Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(21), P. 13987 - 14002
Published: Nov. 9, 2023
Abstract.
The
spatiotemporal
variation
of
fog
reflects
the
complex
interactions
among
fog,
boundary
layer
thermodynamics
and
synoptic
systems.
Previous
studies
revealed
that
can
present
a
fast
spatial
propagation
feature
attribute
it
to
low-level
jet
(BLLJ),
but
effect
BLLJ
on
is
not
quantitatively
understood.
Here
we
analyze
large-scale
event
in
Jiangsu,
China,
from
20
21
January
2020.
Satellite
retrievals
show
propagates
southeast
coastal
area
northwest
inland
with
speed
9.6
m
s−1,
which
3
times
larger
than
ground
wind
speeds.
meteorologies
are
insufficient
explain
propagation,
further
investigated
by
Weather
Research
Forecasting
model
(WRF)
simulations.
could
be
attributed
occurring
between
50
500
m,
because
speeds
(10
s−1)
directions
(southeast)
core
consistent
propagation.
Through
sensitive
experiments
process
analysis,
three
possible
mechanisms
revealed:
(1)
abundant
oceanic
moisture
transported
inland,
increasing
humidity
promoting
condensation;
(2)
warm
air
enhancing
inversion
favoring
accumulation;
(3)
advection
probably
promotes
low-stratus
formation,
later
subsides
become
turbulent
mixing
droplets.
would
decrease
notably
6.4
s−1
(66
%)
if
BLLJ-related
advections
were
turned
off.
Geophysical Research Letters,
Journal Year:
2025,
Volume and Issue:
52(7)
Published: March 31, 2025
Abstract
Relative
dispersion
(
ε
),
as
a
parameter
characterizing
droplet
spectral
shape,
exerts
considerable
impact
on
cloud
radiation
and
precipitation
processes,
its
accurate
parameterization
is
urgently
needed
in
models.
Current
parameterizations,
which
are
based
number
concentration
or
simply
set
constants,
inadequate
to
satisfy
the
demand.
This
study
shows,
utilizing
in‐situ
fog
observations
from
five
underlying
surface
regions
(urban,
suburban,
mountainous,
coastal
rainforest)
of
China,
that
uniformly
stably
manifests
initially
increasing
then
decreasing
volume‐mean
diameter
increases
across
these
regions.
Based
this
relationship,
established,
exhibits
improved
predictive
capabilities
evaluating
both
albedo
effect
lifetime
effect.
The
expected
enhance
simulation
accuracy
minimize
discrepancy
between
observed
simulated
precipitation,
particularly
for
weather
climate
models
commonly
use
double‐moment
microphysical
schemes.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(14), P. 8169 - 8186
Published: July 21, 2023
Abstract.
Clouds
exhibit
a
wide
range
of
vertical
morphologies
that
are
regulated
by
distinct
atmospheric
dynamics
and
thermodynamics
related
to
diversity
microphysical
properties
radiative
effects.
In
this
study,
the
new
CERES-CloudSat-CALIPSO-MODIS
(CCCM)
RelD1
dataset
is
used
investigate
morphology
spatial
distribution
different
cloud
structure
(CVS)
types
during
2007–2010.
The
combined
active
passive
satellites
provide
more
precise
CVS
than
those
only
based
on
imagers
or
microwave
radiometers.
We
group
clouds
into
12
classes
how
they
located
overlapping
in
three
standard
layers
with
pressure
thresholds
440
680
hPa.
For
each
types,
global
average
effects
(CREs)
at
top
atmosphere,
within
atmosphere
surface,
as
well
heating
rate
(CHR)
profiles
examined.
observations
subsequently
evaluate
variations
total,
high-,
middle-
low-level
fractions
CMIP6
models.
“historical”
experiment
1850–2014
two
scenarios
(ssp245
ssp585)
2015–2100
analyzed.
observational
results
show
substantial
difference
pattern
among
greatest
contrast
between
high
low
clouds.
Single-layer
fraction
almost
4
times
larger
multi-layer
fraction,
significant
geographic
differences
associated
clearly
distinguishable
regimes,
showing
regionally
confined.
CREs
reveal
four
CVSs
warm
planet,
while
eight
them
cool
it.
longwave
component
drives
net
CHR
profile,
curved
intricate
single-layer
clouds,
resulting
complex
thermal
stratifications.
According
long-term
analysis
from
CMIP6,
projected
total
decreases
faster
over
land
ocean.
ocean
increase
significantly,
but
other
continue
decrease,
helping
offset
decrease
oceanic
fraction.
