
along
coast
based
on
sparsely
available
impact‐based
thresholds.
We
use
those
newly
modeled
make
an
updated
assessment
changes
across
over
past
few
decades.
From
1990–2000
2010–2020,
almost
certainly
(probability
)
increased
East
Coast,
Gulf
California,
Pacific
Islands,
while
they
very
likely
decreased
Alaska
during
that
time;
significant
between
two
decades
were
not
detected
Oregon,
Washington,
Caribbean.
Averaging
spatially,
find
probably
doubled
nationally
2010–2020.
Our
approach
lays
foundation
future
accurately
model
global
coastline.
Estuaries and Coasts,
Journal Year:
2025,
Volume and Issue:
48(4)
Published: April 16, 2025
Abstract
Extremechange
climate
events
provide
an
opportunity
to
understand
how
habitats
will
respond
future
long-term
change.
Starting
in
late
2013,
exceptionally
strong
marine
heatwave,
or
the
“Blob”,
which
was
followed
by
El
Niño
2015–2016,
resulted
anomalous
temporary
rise
sea
level
on
Pacific
US
coast.
We
examined
response
of
tidal
marsh
plant
communities
three
California
estuaries
spanning
over
600
km
these
elevated
water
levels.
focused
seaward
ecotone
Salicornia
pacifica
,
succulent
dominant
region.
S.
cover
declined
rapidly
and
sharply
at
all
increased
inundation.
In
areas
with
Spartina
foliosa
(Tijuana
River
Estuary),
this
low
colonized
dieback.
absence
(Carpinteria
Salt
Marsh
Elkhorn
Slough),
converted
mudflat.
demonstrate
rapid
systems
transient
changes,
emphasize
value
consistent
monitoring
using
field
surveys
remote
sensing
for
detecting
responses
rise.
These
case
studies
can
be
used
test
model
predictions,
as
we
empirical
evidence
vegetative
~
15
cm
sea-level
They
also
offer
concrete
examples
habitat
loss
type
conversion
resulting
from
change,
thereby
build
support
adaptation
strategies.
Anthropocene Coasts,
Journal Year:
2025,
Volume and Issue:
8(1)
Published: May 7, 2025
Abstract
Coastal
areas
are
one
of
the
most
vulnerable
regions
being
subjected
to
multiple
hazards
while
sheltering
people,
diverse
ecosystems,
key
infrastructure
and
other
assets.
Climate
change
will
produce
expected
changes
drivers
affecting
these
hazardous
events
which
when
coupled
with
uncertainty
degree
adverse
impacts,
place
coastal
communities
in
intractable
circumstances.
In
limited
access
human
financial
resources,
like
Caribbean
Small
Island
Developing
States
(SIDS),
there
must
be
a
focus
on
practical
solutions
tools
that
can
support
optimal
decision-making
areas.
The
adoption
nature-based
approaches
is
but
solution
mitigating
potentially
deleterious
effects,
reducing
vulnerability
enhancing
resilience.
Through
physical
modelling,
this
study
explores
how
selected
characteristics
synthesized
offshore
coral
reefs
affect
hydrodynamics
nearshore
zone
seeks
formulate
quantitative
relationships
for
applications.
These
serve
assessment
present-day
levels
protection
offered
by
provide
an
insight
into
future
ecosystems
conditions,
whether
caused
man
or
natural
influences,
hydrodynamics.
Assessment
potential
under
different
scenarios
allow
holistic
optimization
proposed
solutions.
outputs
demonstrated
good
correlation
between
wave
height
after
reef
above
velocities
incident
width
water
depths
reef.
experimental
results
also
trends
observed
from
studies
terms
attenuation,
albeit
smaller
extent.
assessed
parameters
generally
corroborated
anticipated
patterns
although
reflection
flume
appeared
skew
some
output.
expressions
produced
study,
though
given
scope,
demonstrate
methodology
readily
augmented
improve
existing
order
implement
hazard
mitigation
strategies
not
only
reduce
risk
assets
areas,
incorporate
systems
meaningful
way
valuable
co-benefits
communities.
Earth s Future,
Journal Year:
2024,
Volume and Issue:
12(5)
Published: April 30, 2024
Abstract
When
different
flooding
drivers
co‐occur,
they
can
cause
compound
floods.
Despite
the
potential
impact
of
flooding,
few
studies
have
projected
how
joint
probability
may
change.
Furthermore,
existing
projections
not
be
very
robust,
as
are
based
on
only
5
to
6
climate
model
simulations.
Here,
we
use
a
large
ensemble
simulations
from
Coupled
Model
Intercomparison
Project
(CMIP6)
project
changes
in
extreme
storm
surges
and
precipitation
at
European
tide
gauges
under
medium
high
emissions
scenario,
enabled
by
data‐proximate
cloud
computing
statistical
surge
modeling.
We
find
that
will
increase
northwest
decrease
most
southwest
Europe.
Averaged
over
Europe,
absolute
magnitude
these
is
36%–49%
2080,
depending
scenario.
The
large‐scale
similar
those
wind
speeds
precipitation,
but
locally,
differences
exceed
themselves.
Due
internal
variability
inter‐model
differences,
randomly
chosen
CMIP6
models
higher
than
10%
differ
qualitatively
all
multiple
regions,
especially
scenario
earlier
twenty‐first
century.
Therefore,
our
results
provide
more
robust
less
uncertain
representation
for
Europe
previous
projections.
Geophysical Research Letters,
Journal Year:
2023,
Volume and Issue:
50(21)
Published: Nov. 8, 2023
Abstract
Due
to
their
choked
geometry,
coastal
lagoons
can
attenuate
extreme
water
levels
compared
the
open
sea.
However,
this
protective
property
is
expected
decrease
due
sea‐level
rise.
By
studying
idealized
in
a
non‐dimensional
parameter
space,
study
describes
non‐linear
interactions
between
tides,
storm
surges,
freshwater
fluxes
into
lagoon,
and
The
numbers
include
lagoon
geometry
forcing
scales.
main
objective
provide
an
overview
of
potentially
affected
highlight
importance
attenuation
changes
Tidal
surge
induced
maximum
inside
rise
faster
than
for
most
space.
Maximum
slower
strongly
lagoons.
For
compound
events,
response
rising
or
depends
on
geometry.
Earth s Future,
Journal Year:
2024,
Volume and Issue:
12(2)
Published: Feb. 1, 2024
Abstract
Sea‐level
rise
is
leading
to
increasingly
frequent
coastal
floods
globally.
Recent
research
shows
that
changes
in
tidal
properties
and
storm
surge
magnitudes
can
further
exacerbate
sea‐level
rise‐related
increases
flood
frequencies.
However,
such
non‐stationarity
tide
statistics
are
largely
neglected
existing
projection
methodologies.
Here
we
develop
a
framework
explore
the
effect
different
realizations
of
various
sources
uncertainty
have
on
projections
frequencies,
including
range
storminess.
Our
methodology
captures
how
observed
rates
depend
surges
coincide
with
extremes.
We
show
higher
earlier
emergence
chronic
flooding
associated
larger
rates,
lower
thresholds,
skew
magnitudes.
Smaller
thresholds
decreases
sea
level
variability
lead
commensurately
rates.
Percentagewise,
amplitudes
generally
much
impact
frequencies
than
equivalent
percentagewise
several
implications
these
findings.
Firstly,
understanding
future
local
tides
required
fully
quantify
hazards.
Secondly,
hazard
assessments
may
underestimate
as
not
considered.
Finally,
identifying
severities
relevant
managers
imperative
useable
policy‐relevant
for
decisionmakers.
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.
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.