Hydrological Sciences Journal,
Journal Year:
2018,
Volume and Issue:
63(4), P. 493 - 512
Published: March 12, 2018
This
study
analyses
the
differences
in
significant
trends
magnitude
and
frequency
of
floods
detected
annual
maximum
flood
(AMF)
peak
over
threshold
(POT)
series,
for
period
1965–2005.
Flood
peaks
are
identified
from
European
daily
discharge
data
using
a
baseflow-based
algorithm
AMF
series
compared
with
those
POT
derived
six
different
exceedence
thresholds.
The
results
show
that
more
than
magnitude.
Spatially
coherent
patterns
detected,
which
further
investigated
by
stratifying
into
five
regions
based
on
catchment
hydro-climatic
characteristics.
All
tools
used
this
open-access
fully
reproducible.
Water Resources Research,
Journal Year:
2021,
Volume and Issue:
58(1)
Published: Dec. 27, 2021
Abstract
Long
short‐term
memory
(LSTM)
networks
represent
one
of
the
most
prevalent
deep
learning
(DL)
architectures
in
current
hydrological
modeling,
but
they
remain
black
boxes
from
which
process
understanding
can
hardly
be
obtained.
This
study
aims
to
demonstrate
potential
interpretive
DL
gaining
scientific
insights
using
flood
prediction
across
contiguous
United
States
(CONUS)
as
a
case
study.
Two
interpretation
methods
were
adopted
decipher
machine‐captured
patterns
and
inner
workings
LSTM
networks.
The
by
expected
gradients
method
revealed
three
distinct
input‐output
relationships
learned
LSTM‐based
runoff
models
160
individual
catchments.
These
correspond
flood‐inducing
mechanisms—snowmelt,
recent
rainfall,
historical
rainfall—that
account
for
10.1%,
60.9%,
29.0%
20,908
flow
peaks
identified
data
set,
respectively.
Single
flooding
mechanisms
dominate
70.7%
investigated
catchments
(11.9%
snowmelt‐dominated,
34.4%
rainfall‐dominated,
24.4%
rainfall‐dominated
mechanisms),
remaining
29.3%
have
mixed
mechanisms.
spatial
variability
dominant
reflects
catchments'
geographic
climatic
conditions.
Moreover,
additive
decomposition
unveils
how
network
behaves
differently
retaining
discarding
information
when
emulating
different
types
floods.
Information
inputs
within
previous
time
steps
partially
stored
predict
snowmelt‐induced
rainfall‐induced
floods,
while
only
is
retained.
Overall,
this
provides
new
perspective
processes
extremes
demonstrates
prospect
artificial
intelligence‐assisted
discovery
future.
Earth system science data,
Journal Year:
2020,
Volume and Issue:
12(3), P. 2075 - 2096
Published: Sept. 8, 2020
Abstract.
We
introduce
a
new
catchment
dataset
for
large-sample
hydrological
studies
in
Brazil.
This
encompasses
daily
time
series
of
observed
streamflow
from
3679
gauges,
as
well
meteorological
forcing
(precipitation,
evapotranspiration,
and
temperature)
897
selected
catchments.
It
also
includes
65
attributes
covering
range
topographic,
climatic,
hydrologic,
land
cover,
geologic,
soil,
human
intervention
variables,
data
quality
indicators.
paper
describes
how
the
hydrometeorological
were
produced,
their
primary
limitations,
main
spatial
features.
To
facilitate
comparisons
with
catchments
other
countries,
follow
same
standards
previous
CAMELS
(Catchment
Attributes
MEteorology
Large-sample
Studies)
datasets
United
States,
Chile,
Great
Britain.
CAMELS-BR
(Brazil)
complements
by
providing
hundreds
tropics
Amazon
rainforest.
Importantly,
precipitation
evapotranspiration
uncertainties
are
assessed
using
several
gridded
products,
quantitative
estimates
water
consumption
provided
to
characterize
impacts
on
resources.
By
extracting
combining
these
different
products
making
publicly
available,
we
aim
create
opportunities
research
Brazil
inclusion
Brazilian
basins
continental
global
studies.
envision
that
this
will
enable
community
gain
insights
into
drivers
behavior,
better
extreme
hydroclimatic
events,
explore
climate
change
activities
resources
The
is
freely
available
at
https://doi.org/10.5281/zenodo.3709337
(Chagas
et
al.,
2020).
