Nature Communications,
Journal Year:
2016,
Volume and Issue:
7(1)
Published: Nov. 11, 2016
Abstract
The
changes
in
extreme
rainfall
associated
with
a
warming
climate
have
drawn
significant
attention
recent
years.
Mounting
evidence
shows
that
sub-daily
convective
extremes
are
increasing
faster
than
the
rate
of
change
atmospheric
precipitable
water
capacity
climate.
However,
response
precipitation
depends
on
type
storm
supported
by
meteorological
environment.
Here
using
long-term
satellite,
surface
radar
and
rain-gauge
network
data
reanalyses,
we
show
observed
increases
springtime
total
central
United
States
dominated
mesoscale
systems
(MCSs),
largest
storm,
increased
frequency
intensity
long-lasting
MCSs.
A
strengthening
southerly
low-level
jet
its
moisture
transport
Central/Northern
Great
Plains,
overall
climatology
particularly
days
MCSs,
accounts
for
produced
these
storms.
Journal of Climate,
Journal Year:
2015,
Volume and Issue:
28(17), P. 6938 - 6959
Published: July 22, 2015
Abstract
Quantile
mapping
bias
correction
algorithms
are
commonly
used
to
correct
systematic
distributional
biases
in
precipitation
outputs
from
climate
models.
Although
they
effective
at
removing
historical
relative
observations,
it
has
been
found
that
quantile
can
artificially
corrupt
future
model-projected
trends.
Previous
studies
on
the
modification
of
trends
by
have
focused
mean
quantities,
with
less
attention
paid
extremes.
This
article
investigates
extent
which
modify
global
model
(GCM)
and
extremes
indices.
First,
a
algorithm,
delta
(QDM),
explicitly
preserves
changes
quantiles
is
presented.
QDM
compared
synthetic
data
detrended
(DQM),
designed
preserve
mean,
standard
(QM).
Next,
methods
applied
phase
5
Coupled
Model
Intercomparison
Project
(CMIP5)
daily
projections
over
Canada.
Performance
assessed
based
indices
results
generalized
extreme
value
analysis
annual
maxima.
QM
inflate
magnitude
respect
raw
GCM,
often
substantially,
as
DQM
especially
QDM.
The
degree
corruption
GCM
particularly
large
for
long
period
return
values.
By
2080s,
excess
+500%
conditions
noted
some
locations
20-yr
values,
maximum
nearing
+240%
+140%,
respectively,
whereas
never
projected
exceed
+120%.
Reviews of Geophysics,
Journal Year:
2015,
Volume and Issue:
53(2), P. 323 - 361
Published: April 28, 2015
Abstract
Regional
climate
modeling
using
convection‐permitting
models
(CPMs;
horizontal
grid
spacing
<4
km)
emerges
as
a
promising
framework
to
provide
more
reliable
information
on
regional
local
scales
compared
traditionally
used
large‐scale
(LSMs;
>10
km).
CPMs
no
longer
rely
convection
parameterization
schemes,
which
had
been
identified
major
source
of
errors
and
uncertainties
in
LSMs.
Moreover,
allow
for
accurate
representation
surface
orography
fields.
The
drawback
is
the
high
demand
computational
resources.
For
this
reason,
first
CPM
simulations
only
appeared
decade
ago.
In
study,
we
aim
common
basis
by
giving
holistic
review
topic.
most
important
components
such
physical
parameterizations
dynamical
formulations
are
discussed
critically.
An
overview
weaknesses
an
outlook
required
future
developments
provided.
Most
importantly,
presents
consolidated
outcome
studies
that
addressed
added
value
Improvements
evident
mostly
statistics
related
deep
convection,
mountainous
regions,
or
extreme
events.
change
signals
suggest
increase
flash
floods,
changes
hail
storm
characteristics,
reductions
snowpack
over
mountains.
conclusion,
very
tool
research.
However,
coordinated
programs
crucially
needed
advance
unresolved
physics
assess
full
potential
CPMs.
Scientific Reports,
Journal Year:
2019,
Volume and Issue:
9(1)
Published: Nov. 5, 2019
The
intensity
of
the
heaviest
extreme
precipitation
events
is
known
to
increase
with
global
warming.
How
often
such
occur
in
a
warmer
world
however
less
well
established,
and
combined
effect
changes
frequency
on
total
amount
rain
falling
as
much
explored,
spite
potentially
large
societal
impacts.
