Journal of Geophysical Research Atmospheres,
Journal Year:
2019,
Volume and Issue:
125(1)
Published: Dec. 18, 2019
Abstract
This
work
for
the
first
time
analyzed
vertical
structures
of
different
stages
Meiyu
precipitation
systems
over
Yangtze‐Huai
River
Valley
in
central
China
using
measurements
and
retrievals
from
Global
Precipitation
Measurement
Mission
Dual‐Frequency
Radar
(GPM‐DPR)
Feng
Yun
satellites.
GPM‐DPR
‐
retrieved
near‐surface
rain
drop
size
distributions
were
validated
against
surface
disdrometer
showed
good
agreement.
Then
we
three
cases
Integrative
Monsoon
Frontal
Rainfall
Experiment
to
demonstrate
characteristics
convective
stratiform
(SP)
developing,
mature,
dissipating
systems,
respectively.
For
statistical
analysis,
all
during
period
2016–2018
detected
by
collected
classified
into
types
stages.
In
regions
coalescence
slightly
overwhelms
breakup
and/or
evaporation
processes,
but
it
was
dominant
when
raindrops
fall.
There
large
numbers
ice
particles
developing
stage
due
strong
updrafts
abundant
moisture,
whereas
there
both
liquid
mature
stage.
The
SP
examined
this
study
similar
those
ocean
high
relative
humidity
mountainous
west
USA.
findings
stage‐dependent
provide
better
understanding
evolution
monsoon
frontal
precipitation,
as
well
associated
microphysical
properties,
insights
improve
parameterization
future
models.
Journal of Geophysical Research Atmospheres,
Journal Year:
2019,
Volume and Issue:
124(23), P. 13026 - 13054
Published: Oct. 23, 2019
Abstract
Aerosols
have
significant
and
complex
impacts
on
regional
climate
in
East
Asia.
Cloud‐aerosol‐precipitation
interactions
(CAPI)
remain
most
challenging
studies.
The
quantitative
understanding
of
CAPI
requires
good
knowledge
aerosols,
ranging
from
their
formation,
composition,
transport,
radiative,
hygroscopic,
microphysical
properties.
A
comprehensive
review
is
presented
here
centered
the
based
chiefly,
but
not
limited
to,
publications
special
section
named
EAST‐AIRcpc
concerning
(1)
observations
aerosol
loading
properties,
(2)
relationships
between
aerosols
meteorological
variables
affecting
CAPI,
(3)
mechanisms
behind
(4)
quantification
impact
climate.
Heavy
Asia
has
radiative
effects
by
reducing
surface
radiation,
increasing
air
temperature,
lowering
boundary
layer
height.
key
factor
absorption,
which
particularly
strong
central
China.
This
absorption
can
a
wide
range
such
as
creating
an
imbalance
forcing
at
top
bottom
atmosphere,
leading
to
inconsistent
retrievals
cloud
space‐borne
ground‐based
instruments.
Aerosol
delay
or
suppress
initiation
development
convective
clouds
whose
microphysics
be
further
altered
effect
aerosols.
For
same
thickness,
likelihood
precipitation
influenced
aerosols:
suppressing
light
rain
enhancing
heavy
rain,
delaying
intensifying
thunderstorms,
onset
isolated
showers
parts
Rainfall
become
more
inhomogeneous
extreme
heavily
polluted
urban
regions.
Journal of Geophysical Research Atmospheres,
Journal Year:
2021,
Volume and Issue:
126(8)
Published: April 7, 2021
Abstract
A
new
methodology
is
developed
to
construct
a
global
(60°S–60°N)
long‐term
(2000–2019)
high‐resolution
(∼10‐km
h)
mesoscale
convective
system
(MCS)
database
by
tracking
MCS
jointly
using
geostationary
satellite
infrared
brightness
temperature
(
T
b
)
and
precipitation
feature
(PF)
characteristics
from
the
Integrated
Multi‐satellitE
Retrievals
for
GPM
data
sets.
Independent
validation
shows
that
satellite‐based
set
able
reproduce
important
statistics
derived
ground‐based
radar
network
observations
in
United
States
China.
We
show
carefully
considering
key
PF
addition
signatures,
method
significantly
improves
upon
previous
‐only
methods
detecting
MCSs
midlatitudes
all
seasons.
Results
account
over
50%
of
annual
total
rainfall
across
most
tropical
belt
selected
regions
midlatitudes,
with
strong
seasonality
many
globe.
