Abstract.
The
NASA
Aerosol
Cloud
meTeorology
Interactions
oVer
the
western
ATlantic
Experiment
(ACTIVATE)
produced
a
unique
dataset
for
research
into
aerosol-cloud-meteorology
interactions
with
applications
extending
from
process-based
studies
to
multi-scale
model
intercomparison
and
improvement,
remote
sensing
algorithm
assessments
advancements.
ACTIVATE
used
two
Langley
Research
Center
aircraft,
HU-25
Falcon
King
Air,
conduct
systematic
spatially
coordinated
flights
over
northwest
Atlantic
Ocean
amounting
162
joint
17
other
single-aircraft
between
2020
2022
across
all
seasons.
Data
cover
574
592
cumulative
hours
respectively.
flew
conducted
profiling
at
different
level
legs
below,
in,
just
above
boundary
layer
clouds
(<
3
km)
obtained
in
situ
measurements
of
trace
gases,
aerosol
particles,
clouds,
atmospheric
state
parameters.
In
cloud-free
conditions,
similarly
within
immediately
layer.
Air
(the
high-flyer)
approximately
~9
km
conducting
lidar
polarimeter
while
also
launching
dropsondes.
Collectively,
simultaneous
data
collected
both
aircraft
help
characterize
same
vertical
column
atmosphere.
addition
individual
instrument
files,
are
combined
“merge
files”
on
publicly
available
archive
that
created
time
resolutions
interest
(e.g.,
1,
5,
10,
15,
30,
60
s,
or
matching
an
product
start
stop
times).
This
paper
describes
flight
strategy,
complementary
products,
access
usage
details,
application
notes.
Reviews of Geophysics,
Journal Year:
2023,
Volume and Issue:
61(2)
Published: May 4, 2023
Abstract
Aerosol
forcing
uncertainty
represents
the
largest
climate
overall.
Its
magnitude
has
remained
virtually
undiminished
over
past
20
years
despite
considerable
advances
in
understanding
most
of
key
contributing
elements.
Recent
work
produced
modest
increases
only
confidence
estimate
itself.
This
review
summarizes
contributions
toward
reducing
aerosol
made
by
satellite
observations,
measurements
taken
within
atmosphere,
as
well
modeling
and
data
assimilation.
We
adopt
a
more
measurement‐oriented
perspective
than
reviews
subject
assessing
strengths
limitations
each;
gaps
possible
ways
to
fill
them
are
considered.
Currently
planned
programs
supporting
advanced,
global‐scale
surface‐based
aerosol,
cloud,
precursor
gas
modeling,
intensive
field
campaigns
aimed
at
characterizing
underlying
physical
chemical
processes
involved,
all
essential.
But
addition,
new
efforts
needed:
(a)
obtain
systematic
aircraft
situ
capturing
multi‐variate
probability
distribution
functions
particle
optical,
microphysical,
properties
(and
associated
estimates),
co‐variability
with
meteorology,
for
major
airmass
types;
(b)
conceive,
develop,
implement
suborbital
(aircraft
plus
surface‐based)
program
systematically
quantifying
cloud‐scale
microphysics,
cloud
optical
properties,
cloud‐related
vertical
velocities
aerosol‐cloud
interactions;
(c)
focus
much
research
on
integrating
unique
measurements,
reduce
persistent
forcing.
Atmosphere,
Journal Year:
2022,
Volume and Issue:
13(8), P. 1242 - 1242
Published: Aug. 5, 2022
A
challenging
aspect
of
conducting
airborne
in
situ
observations
the
atmosphere
is
how
to
optimize
flight
plans
for
specific
objectives
and
constraints
associated
with
weather
restrictions.
For
aerosol-cloud
interaction
research,
two
recent
campaigns
utilized
a
“stairstepping”
approach
whereby
an
aircraft
conducts
level
legs
at
various
altitudes
while
moving
forward
each
subsequent
leg:
2019
MONterey
Aerosol
Research
Campaign
(MONARC)
over
northeast
Pacific
2020–2022
Cloud
meTeorology
Interactions
oVer
western
ATlantic
Experiment
(ACTIVATE)
northwest
Atlantic.
We
examine
homogeneity
several
atmospheric
variables
both
vertically
horizontally
marine
boundary
layer
focus
on
sub-cloud
environment.
In
well-mixed
layers,
there
was
generally
good
horizontal
vertical
potential
temperature,
winds,
water
vapor
mixing
ratio,
trace
gases,
many
aerosol
variables.
Selected
exhibited
most
variability
owing
sensitivity
humidity
near-cloud
conditions
(supermicrometer
concentrations),
coastal
pollution
gradients
(e.g.,
organic
mass),
small
spatial
scale
phenomena
such
as
new
particle
formation
(aerosol
number
concentration
particles
diameter
>3
nm).