Here,
we
employ
observations
climate
model
simulations
document
strong
increases
frequencies
occurring
decadal
timescales.
Based
find
that
from
these
intense
almost
doubles
per
degree
warming,
mainly
due
frequency,
while
are
relatively
weak,
accordance
previous
studies.
This
shift
towards
stronger
seen
models,
strength
-
hence
rareness
event.
results,
project
if
historical
trends
continue,
most
observed
today
likely
double
occurrence
for
each
further
Changes
this
magnitude
dramatically
than
more
widely
communicated
mean
precipitation.
Philosophical Transactions of the Royal Society B Biological Sciences,
Journal Year:
2017,
Volume and Issue:
372(1723), P. 20160135 - 20160135
Published: May 8, 2017
Robust
evidence
exists
that
certain
extreme
weather
and
climate
events,
especially
daily
temperature
precipitation
extremes,
have
changed
in
regard
to
intensity
frequency
over
recent
decades.
These
changes
been
linked
human-induced
change,
while
the
degree
which
change
impacts
an
individual
event
(ECE)
is
more
difficult
quantify.
Rapid
progress
attribution
has
recently
made
through
improved
understanding
of
observed
simulated
variability,
methods
for
advances
numerical
modelling.
Attribution
events
stronger
compared
with
other
types,
notably
those
related
hydrological
cycle.
Recent
ECEs,
both
observations
their
representation
state-of-the-art
models,
open
new
opportunities
assessing
effect
on
human
natural
systems.
Improved
spatial
resolution
global
models
statistical
dynamical
downscaling
now
provide
climatic
information
at
appropriate
temporal
scales.
Together
continued
development
Earth
System
Models
simulate
biogeochemical
cycles
interactions
biosphere
increasing
complexity,
these
make
it
possible
develop
a
mechanistic
how
ECEs
affect
biological
processes,
ecosystem
functioning
adaptation
capabilities.
Limitations
observational
network,
physical
system
parameters
even
so
long-term
ecological
monitoring,
hampered
bio-physical
across
range
New
modulate
structure
arise
from
better
scientific
coupled
technological
observing
systems
instrumentation.
This
article
part
themed
issue
‘Behavioural,
evolutionary
responses
events’.
Current Climate Change Reports,
Journal Year:
2015,
Volume and Issue:
1(2), P. 49 - 59
Published: April 20, 2015
The
response
of
precipitation
extremes
to
climate
change
is
considered
using
results
from
theory,
modeling,
and
observations,
with
a
focus
on
the
physical
factors
that
control
response.
Observations
simulations
models
show
intensify
in
warming
climate.
However,
sensitivity
remains
uncertain
when
convection
important,
it
may
be
higher
tropics
than
extratropics.
Several
contributions
govern
extremes.
thermodynamic
contribution
robust
well
understood,
but
theoretical
understanding
microphysical
dynamical
still
being
developed.
Orographic
snowfall
respond
differently
other
require
particular
attention.
Outstanding
research
challenges
include
influence
mesoscale
convective
organization,
dependence
duration
considered,
need
better
constrain
tropical
warming.
Water Resources Research,
Journal Year:
2019,
Volume and Issue:
55(6), P. 4901 - 4914
Published: May 9, 2019
Abstract
Global
warming
is
expected
to
change
the
regime
of
extreme
precipitation.
Physical
laws
translate
increasing
atmospheric
heat
into
water
content
that
drives
precipitation
changes.
Within
literature,
general
agreement
changing,
yet
different
assessment
methods,
data
sets,
and
study
periods
may
result
in
patterns
rates
change.
Here
we
perform
a
global
analysis
8,730
daily
records
focusing
on
1964–2013
period
when
accelerates.
We
introduce
novel
N
largest
extremes
having
complete
years
within
period.
Based
these
extremes,
which
represent
more
accurately
heavy
than
annual
maxima,
form
time
series
their
frequency
mean
magnitude.
The
offers
new
insights
reveals
(1)
zonal
trends
are
highly
unlikely
under
assumption
stationarity
(2)
magnitude
changes
not
as
evident.
Frequency
reveal
coherent
spatial
pattern
with
being
detected
large
parts
Eurasia,
North
Australia,
Midwestern
United
States.
Globally,
over
last
decade
studied
find
7%
events
number.
Finally,
report
correlated
frequency.