Moreover,
it
concluded
may
not
be
significantly
altered
climate
change,
influenced.
Our
findings
suggest
observed
should
emphasized
future
better
understand
responses
anthropogenic
forcing
change.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(17), P. 9873 - 9890
Published: Sept. 6, 2023
Abstract.
Aerosol–cloud
interaction
(ACI)
in
fog
and
planetary
boundary
layer
(PBL)
conditions
plays
critical
roles
the
life
cycle.
However,
it
is
not
clear
how
ACI
first
(Fog1)
affects
PBL
subsequently
second
(Fog2),
which
important
information
for
understanding
between
PBL,
as
well
their
effects
on
properties.
To
fill
this
knowledge
gap,
we
simulate
two
successive
radiation
events
Yangtze
River
Delta,
China,
using
Weather
Research
Forecasting
model
coupled
with
Chemistry
(WRF-Chem).
Our
simulations
indicate
that
conducive
to
Fog2
formation
are
affected
by
high
aerosol
loading
Fog1;
subsequently,
promotes
Fog2,
resulting
a
higher
liquid
water
content,
droplet
number
concentration,
smaller
size,
larger
optical
depth,
wider
distribution,
longer
lifetime
than
Fog1.
This
phenomenon
related
following
physical
factors.
The
factor
involves
meteorological
formation,
including
low
temperature,
humidity,
stability.
feedbacks
microphysics
radiative
cooling.
A
concentration
increases
path
thereby
enhancing
long-wave
cooling
condensation
near
top.
third
macrophysics,
radiation,
turbulence.
top
presents
stronger
base,
weakens
temperature
inversion
strengthens
turbulence,
ultimately
increasing
fog-top
height
area.
In
summary,
under
polluted
conditions,
postpones
dissipation
of
Fog1
owing
these
generates
more
those
prior
These
promote
earlier
further
strengthening
Fog2.
findings
studying
aerosols,
fog,
PBL;
moreover,
they
shed
new
light
ACI.
Sensors,
Journal Year:
2023,
Volume and Issue:
23(15), P. 6891 - 6891
Published: Aug. 3, 2023
In
this
work,
we
introduce
a
novel
approach
to
model
the
rain
and
fog
effect
on
light
detection
ranging
(LiDAR)
sensor
performance
for
simulation-based
testing
of
LiDAR
systems.
The
proposed
methodology
allows
simulation
using
rigorous
applications
Mie
scattering
theory
time
domain
transient
point
cloud
levels
spatial
analyses.
analysis
permits
us
benchmark
virtual
signal
attenuation
signal-to-noise
ratio
(SNR)
caused
by
droplets.
addition,
rate
(DR),
false
(FDR),
distance
error
derror
due
droplets
are
evaluated
level.
mean
absolute
percentage
(MAPE)
is
used
quantify
real
measurement
results
measurements
match
well
if
simulated
distributions
same.
degrades
more
under
influence
than
in
rain.
Quarterly Journal of the Royal Meteorological Society,
Journal Year:
2024,
Volume and Issue:
150(762), P. 2690 - 2711
Published: June 24, 2024
Abstract
With
the
changing
climate,
study
of
fog
formation
is
essential
due
to
impact
complexity
natural
and
anthropogenic
aerosols.
The
evolution
droplet
size
distribution
in
presence
different
aerosol
species
remains
poorly
understood.
To
make
progress
towards
reducing
uncertainty
forecasts,
Eulerian–Lagrangian
particle‐based
small‐scale
model
for
diffusional
growth
droplets
used
better
understand
activation
growth.
simulations
are
performed
using
observed
data
from
Winter
Fog
Experiment
over
Indira
Gandhi
International
Airport,
New
Delhi.
microphysical
properties,
such
as
number
concentrations
(Nd)
liquid
water
content
(LWC),
important
simulation,
evaluated
gain
more
insights.
have
shown
properties
at
evolutionary
stages.
Nd
effective
radius
change
with
variations
LWC
chemistries
(i.e.,
organics,
mix,
inorganic).
calculated
visibility
small
scale
also
variation
LWC.
This
compared
an
existing
parametrization
parcel–direct
numerical
simulation
calculation.
hygroscopicity
,
which
highly
related
aerosols
condensation
nuclei,
taken
into
account
demonstrate
contribution
chemistry
formation.
results
highlight
that
prediction
regulated
by
species.