Authorea (Authorea),
Journal Year:
2023,
Volume and Issue:
unknown
Published: Nov. 8, 2023
A
formulation
based
on
the
anelastic
approximation
yields
time-dependent
simulations
of
convective
updrafts,
downdrafts
and
other
aspects
convection-such
as
stratiform
layers-under
reasonably
flexible
geometry
assumptions.
Termed
entities
(ACEs),
such
realizations
can
aid
understanding
processes,
potentially
provide
building
blocks
for
parameterization
at
a
complexity
between
steady-plume
models
cloud-resolving
simulations.
Even
cases
deliberately
formulated
to
comparison
traditional
plume,
ACE
behavior
differs
substantially
because
dynamic
entrainment,
detrainment
nonhydrostatic
perturbation
pressure
are
consistently
included.
Entrainment
varies
with
evolution
entity
but
akin
deep-inflow
effects
noted
in
observations
emerges
naturally.
The
magnitude
mass
flux
nonlocal
included
is
smaller
than
corresponding
model.
solutions
do
not
necessarily
approach
steady
state
even
fixed
environment
exhibit
chains
rising
thermals,
episodic
deep
convection.
inclusion
dynamics
allows
developing
updraft
tunnel
through
layers
substantial
inhibition
(CIN).
For
nighttime
continental
convection
using
GoAmazon
soundings,
this
found
greatly
reduce
effect
surface-inversion
CIN.
observed
cold
top
seen
an
inherent
property
solution,
both
transient,
phase
persistent
feature
mature
An
embedded
configuration
cloud
formation
by
modified
feedbacks
during
grid-scale
adjustment
process.
SIGNIFICANCE
STATEMENT:
Convective
storms
cause
hazardous
events
flooding,
often
economic
losses.
Forecasting
how
they
change
warming
climate
mitigation
planning
hard.
In
modern
numerical
weather
models,
one
issue
standing
out
that
model
cannot
satisfactorily
simulate
over
land
commonly
over,
instance,
North
American
Great
Plains
or
Amazon
basin.
Here,
we
propose
new
model-named
(ACE)-with
two
purposes
mind:
(i)
be
useful
improving
models;
(ii)
help
understand
processes
general.
Preliminary
results
covered
here
promising,
especially
problem.
Authorea (Authorea),
Journal Year:
2023,
Volume and Issue:
unknown
Published: Feb. 14, 2023
The
small-scale
mixing
of
clouds
with
their
environment
is
an
essential
cloud
process.
Following
entrainment
event,
turbulent
breaks
down
the
entrained
air
and
homogenizes
it
cloud,
covering
multiple
orders
magnitude
in
lengthscales
from
entraining
eddies
(∼
100
m)
to
Kolmogorov
length
1
mm).
character
this
process,
traditionally
categorized
into
homogeneous
inhomogeneous
scenarios,
can
affect
microphysical
composition
clouds,
commensurate
impacts
on
large-scale
properties
such
as
albedo
lifetime.
Based
current
physical
understanding
cloudy
cloud-free
air,
chapter
will
summarize
basic
theories
describing
By
considering
wide
range
involved
scales,
we
outline
different
observational
numerical
approaches
used
investigate
process
well
methods
parameterize
models.
Finally,
review
focusing
microscale
changes
droplet
size
distribution
macroscale
effects
relevant
our
climate
system.
Authorea (Authorea),
Journal Year:
2024,
Volume and Issue:
unknown
Published: March 5, 2024
Stratocumulus
clouds,
a
key
component
of
global
climate,
are
sensitive
to
aerosol
properties.
Aerosol-cloud-precipitation
interactions
in
these
clouds
influence
their
closed-to-open
cell
dynamical
transition
and
hence
cloud
cover
radiative
forcing.
This
study
uses
large-eddy
simulations
with
Lagrangian
super-particle
bin
microphysics
schemes
investigate
impacts
scavenging
physical
processing
by
on
drizzle
initiation
the
cellular
process.
The
simulation
using
explicit
representation
cloud-borne
shows
significant
that
precipitation
generation
consequently
transition.
Sensitivity
scheme
comparison
suggest
reduced
concentration
due
is
primary
microphysical
catalyst
for
enhanced
scheme.
However,
changes
distribution
shape
through
also
contribute
appreciably
differences
rate.
Thus,
both
drive
earlier
rain
formation
open
cells
microphysics.
highlights
shortcoming
Eulerian
producing
smaller
mean
drop
radius
water
mixing
ratios
owing
numerical
diffusion.
