Abstract.
Cloud
processing
is
known
to
generate
aerosol
species
such
as
sulfate
and
secondary
organic
aerosol,
yet
there
a
scarcity
of
airborne
data
examine
this
issue.
The
NASA
Aerosol
meTeorology
Interactions
oVer
the
western
ATlantic
Experiment
(ACTIVATE)
was
designed
build
an
unprecedented
dataset
relevant
aerosolâcloud
interactions
with
two
coordinated
aircraft
over
northwestern
Atlantic,
mass
spectrometer
used
from
four
deployments
between
2020â2021
contrast
composition
below,
in
(using
counterflow
virtual
impactor)
above
boundary
layer
clouds.
Consistent
features
all
time
periods
(JanuaryâMarch,
MayâJune,
AugustâSeptember)
include
fraction
organics
relative
amount
oxygenated
organicsÂ
(â44)
total
class="inline-formula">f44)
increasing
droplet
residuals
below
cloud.
Detailed
analysis
comparing
cloud
suggests
possible
role
for
in-cloud
aqueous
explaining
results;
intriguing
aspect
though
requiring
more
attention
that
only
approximately
quarter
casesÂ
(29
110)
showed
higher
fractions
either
or
Of
those
29Â
cases,
majority
(25)
base
where
signature
presumably
evident
compared
These
results
are
consistent
few
past
studies
analyzing
pointing
enrichment
than
adjacent
cloud-free
areas.
findings
important
other
datasets
(e.g.,
reanalysis)
suggest
both
abundant
(in
work)
closely
related
drop
number
concentrations
winter
when
strongest.
Here
we
show
interaction
clouds
potentially
decreases
particle
hygroscopicity
due
increase
organic:sulfate
ratio
surrounding
air.
light
growing
importance
Atlantic
recent
decades
owing
success
regulatory
activity
eastern
United
States
cut
sulfur
dioxide
emissions.
Frontiers in Remote Sensing,
Journal Year:
2023,
Volume and Issue:
4
Published: April 3, 2023
Airborne
NASA
Langley
Research
Center
(LaRC)
High
Spectral
Resolution
Lidar-2
(HSRL-2)
measurements
acquired
during
the
recent
Earth
Venture
Suborbital-3
(EVS-3)
Aerosol
Cloud
Meteorology
Interactions
over
Western
Atlantic
Experiment
(ACTIVATE)
revealed
elevated
particulate
linear
depolarization
associated
with
aerosols
within
marine
boundary
layer.
These
observations
were
off
east
coast
of
United
States
both
winter
and
summer
2020
2021
when
HSRL-2
was
deployed
on
LaRC
King
Air
aircraft.
During
20
63
total
flight
days,
particularly
days
cold
air
outbreaks,
at
532
nm
exceeded
0.15–0.20
lowest
several
hundred
meters
atmosphere,
indicating
that
these
particles
non-spherical.
Higher
values
typically
measured
355
lower
1,064
nm.
Several
lines
evidence
suggest
non-spherical
sea
salt
including
aerosol
extinction/backscatter
ratio
(“lidar
ratio”)
20–25
sr
by
HSRL-2,
higher
low
(<
60%)
relative
humidity,
coincident
airborne
in
situ
size
composition
measurements,
transport
simulations.
The
not
correlated
wind
speed
but
mass
fraction
effective
radius
humidity
below
60%.
median
extinction
about
Mm
−1
found
optical
depth
(AOD)
contributed
remained
small
(0.03–0.04)
represented
average
30%–40%
column
AOD.
Cloud-Aerosol
Lidar
Orthogonal
Polarization
(CALIOP)
spaceborne
lidar
outbreaks
CALIOP
retrievals
using
AOD
constraints
operational
algorithms
can
misclassify
as
dusty
rather
than
aerosols.
Such
misclassification
leads
to
∼40–50%
overestimates
assumed
subsequent
extinction.
Scientific Data,
Journal Year:
2023,
Volume and Issue:
10(1)
Published: Nov. 1, 2023
The
Aerosol
Cloud
meTeorology
Interactions
oVer
the
western
ATlantic
Experiment
(ACTIVATE)
field
campaign
provides
accurate
data
for
aerosol
characterization
and
trace
gas
profiles,
establishes
knowledge
of
relationships
between
aerosols
water.
dropsonde
dataset
an
in
situ
vertical
thermodynamic
structure
atmosphere
during
165
research
flights
by
NASA
Langley's
King
Air
aircraft
February
2020
June
2022
four
test
December
2019
November
2021.
covered
North
Atlantic
region,
off
coast
Eastern
United
States
around
Bermuda
all
seasons.
profiles
provide
observations
temperature,
pressure,
relative
humidity,
horizontal
winds
surface
about
9
km.
