Water Resources Research,
Journal Year:
2015,
Volume and Issue:
51(7), P. 4923 - 4947
Published: June 17, 2015
Abstract
Global
hydrology
has
come
a
long
way
since
the
first
introduction
of
primitive
land
surface
model
Manabe
(1969)
and
declaration
“Emergence
Hydrology”
by
Eagleson
(1986).
Hydrological
submodels
varying
complexity
are
now
part
global
climate
models,
models
calculating
terrestrial
carbon
sequestration,
earth
system
even
integrated
assessment
models.
This
paper
reviews
current
state
hydrological
modeling,
discusses
past
recent
developments,
extrapolates
these
to
future
challenges
directions.
First,
established
domains
applications
discussed,
in
terms
societal
science
questions
posed,
type
developed,
advances
therein.
Next,
genealogy
is
given.
After
reviewing
efforts
connect
components
from
different
domains,
new
identified
where
starting
become
an
integral
analyses.
Finally,
inspired
application,
persistent
emerging
as
well
directions
likely
take
coming
decade
beyond.
The
Working
Group
II
contribution
to
the
Sixth
Assessment
Report
of
Intergovernmental
Panel
on
Climate
Change
(IPCC)
provides
a
comprehensive
assessment
scientific
literature
relevant
climate
change
impacts,
adaptation
and
vulnerability.
report
recognizes
interactions
climate,
ecosystems
biodiversity,
human
societies,
integrates
across
natural,
ecological,
social
economic
sciences.
It
emphasizes
how
efforts
in
reducing
greenhouse
gas
emissions
can
come
together
process
called
resilient
development,
which
enables
liveable
future
for
biodiversity
humankind.
IPCC
is
leading
body
assessing
science.
reports
are
produced
comprehensive,
objective
transparent
ways,
ensuring
they
reflect
full
range
views
literature.
Novel
elements
include
focused
topical
assessments,
an
atlas
presenting
observed
impacts
risks
from
global
regional
scales.
Available
as
Open
Access
Cambridge
Core.
Hydrological Sciences Journal,
Journal Year:
2013,
Volume and Issue:
59(1), P. 1 - 28
Published: Dec. 20, 2013
A
holistic
perspective
on
changing
rainfall-driven
flood
risk
is
provided
for
the
late
20th
and
early
21st
centuries.
Economic
losses
from
floods
have
greatly
increased,
principally
driven
by
expanding
exposure
of
assets
at
risk.
It
has
not
been
possible
to
attribute
rain-generated
peak
streamflow
trends
anthropogenic
climate
change
over
past
several
decades.
Projected
increases
in
frequency
intensity
heavy
rainfall,
based
models,
should
contribute
precipitation-generated
local
flooding
(e.g.
flash
urban
flooding).
This
article
assesses
literature
included
IPCC
SREX
report
new
published
since,
includes
an
assessment
changes
seven
regions
considered
recent
report—Africa,
Asia,
Central
South
America,
Europe,
North
Oceania
Polar
regions.
Also
considering
newer
publications,
this
consistent
with
finding
that
impacts
characteristics
are
highly
sensitive
detailed
nature
those
presently
we
only
low
confidence1
numerical
projections
magnitude
or
resulting
change.Editor
D.
KoutsoyiannisCitation
Kundzewicz,
Z.W.,
et
al.,
2013.
Flood
change:
global
regional
perspectives.
Hydrological
Sciences
Journal,
59
(1),
1–28.
Scientific Reports,
Journal Year:
2020,
Volume and Issue:
10(1)
Published: Aug. 13, 2020
Abstract
The
hydrological
cycle
is
expected
to
intensify
with
global
warming,
which
likely
increases
the
intensity
of
extreme
precipitation
events
and
risk
flooding.
changes,
however,
often
differ
from
theorized
expectation
in
water‐holding
capacity
atmosphere
warmer
conditions,
especially
when
water
availability
limited.
Here,
relationships
changes
flood
intensities
for
end
twenty-first
century
spatial
seasonal
are
quantified.
Results
show
an
intensification
over
all
climate
regions
as
dry
wet
regions.
Similarly,
there
increase
availability.
connection
between
becomes
stronger
become
less
extreme.
Climatic Change,
Journal Year:
2014,
Volume and Issue:
134(3), P. 387 - 401
Published: March 5, 2014
This
paper
presents
an
assessment
of
the
implications
climate
change
for
global
river
flood
risk.