Initially
larger
induce
faster
development
compared
A
positive
feedback
turn
accelerates
removal
further
production
and,
consequently,
droplet
number,
increased
size,
spectral
width.
Geophysical Research Letters,
Journal Year:
2023,
Volume and Issue:
50(3)
Published: Jan. 9, 2023
Abstract
Spectral
width
of
the
cloud
droplet
spectrum
is
important
for
radiative
properties
and
drizzle/rain
development
in
warm
ice‐free
clouds.
We
use
an
adiabatic
rising
parcel
model
to
study
activation
diffusional
growth
droplets,
focusing
on
spectral
evolution,
contrasting
clean
polluted
environments.
A
comprehensive
equation
used
that
includes
kinetic,
solute,
surface
tension
effects.
show
those
effects
have
appreciable
impact
evolution
above
base.
Without
effects,
area
standard
deviation
should
not
change
once
completed.
In
contrast,
simulation
results
does
increase
with
height,
especially
weak
updrafts
Implications
modeling,
applying
conventional
bin
microphysics,
are
discussed.
Journal of Geophysical Research Atmospheres,
Journal Year:
2023,
Volume and Issue:
128(16)
Published: Aug. 7, 2023
Abstract
The
activation
of
aerosol
particles
and
its
contribution
to
cloud
droplet
size
distributions
in
shallow
cumulus
clouds
are
investigated
by
analyzing
the
field
simulation
results
using
a
Lagrangian
model
coupled
with
large
eddy
simulation,
which
allows
explicit
simulations
tracking
each
super‐droplet.
Analysis
is
focused
on
differences
activations
for
following
central
updraft
from
base
(CB)
entrained
above
(EA).
Time
series
various
variables
individual
confirm
distinctive
nature
CB
EA
activation.
Strong
supersaturation
fluctuations
induced
entrainment
turbulent
mixing
at
edges
cause
most
be
deactivated
soon
after
activation,
substantially
limiting
their
lifetime
growth
relative
particles.
Most
net
activation—the
difference
between
deactivation—occurs
vanishes
aloft.
Cloud
spectra
follow
theoretical
prediction
high
conditions,
although
proportional
constant
smaller
because
particle
deactivation.
deviate
low
conditions
since
they
affected
transport
activated
elsewhere.
Authorea (Authorea),
Journal Year:
2023,
Volume and Issue:
unknown
Published: Nov. 8, 2023
A
formulation
based
on
the
anelastic
approximation
yields
time-dependent
simulations
of
convective
updrafts,
downdrafts
and
other
aspects
convection-such
as
stratiform
layers-under
reasonably
flexible
geometry
assumptions.
Termed
entities
(ACEs),
such
realizations
can
aid
understanding
processes,
potentially
provide
building
blocks
for
parameterization
at
a
complexity
between
steady-plume
models
cloud-resolving
simulations.
Even
cases
deliberately
formulated
to
comparison
traditional
plume,
ACE
behavior
differs
substantially
because
dynamic
entrainment,
detrainment
nonhydrostatic
perturbation
pressure
are
consistently
included.
Entrainment
varies
with
evolution
entity
but
akin
deep-inflow
effects
noted
in
observations
emerges
naturally.
The
magnitude
mass
flux
nonlocal
included
is
smaller
than
corresponding
model.
solutions
do
not
necessarily
approach
steady
state
even
fixed
environment
exhibit
chains
rising
thermals,
episodic
deep
convection.
inclusion
dynamics
allows
developing
updraft
tunnel
through
layers
substantial
inhibition
(CIN).
For
nighttime
continental
convection
using
GoAmazon
soundings,
this
found
greatly
reduce
effect
surface-inversion
CIN.
observed
cold
top
seen
an
inherent
property
solution,
both
transient,
phase
persistent
feature
mature
An
embedded
configuration
cloud
formation
by
modified
feedbacks
during
grid-scale
adjustment
process.
SIGNIFICANCE
STATEMENT:
Convective
storms
cause
hazardous
events
flooding,
often
economic
losses.
Forecasting
how
they
change
warming
climate
mitigation
planning
hard.
In
modern
numerical
weather
models,
one
issue
standing
out
that
model
cannot
satisfactorily
simulate
over
land
commonly
over,
instance,
North
American
Great
Plains
or
Amazon
basin.
Here,
we
propose
new
model-named
(ACE)-with
two
purposes
mind:
(i)
be
useful
improving
models;
(ii)
help
understand
processes
general.
Preliminary
results
covered
here
promising,
especially
problem.