Illustrative
cases
are
described
when
stairstepping
can
pose
issues
requiring
extra
caution
data
analysis:
(i)
poor
layers
decoupled
from
those
below;
(ii)
multiple
cloud
layers;
(iii)
fluctuating
base/top
top
heights;
(iv)
across
features
leading
sharp
right
near
coastlines
Gulf
Stream
strong
sea
surface
temperature
changes.
Results
this
study
provide
guide
future
studies
aiming
these
mission
datasets
designing
campaigns.
Earth system science data,
Journal Year:
2023,
Volume and Issue:
15(8), P. 3419 - 3472
Published: Aug. 3, 2023
Abstract.
The
NASA
Aerosol
Cloud
meTeorology
Interactions
oVer
the
western
ATlantic
Experiment
(ACTIVATE)
produced
a
unique
dataset
for
research
into
aerosol–cloud–meteorology
interactions,
with
applications
extending
from
process-based
studies
to
multi-scale
model
intercomparison
and
improvement
as
well
remote-sensing
algorithm
assessments
advancements.
ACTIVATE
used
two
Langley
Research
Center
aircraft,
HU-25
Falcon
King
Air,
conduct
systematic
spatially
coordinated
flights
over
northwest
Atlantic
Ocean,
resulting
in
162
joint
17
other
single-aircraft
between
2020
2022
across
all
seasons.
Data
cover
574
592
cumulative
hours
respectively.
conducted
profiling
at
different
level
legs
below,
in,
just
above
boundary
layer
clouds
(<
3
km)
obtained
situ
measurements
of
trace
gases,
aerosol
particles,
clouds,
atmospheric
state
parameters.
Under
cloud-free
conditions,
similarly
within
immediately
layer.
Air
(the
high-flying
aircraft)
flew
approximately
∼
9
km
remote
sensing
lidar
polarimeter
while
also
launching
dropsondes
(785
total).
Collectively,
simultaneous
data
both
aircraft
help
characterize
same
vertical
column
atmosphere.
In
addition
individual
instrument
files,
are
combined
“merge
files”
on
publicly
available
archive
that
created
time
resolutions
interest
(e.g.,
1,
5,
10,
15,
30,
60
s,
or
matching
an
product's
start
stop
times).
This
paper
describes
flight
strategy,
complementary
products,
access
usage
details,
application
notes.
accessible
through
https://doi.org/10.5067/SUBORBITAL/ACTIVATE/DATA001
(ACTIVATE
Science
Team,
2020).
Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(4), P. 2087 - 2121
Published: Feb. 19, 2025
Abstract.
The
Aerosol
Cloud
meTeorology
Interactions
oVer
the
western
ATlantic
Experiment
(ACTIVATE)
is
a
NASA
mission
to
characterize
aerosol–cloud
interactions
over
North
Atlantic
Ocean
(WNAO).
Such
characterization
requires
understanding
of
life
cycle,
composition,
transport
pathways,
and
distribution
aerosols
WNAO.
This
study
uses
GEOS-Chem
model
simulate
aerosol
distributions
properties
that
are
evaluated
against
aircraft,
ground-based,
satellite
observations
during
winter
summer
field
deployments
in
2020
ACTIVATE.
Transport
boundary
layer
(BL)
behind
cold
fronts
was
major
mechanism
for
American
continental
outflow
pollution
WNAO
winter.
Turbulent
mixing
main
driver
upward
sea
salt
within
ventilation
out
BL
composition
dominated
by
salt,
which
increased
summer,
followed
organics
sulfate.
Aircraft
situ
measurements
provided
useful
constraints
on
wet
scavenging
GEOS-Chem.
generally
captured
observed
features
such
as
outflow,
land–ocean
gradient,
anthropogenic
with
salt.
Model
sensitivity
experiments
elevated
smoke
injection
heights
mid-troposphere
(versus
BL)
better
reproduced
from
US
wildfires
summer.
analysis
suggests
strong
hygroscopic
growth
particles
their
seeding
marine
clouds
(<
35°
N).
Future
modeling
efforts
should
focus
improving
parameterizations
scavenging,
implementing
realistic
heights,
applying
high-resolution
models
resolve
vertical
transport.
Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(3), P. 1639 - 1657
Published: Feb. 5, 2025
Abstract.
The
accurate
representation
of
microphysical
properties
atmospheric
aerosol
particles
–
such
as
the
number,
mass,
and
cloud
condensation
nuclei
(CCN)
concentration
is
key
to
constraining
climate
forcing
estimations
improving
weather
air
quality
forecasts.