The
allows
Lagrangian
aspects
such
as
lifetime
translational
speed
direction
be
analyzed.
longest‐lived
preferentially
occur
subtropical
oceans.
land
have
higher
cloud‐tops
associated
more
intense
convection,
oceanic
much
production.
While
are
observed
globe,
there
fundamental
differences
their
dynamic
thermodynamic
structures
warrant
better
understanding
processes
control
evolution.
This
provides
significant
opportunities
observational
modeling
studies
MCSs,
characteristics,
roles
regional
water
energy
cycles,
well
hydrologic
other
impacts.
Journal of Meteorological Research,
Journal Year:
2022,
Volume and Issue:
36(1), P. 6 - 25
Published: Feb. 1, 2022
In
this
study,
the
unprecedented
extreme
rainfall
event
during
19–20
July
2021,
which
caused
devastating
flooding
in
Zhengzhou
City
and
its
nearby
areas,
is
examined
based
on
observational
data
analysis
WRF
model
40-h
simulations
1-km
horizontal
resolution.
The
results
show
that
successfully
reproduces
(i)
major
synoptic-scale
weather
systems
(i.e.,
western
Pacific
subtropical
high,
Tibetan
two
typhoons,
Huang-Huai
cyclone),
(ii)
convective
initiation
along
east
to
north
edge
of
Songshan
Mountain,
where
orographic
lifting
obvious,
(iii)
subsequent
formation
storm
producing
Zhengzhou.
particular,
generates
maximum
rate
233
mm
h−1
accumulated
704
mm,
corresponding
well
observed
values
201.9
818
at
nearly
timing
location.
Importantly,
an
intense
quasi-stationary,
well-organized
meso-γ-scale
system,
surrounded
by
arc-shaped
convergence
zone,
allowing
development
updrafts
a
three-quarter
circle
around
way
similar
"multidirectional
pumping,"
attracting
all
associated
precipitation
overlaid
concentrated
into
same
trailing
region
generate
hourly
over
Our
study
emphasizes
significant
contribution
unique
dynamic
structure
system
record-high
rainfall.
A
possible
mechanism
for
short-time
production
proposed.
That
is,
zone
mesoscale
acting
like
multidirectional
pumps,
transports
from
different
directions
region,
thus
produces
gained
herein
may
shed
new
light
better
understanding
forecasting
Reviews of Geophysics,
Journal Year:
2020,
Volume and Issue:
58(4)
Published: Oct. 31, 2020
Abstract
Earth's
tropical
and
subtropical
rainbands,
such
as
Intertropical
Convergence
Zones
(ITCZs)
monsoons,
are
complex
systems,
governed
by
both
large‐scale
constraints
on
the
atmospheric
general
circulation
regional
interactions
with
continents
orography,
coupled
to
ocean.
Monsoons
have
historically
been
considered
sea
breeze
circulations,
driven
land‐sea
contrast.
More
recently,
a
perspective
has
emerged
of
global
monsoon,
global‐scale
solstitial
mode
that
dominates
annual
variation
precipitation.
This
results
from
seasonal
overturning
migration
associated
convergence
zone.
Regional
subsystems
embedded
in
this
localized
surface
boundary
conditions.
Parallel
this,
much
theoretical
progress
made
fundamental
dynamics
Hadley
cells
zones
via
use
hierarchical
modeling
approaches,
including
aquaplanets.
Here
we
review
explore
extent
which
these
advances
can
help
synthesize
theory
observations
better
understand
differing
characteristics
monsoons
their
responses
certain
forcings.
After
summarizing
dynamical
energetic
balances
distinguish
an
ITCZ
show
framework
provides
strong
support
for
migrating
zone
picture
allows
be
identified
momentum
energy
budgets.
Limitations
current
theories
discussed,
need
understanding
influence
zonal
asymmetries
transients
circulation.
Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences,
Journal Year:
2021,
Volume and Issue:
379(2195), P. 20190546 - 20190546
Published: March 1, 2021
Mesoscale
convective
systems
(MCSs)
are
complexes
of
thunderstorms
that
become
organized
and
cover
hundreds
kilometres
over
several
hours.
MCSs
prolific
rain
producers
in
the
tropics
mid-latitudes
major
cause
warm-season
flooding.
Traditionally,
climate
models
have
difficulties
simulating
partly
due
to
misrepresentation
complex
process
interactions
operate
across
a
large
range
scales.
Significant
improvements
been
found
kilometre-scale
explicitly
simulate
deep
convection.