It
is
based
on
estimation
frequency
relationships
at
a
grid
resolution
0.5
×
0.5°,
using
hydrological
model
with
scenarios
derived
from
21
models,
together
projections
future
population.
Four
indicators
hazard
are
calculated;
in
magnitude
and
return
period
peaks,
flood-prone
population
cropland
exposed
to
substantial
frequency,
generalised
measure
regional
risk
combining
curves
generic
damage
functions.
Under
one
model,
emissions
socioeconomic
scenario
(HadCM3
SRES
A1b),
2050
current
100-year
would
occur
least
twice
as
frequently
across
40
%
globe,
approximately
450
million
people
430
thousand
km2
be
doubling
increase
by
187
over
absence
change.
There
strong
variability
(most
adverse
impacts
Asia),
considerable
between
models.
In
2050,
range
increased
exposure
models
under
A1b
31–450
59
cropland,
varies
−9
+376
%.
The
region,
also
mean
surface
temperature
hazard.
number
caveats
analysis;
it
only,
constructed
pattern-scaling,
precise
sensitive
some
assumptions
definition
application.
Earth s Future,
Journal Year:
2016,
Volume and Issue:
5(2), P. 171 - 182
Published: Dec. 26, 2016
Rising
global
temperature
has
put
increasing
pressure
on
understanding
the
linkage
between
atmospheric
warming
and
occurrence
of
natural
hazards.
While
Paris
Agreement
set
ambitious
target
to
limiting
1.5°C
compared
preindustrial
levels,
scientists
are
urged
explore
scenarios
for
different
thresholds
quantify
ranges
socioeconomic
impact.
In
this
work,
we
present
a
framework
estimate
economic
damage
population
affected
by
river
floods
at
scale.
It
is
based
modeling
cascade
involving
hydrological,
hydraulic
impact
simulations,
makes
use
state-of-the-art
layers
hazard,
exposure
vulnerability
1-km
grid
resolution.
An
ensemble
seven
high-resolution
climate
projections
Representative
Concentration
Pathways
8.5
used
derive
streamflow
simulations
in
future
climate.
Those
were
analyzed
assess
frequency
magnitude
their
impacts
under
corresponding
1.5°C,
2°C,
4°C
warming.
Results
indicate
clear
positive
correlation
flood
risk
At
warming,
countries
representing
more
than
70%
gross
domestic
product
will
face
increases
excess
500%.
Changes
unevenly
distributed,
with
largest
Asia,
U.S.,
Europe.
contrast,
changes
statistically
not
significant
most
Africa
Oceania
all
considered
levels.
New Phytologist,
Journal Year:
2015,
Volume and Issue:
206(1), P. 57 - 73
Published: Jan. 7, 2015
Summary
Unanticipated
flooding
challenges
plant
growth
and
fitness
in
natural
agricultural
ecosystems.
Here
we
describe
mechanisms
of
developmental
plasticity
metabolic
modulation
that
underpin
adaptive
traits
acclimation
responses
to
waterlogging
root
systems
submergence
aerial
tissues.
This
includes
insights
into
processes
enhance
ventilation
submerged
organs.
At
the
intersection
between
metabolism
growth,
survival
strategies
have
evolved
involving
an
ethylene‐driven
gibberellin‐enhanced
module
regulates
Opposing
regulation
this
pathway
is
facilitated
by
a
subgroup
ethylene‐response
transcription
factors
(ERFs),
which
include
members
require
low
O
2
or
nitric
oxide
(NO)
conditions
for
their
stabilization.
These
control
genes
encoding
enzymes
required
anaerobic
as
well
proteins
fine‐tune
function
turnover.
Other
at
seed,
seedling
mature
stages
under
are
reviewed,
findings
demonstrating
true
endurance
ability
restore
following
deluge.
Finally,
highlight
molecular
obtained
from
variation
domesticated
wild
species
occupy
different
hydrological
niches,
emphasizing
value
understanding
efforts
stabilize
crop
yields
flood‐prone
environments.
Contents
57
I.
Introduction
58
II.
Root
acclimations
promote
aeration
60
III.
Regulating
reaeration
active
emergence
Rumex
palustris
Oryza
sativa
62
IV.
Limiting
starvation
with
gas
films
underwater
photosynthesis
64
V.
Key
low‐O
stress
65
VI.
Managing
quiescence
during
67
VII.
After
deluge
68
VIII.
Perspective
69
Acknowledgements
References