Lidars
capable
vertically
resolving
optical
have
been
increasingly
utilized
study
aerosol–cloud
interactions,
allowing
for
cloud-relevant
properties.
Recently,
lidars
employed
identify
monitor
pollen
in
atmosphere,
an
understudied
particle
with
health
possibly
implications.
Lidar
remote
sensing
emerging
research
field,
this
study,
we
present
first
time
retrievals
CCN,
giant
CCN
(GCCN),
ultragiant
(UGCCN)
birch
derived
from
polarization
lidar
observations
specifically
a
PollyXT
Vaisala
CL61
ceilometer
at
532
910
nm,
respectively.
A
pivotal
role
these
played
by
conversion
factors
necessary
convert
measurements
into
This
set
parameters
situ
major
events
Vehmasmäki
station
eastern
Finland.
results
show
that
under
well-mixed
conditions,
surface
instrumentation
can
be
correlated
higher
altitudes
estimate
factors.
Better
linear
agreement
was
found
longer
wavelength
which
attributed
combination
lower
overlap
sensitivity
bigger
compared
nm.
Then,
are
applied
ground-based
against
particles.
In
turn,
demonstrates
potential
network
capacity
document
large-scale
outbursts
detail
thus
provide
valuable
information
climate,
cloud,
modeling
efforts,
elucidating
within
system.
Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(4), P. 2407 - 2422
Published: Feb. 25, 2025
Abstract.
Quantifying
the
degree
of
coupling
between
marine
boundary
layer
(MBL)
clouds
and
surface
is
critical
for
understanding
evolution
low
explaining
vertical
distribution
aerosols
microphysical
cloud
properties.
Previous
work
has
characterized
as
either
coupled
or
decoupled,
but
this
study
rather
considers
four
degrees
coupling,
ranging
from
strongly
to
weakly
coupled.
We
use
aircraft
data
NASA
Aerosol
Cloud
meTeorology
Interactions
oVer
western
ATlantic
Experiment
(ACTIVATE)
assess
aerosol
characteristics
following
regimes,
quantified
using
differences
in
liquid
water
potential
temperature
(θℓ)
total
mixing
ratio
(qt)
flight
near
level
(∼150
m)
directly
below
bases:
strong
(Δθℓ≤1.0
K,
Δqt≤0.8
g
kg−1),
moderate
with
high
Δθℓ
(Δθℓ>1.0
Δqt
Δqt>0.8
weak
kg−1).
Results
show
that
(i)
turbulence
greater
regime
compared
regime,
former
corresponding
more
homogeneity
550
nm
scattering,
integrated
volume
concentration,
giant
number
concentration
(Dp>3
µm)
coincident
increased
MBL
mixing;
(ii)
drop
during
periods
due
upward
velocity
subsequent
activation
particles;
(iii)
sea
salt
tracer
species
(Na+,
Cl−,
Mg2+,
K+)
are
present
concentrations
while
tracers
continental
pollution
(Ca2+,
non-sea-salt
(nss)
SO42-,
NO3-,
oxalate,
NH4+)
higher
mass
fraction
regime.
Additionally,
pH
Cl-:Na+
(a
marker
chloride
depletion)
consistently
lower
There
were
also
two
regimes:
had
turbulent
water,
along
smaller
across
levels
compared.
This
shows
value
defining
multiple
regimes
(rather
than
traditional
versus
decoupled)
demonstrates
behavior
various
regimes.
Abstract.
The
NASA
Aerosol
Cloud
meTeorology
Interactions
oVer
the
western
ATlantic
Experiment
(ACTIVATE)
produced
a
unique
dataset
for
research
into
aerosol-cloud-meteorology
interactions
with
applications
extending
from
process-based
studies
to
multi-scale
model
intercomparison
and
improvement,
remote
sensing
algorithm
assessments
advancements.
ACTIVATE
used
two
Langley
Research
Center
aircraft,
HU-25
Falcon
King
Air,
conduct
systematic
spatially
coordinated
flights
over
northwest
Atlantic
Ocean
amounting
162
joint
17
other
single-aircraft
between
2020
2022
across
all
seasons.
Data
cover
574
592
cumulative
hours
respectively.
flew
conducted
profiling
at
different
level
legs
below,
in,
just
above
boundary
layer
clouds
(<
3
km)
obtained
in
situ
measurements
of
trace
gases,
aerosol
particles,
clouds,
atmospheric
state
parameters.
In
cloud-free
conditions,
similarly
within
immediately
layer.
Air
(the
high-flyer)
approximately
~9
km
conducting
lidar
polarimeter
while
also
launching
dropsondes.