However,
these
grey
zone
turbulent
motion
known
deficiencies
small-scale
processes
(e.g.
entrainment,
vertical
mass
transport).
Here,
we
perform
mid-latitude
idealized
ensemble
MCS
simulations
under
current
future
conditions
three
atmospheric
regimes:
hydrostatic
(12
km
horizontal
grid
spacing;
Δx),
non-hydrostatic
(Δx
=
4,
2
1
km)
eddy
scale
500
m
250
m).
Our
results
show
dramatic
improvement
precipitation,
movement,
cold
pools,
cloud
properties
when
transitioning
from
12
4
Δx.
Decreasing
Δx
beyond
modest
except
for
up-
downdraft
sizes,
average
fluxes,
top
height
temperature,
which
continue
change.
Most
important
modelling
is
reliably
capture
most
change
signals
compared
those
runs.
Significantly
different
runs
overestimate
extreme
precipitation
changes
by
up
100%.
This
article
part
discussion
meeting
issue
'Intensification
short-duration
rainfall
extremes
implications
flash
flood
risks'.
Meteorological Monographs,
Journal Year:
2019,
Volume and Issue:
59, P. 13.1 - 13.67
Published: Jan. 1, 2019
Abstract
Over
the
past
100
years,
collaborative
effort
of
international
science
community,
including
government
weather
services
and
media,
along
with
associated
proliferation
environmental
observations,
improved
scientific
understanding,
growth
technology,
has
radically
transformed
forecasting
into
an
effective
global
regional
prediction
capability.
This
chapter
traces
evolution
forecasting,
starting
in
1919
[when
American
Meteorological
Society
(AMS)
was
founded],
over
four
eras
separated
by
breakpoints
at
1939,
1956,
1985.
The
current
state
could
not
have
been
achieved
without
essential
collaboration
within
among
countries
pursuing
common
Earth-system
challenge.
AMS
itself
had
a
strong
role
enabling
this
collaboration.
Journal of Hydrometeorology,
Journal Year:
2019,
Volume and Issue:
21(1), P. 39 - 57
Published: Nov. 22, 2019
Abstract
Mesoscale
convective
systems
(MCSs)
play
an
important
role
in
water
and
energy
cycles
as
they
produce
heavy
rainfall
modify
the
radiative
profile
tropics
midlatitudes.
An
accurate
representation
of
MCSs’
is
therefore
crucial
understanding
their
impact
on
climate
system.
The
V06B
Integrated
Multisatellite
Retrievals
from
Global
Precipitation
Measurement
(IMERG)
half-hourly
precipitation
final
product
a
useful
tool
to
study
characteristics
MCSs
because
its
global
coverage
fine
spatiotemporal
resolutions.
However,
errors
uncertainties
IMERG
should
be
quantified
before
applying
it
hydrology
applications.
This
evaluates
performance
capturing
detecting
central
eastern
United
States
during
3-yr
period
against
radar-based
Stage
IV
product.
tracked
are
divided
into
four
seasons
analyzed
separately
for
both
datasets.
shows
wet
bias
total
but
dry
hourly
mean
all
due
false
classification
nonprecipitating
pixels
precipitating.
These
alarm
events
possibly
caused
by
evaporation
under
cloud
base
or
misrepresentation
MCS
cold
anvil
regions
precipitating
clouds
algorithm.
agrees
reasonably
well
with
terms
seasonal
spatial
distribution
diurnal
cycle
precipitation.
A
relative
humidity
(RH)-based
correction
has
been
applied
product,
which
helps
reduce
number
improves
overall
respect
IV.
Geophysical Research Letters,
Journal Year:
2019,
Volume and Issue:
46(22), P. 13281 - 13289
Published: Oct. 16, 2019
Abstract
The
local‐scale
precipitation
(LSP)
is
mainly
driven
by
thermal
convection.
Here
we
reveal
a
decreasing
trend
in
the
summertime
LSP
frequency
over
both
China
and
United
States
utilizing
hourly
rain
gauge
data
from
1981
to
2012.
contrasting
aerosol
likely
contributes
this
same
declining
of
countries.
As
optical
depth
(AOD)
goes
beyond
turning
zone
0.25–0.30,
impact
on
changes
invigoration
suppression.
mean
AOD
generally
less
larger
than
range
opposite
trends
States,
respectively,
which
accounts
for
hours
two
observed
boomerang
shape
points
importance
loading,
matters
as
much
as,
if
not
more
trend,
thereby
potentially
serving
constraint
climate
model
evaluation.