Precipitation
extremes
will
increase
in
a
warming
climate,
but
the
response
of
flood
magnitudes
to
heavier
precipitation
events
is
less
clear.
Historically,
there
little
evidence
for
systematic
increases
magnitude
despite
observed
extremes.
Here
we
investigate
how
change
warming,
using
large
initial-condition
ensemble
simulations
with
single
climate
model,
coupled
hydrological
model.
The
model
chain
was
applied
historical
(1961–2000)
and
warmer
future
(2060–2099)
conditions
78
watersheds
Bavaria,
region
comprising
headwater
catchments
Inn,
Danube
Main
River,
thus
representing
an
area
expressed
heterogeneity.
For
majority
catchments,
identify
‘return
interval
threshold’
relationship
between
increases:
at
return
intervals
above
this
threshold,
further
extreme
frequency
clearly
yield
increased
magnitudes;
below
modulated
by
land
surface
processes.
We
suggest
that
threshold
behaviour
can
reconcile
climatological
perspectives
on
changing
risk
climate.
Germany
rainfall
processes
not
above,
Geophysical Research Letters,
Journal Year:
2021,
Volume and Issue:
48(6)
Published: March 9, 2021
Abstract
Concepts
like
the
100‐year
flood
event
can
be
misleading
if
they
are
not
updated
to
reflect
significant
changes
over
time.
Here,
we
model
observed
annual
maximum
daily
streamflow
using
a
nonstationary
approach
provide
first
global
picture
of
in:
(a)
magnitudes
20‐,
50‐,
and
floods
(i.e.,
flows
given
exceedance
probability
in
each
year
);
(b)
return
periods
floods,
as
assessed
1970
fixed
magnitude
(c)
corresponding
probabilities.
Empirically,
find
20‐/50‐year
have
mostly
increased
temperate
climate
zones,
but
decreased
arid,
tropical,
polar,
cold
zones.
In
contrast,
arid/temperate
zones
exhibit
mixed
trends
results
influenced
by
small
number
stations
with
long
records,
highlight
need
for
continued
updating
hazard
assessments.
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.
The European Physical Journal Plus,
Journal Year:
2022,
Volume and Issue:
137(1)
Published: Jan. 13, 2022
Abstract
This
article
reviews
recent
bibliography
on
time
series
of
some
extreme
weather
events
and
related
response
indicators
in
order
to
understand
whether
an
increase
intensity
and/or
frequency
is
detectable.
The
most
robust
global
changes
climate
extremes
are
found
yearly
values
heatwaves
(number
days,
maximum
duration
cumulated
heat),
while
trends
heatwave
not
significant.
Daily
precipitation
stationary
the
main
part
stations.
Trend
analysis
tropical
cyclones
show
a
substantial
temporal
invariance
same
true
for
tornadoes
USA.
At
time,
impact
warming
surface
wind
speed
remains
unclear.
then
extended
meteorological
events,
namely
natural
disasters,
floods,
droughts,
ecosystem
productivity
yields
four
crops
(maize,
rice,
soybean
wheat).
None
these
clear
positive
trend
events.
In
conclusion
basis
observational
data,
crisis
that,
according
many
sources,
we
experiencing
today,
evident
yet.
It
would
be
nevertheless
extremely
important
define
mitigation
adaptation
strategies
that
take
into
account
current
trends.
Environmental Research Letters,
Journal Year:
2017,
Volume and Issue:
12(11), P. 114035 - 114035
Published: Aug. 24, 2017
Analyses
of
trends
in
observed
floods
often
focus
on
relatively
frequent
events,
whereas
changes
rare
are
only
studied
for
a
small
number
locations
that
have
exceptionally
long
observational
records.
Understanding
is
especially
relevant
as
these
events
most
damaging
and
influence
the
design
major
structures.
Here,
we
provide
an
assessment
largest
flood
(~0.033
annual
exceedance
probability)
during
period
1980−2009
1744
catchments
located
Australia,
Brazil,
Europe
United
States.
The
occurrence
spatial
aggregate
shows
strong
temporal
variability
peaked
around
1995.
During
30
year
period,
there
overall
increases
both
frequency
magnitude
extreme
floods.
These
strongest
States,
weakest
Brazil
Australia.
Physical
causes
reported
short-term
longer-term
currently
remain
elusive,
because
key
drivers
vary
between
catchments.
Nonetheless,
this
approach
provides
basis
more
spatially
representative
occurrence.