Collectively,
simultaneous
data
collected
both
aircraft
help
characterize
same
vertical
column
atmosphere.
addition
individual
instrument
files,
are
combined
“merge
files”
on
publicly
available
archive
that
created
time
resolutions
interest
(e.g.,
1,
5,
10,
15,
30,
60
s,
or
matching
an
product
start
stop
times).
This
paper
describes
flight
strategy,
complementary
products,
access
usage
details,
application
notes.
Abstract.
Wind
reversals
resulting
in
southerly
flow
along
the
California
coast
are
not
well
understood
terms
of
how
aerosol
and
cloud
characteristics
change.
This
gap
is
addressed
using
airborne
field
measurements
enhanced
with
data
from
space-borne
remote
sensing
(Moderate
Resolution
Imaging
Spectroradiometer),
surface
stations
(Interagency
Monitoring
Protected
Visual
Environments),
models
(Navy
Aerosol
Analysis
Prediction
System
Coupled
Ocean/Atmosphere
Mesoscale
System),
a
focus
on
sub-
supermicron
aerosol,
microphysical
variables:
droplet
number
concentration
(Nd),
optical
thickness
(COT),
effective
radius
(re).
Southerly
coincided
higher
values
submicron
(Na)
mass
concentrations
species
representative
fine
pollution
(NO3-
nss-SO42-)
shipping/continental
emissions
(V,
oxalate,
NH4+,
Ni,
OC,
EC).
Supermicron
Na
did
change,
however,
heightened
levels
acidic
reduced
Cl-:Na+
suggestive
Cl-
depletion
salt
particles.
Clouds
responded
correspondingly
flow,
more
water,
similar
as
phase
(e.g.,
NO3-,
nss-SO42-,
V),
elevated
Nd
COT
re
during
campaigns
liquid
water
paths.
Case
study
flights
help
to
visualize
offshore
gradients
highlight
sensitivity
results
presence
widespread
smoke
coverage
including
associated
plumes
have
Na.
These
implications
for
aerosol-cloud
interactions
wind
reversals,
relevance
weather,
public
welfare,
aviation.
Abstract.
Giant
aerosol,
i.e.,
those
with
diameters
larger
than
1
μm,
can
form
large
droplets
via
condensational
growth
to
sizes
similar
drizzle
particles
without
being
activated.
In
this
study,
we
assess
the
impacts
of
giant
aerosol
on
clouds,
precipitation,
and
radiation
when
activated
are
directly
categorized
as
raindrops
using
U.S.
Department
Energy’s
Energy
Exascale
Earth
System
Model
version
2
(E3SMv2).
We
find
that
categorizing
reduces
cloud
liquid
water
path
by
11.38
%
globally,
most
pronounced
reduction
in
mid-latitudes.
also
approach
improves
model's
ability
simulate
positive
correlation
between
surface
rain
rate
coarse
mode
concentration
regions
low
precipitation.
The
effective
radiative
forcing
associated
aerosol-cloud
interactions
(ERFaci)
from
-1.37
-0.94
-1.23
W
m-2,
depending
size
aerosol.
Our
results
highlight
importance
a
better
representation
system
models
provide
predictions
cloud,
climate.
Abstract.
Wind
reversals
resulting
in
southerly
flow
along
the
California
coast
are
not
well
understood
terms
of
how
aerosol
and
cloud
characteristics
change.
This
gap
is
addressed
using
airborne
field
measurements
enhanced
with
data
from
space-borne
remote
sensing
(Moderate
Resolution
Imaging
Spectroradiometer),
surface
stations
(Interagency
Monitoring
Protected
Visual
Environments),
models
(Navy
Aerosol
Analysis
Prediction
System
Coupled
Ocean/Atmosphere
Mesoscale
System),
a
focus
on
sub-
supermicron
aerosol,
microphysical
variables:
droplet
number
concentration
(Nd),
optical
thickness
(COT),
effective
radius
(re).
Southerly
coincided
higher
values
submicron
(Na)
mass
concentrations
species
representative
fine
pollution
(NO3-
nss-SO42-)
shipping/continental
emissions
(V,
oxalate,
NH4+,
Ni,
OC,
EC).
Supermicron
Na
did
change,
however,
heightened
levels
acidic
reduced
Cl-:Na+
suggestive
Cl-
depletion
salt
particles.
Clouds
responded
correspondingly
flow,
more
water,
similar
as
phase
(e.g.,
NO3-,
nss-SO42-,
V),
elevated
Nd
COT
re
during
campaigns
liquid
water
paths.
Case
study
flights
help
to
visualize
offshore
gradients
highlight
sensitivity
results
presence
widespread
smoke
coverage
including
associated
plumes
have
Na.
These
implications
for
aerosol-cloud
interactions
wind
reversals,
relevance
weather,
public
welfare,
aviation.