PLoS neglected tropical diseases,
Journal Year:
2021,
Volume and Issue:
15(3), P. e0009182 - e0009182
Published: March 18, 2021
Climate
change
and
variability
influence
temperature
rainfall,
which
impact
vector
abundance
the
dynamics
of
vector-borne
disease
transmission.
is
projected
to
increase
frequency
intensity
extreme
climate
events.
Mosquito-borne
diseases,
such
as
dengue
fever,
are
primarily
transmitted
by
Aedes
aegypti
mosquitoes.
Freshwater
availability
affect
populations
via
a
variety
biological
processes
thus
ability
mosquitoes
effectively
transmit
disease.
However,
effect
droughts,
floods,
heat
waves,
cold
waves
not
well
understood.
Using
vector,
climate,
data
collected
between
2013
2019
in
Kenya,
this
retrospective
cohort
study
aims
elucidate
rainfall
on
mosquito
risk
arboviral
infections.
To
define
periods
land
surface
(LST),
we
calculated
monthly
anomalies
deviations
from
long-term
means
(1983–2019
for
2000–2019
LST)
across
four
locations
Kenya.
We
classified
events
upper
lower
10%
these
LST
or
deviations.
Monthly
Ae
.
was
recorded
Kenya
using
trapping
methods.
Blood
samples
were
also
children
with
febrile
illness
presenting
field
sites
tested
virus
an
IgG
enzyme-linked
immunosorbent
assay
(ELISA)
polymerase
chain
reaction
(PCR).
found
that
eggs
adults
significantly
more
abundant
one
month
following
abnormally
wet
month.
The
relationship
follows
non-linear
association.
Our
findings
suggest
early
warnings
targeted
interventions
during
abnormal
temperature,
especially
flooding,
can
potentially
contribute
reductions
viral
Water Resources Research,
Journal Year:
2018,
Volume and Issue:
54(11), P. 8545 - 8551
Published: Nov. 1, 2018
Abstract
Despite
evidence
of
increasing
precipitation
extremes,
corresponding
for
increases
in
flooding
remains
elusive.
If
anything,
flood
magnitudes
are
decreasing
despite
widespread
claims
by
the
climate
community
that
if
extremes
increase,
floods
must
also.
In
this
commentary
we
suggest
reasons
why
extreme
rainfall
not
resulting
flooding.
Among
possible
mechanisms
responsible,
identify
decreases
antecedent
soil
moisture,
storm
extent,
and
snowmelt.
We
argue
understanding
link
between
changes
is
a
grand
challenge
hydrologic
deserving
increased
attention.
Hydrology and earth system sciences,
Journal Year:
2021,
Volume and Issue:
25(7), P. 3897 - 3935
Published: July 7, 2021
Abstract.
Hydroclimatic
extremes
such
as
intense
rainfall,
floods,
droughts,
heatwaves,
and
wind
or
storms
have
devastating
effects
each
year.
One
of
the
key
challenges
for
society
is
understanding
how
these
are
evolving
likely
to
unfold
beyond
their
historical
distributions
under
influence
multiple
drivers
changes
in
climate,
land
cover,
other
human
factors.
Methods
analysing
hydroclimatic
advanced
considerably
recent
decades.
Here
we
provide
a
review
drivers,
metrics,
methods
detection,
attribution,
management,
projection
nonstationary
extremes.
We
discuss
issues
uncertainty
associated
with
approaches
(e.g.
arising
from
insufficient
record
length,
spurious
nonstationarities,
incomplete
representation
sources
modelling
frameworks),
examine
empirical
simulation-based
frameworks
analysis
extremes,
identify
gaps
future
research.
Water Resources Research,
Journal Year:
2021,
Volume and Issue:
57(2)
Published: Feb. 1, 2021
Abstract
Atmospheric
moisture
holding
capacity
increases
with
temperature
by
about
7%
per
°C
according
to
the
Clausius‐Clapeyron
relationship.
Thermodynamically
then,
precipitation
intensity
should
exponentially
intensify
and
thus
worsen
flood
conditions
as
climate
warms.
However,
regional
global
analyses
often
report
a
nonmonotonic
(hook)
scaling
of
runoff,
in
which
extremes
strengthen
rising
up
maximum
or
peak
point
(T
pp
)
decline
thereafter.
The
underlying
cause
this
hook
structure
is
not
yet
well‐understood,
whether
it
may
shift
and/or
regulate
storm
runoff
under
anthropogenic
warming
remains
unknown.
Here,
we
examine
different
using
observations
large
ensemble
hydroclimatic
simulations
over
mainland
China.
In
situ
suggest
spatially
homogeneous,
negative
response
relative
humidity
climates
34.6%
land
area,
remaining
hook‐dominated
regions
usually
show
colder
T
than
that
extremes.
streamflow
series
China's
catchments
throughout
21st
century
are
projected
model
cascade
chain
high‐end
emission
scenario
(RCP
8.5),
involves
31
CMIP5
models,
11
CMIP6
members,
daily
bias
correction
method,
four
lumped
conceptual
hydrological
models.
projects
structures
toward
warmer
bins,
resulting
10%–30%
China,
while
more
severe
future
climates.
Journal of Hydrologic Engineering,
Journal Year:
2022,
Volume and Issue:
27(6)
Published: March 24, 2022
This
review
provides
a
broad
overview
of
the
current
state
flood
research,
challenges,
and
future
directions.
Beginning
with
discussion
flood-generating
mechanisms,
synthesizes
literature
on
forecasting,
multivariate
nonstationary
frequency
analysis,
urban
flooding,
remote
sensing
floods.
Challenges
research
directions
are
outlined
highlight
emerging
topics
where
more
work
is
needed
to
help
mitigate
risks.
It
anticipated
that
systems
will
likely
have
significant
risk
due
compounding
effects
continued
climate
change
land-use
intensification.
The
timely
prediction
floods,
quantification
socioeconomic
impacts
developing
mitigation
strategies
continue
be
challenging.
There
need
bridge
scales
between
model
capabilities
end-user
needs
by
integrating
multiscale
models,
stakeholder
input,
social
citizen
science
input
for
monitoring,
mapping,
dissemination.
Although
much
progress
has
been
made
in
using
applications,
recent
upcoming
Earth
Observations
provide
excellent
potential
unlock
additional
benefits
applications.
community
can
benefit
from
downscaled,
as
well
ensemble
scenarios
consider
changes.
Efforts
also
data
assimilation
approaches,
especially
ingest
local,
citizen,
media
data.
Also
enhanced
compound
hazards
assess
reduce
vulnerability
impacts.
dynamic
complex
interactions
climate,
societal
change,
watershed
processes,
human
factors
often
confronted
deep
uncertainty
highlights
transdisciplinary
science,
policymakers,
stakeholders
vulnerability.