801
dropsondes
were
released,
which
796
processed
788
complete
parameters
flight
level
with
normal
parachute
performance.
Here,
we
describe
dataset,
processing
measurements,
general
statistics,
applications
this
rich
dataset.
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).
Environmental Science Atmospheres,
Journal Year:
2022,
Volume and Issue:
2(4), P. 738 - 752
Published: Jan. 1, 2022
Airborne
field
data
are
used
to
examine
relationships
between
giant
cloud
condensation
nuclei
(GCCN)
and
composition
advance
knowledge
of
poorly
characterized
GCCN–cloud
interactions.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(17), P. 9853 - 9871
Published: Sept. 6, 2023
Abstract.
Nucleation
in
the
free
troposphere
(FT)
and
subsequent
growth
of
new
particles
represent
a
globally
important
source
cloud
condensation
nuclei
(CCN).
Whereas
particle
formation
(NPF)
has
been
shown
to
occur
frequently
upper
over
tropical
oceans,
there
have
few
studies
NPF
at
lower
altitudes.
In
addition,
impact
urban
emissions
biomass
burning
on
marine
FT
remains
poorly
understood.
this
study,
we
examine
mid-troposphere
(3–8.5
km)
ocean
coastal
region
using
airborne
measurements
during
recent
Cloud,
Aerosol
Monsoon
Processes
Philippines
Experiment
(CAMP2Ex).
was
mostly
observed
above
5.5
km
coincided
with
elevated
relative
humidity
(RH)
reduced
sink
(CS),
suggesting
that
occurs
convective
outflow.
The
frequency
increases
altitude,
reaching
∼
50
%
8
km.
An
abrupt
decrease
coincides
early
monsoon
transition
is
attributed
increased
CS
resulting
from
activity
more
frequent
transport
aged
plumes.
Surprisingly,
large
fraction
events
background
air
were
morning,
likely
made
possible
by
very
low
despite
actinic
flux.
Convectively
detrained
biomass-burning
plumes
fresh
enhance
as
result
precursor
concentrations
scavenging
pre-existing
particles.
contrast,
suppressed
where
reactive
precursors
are
consumed,
while
relatively
high.
This
study
shows
strong
FT.
results
also
illustrate
competing
influences
different
variables
interactions
among
anthropogenic
emissions,
clouds,
meteorology,
which
lead
under
variety
conditions
environments.
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.
Geophysical Research Letters,
Journal Year:
2025,
Volume and Issue:
52(8)
Published: April 19, 2025
Abstract
We
investigated
the
occurrence
and
evolution
of
new
particle
formation
(NPF)
events
over
southeast
Atlantic.
The
studied
region
is
under
influence
long‐range
transport
aerosols
gases
during
southern
African
biomass
burning
season,
from
June
to
October
every
year.
Interestingly,
NPF
was
observed
coincide
with
although
wet
removal
pre‐existing
needed
these
events.
Surface
airborne
measurements
show
that
likely
occurred
in
upper
marine
boundary
layer,
newly
formed
were
further
transported
surface
via
vertical
air
motions.
Using
a
box
model,
we
predicted
large
fraction
particles
could
grow
sizes
related
cloud
condensation
nuclei.
Our
study
shows
can
occur
Atlantic,
biomass‐burning
plume
contributed
occurrence.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(24), P. 15671 - 15691
Published: Dec. 20, 2023
Abstract.
Atmospheric
aerosols
affect
the
global
energy
budget
by
scattering
and
absorbing
sunlight
(direct
effects)
changing
microphysical
structure,
lifetime,
coverage
of
clouds
(indirect
effects).
Both
aerosol
direct
indirect
effects
are
affected
vertical
distribution
in
atmosphere,
which
is
further
influenced
a
range
processes,
such
as
dynamics,
long-range
transport,
entrainment.
However,
many
observations
these
processes
based
on
ground
measurements,
limiting
our
ability
to
understand
simulate
their
impact
climate.
In
this
work,
we
examined
heterogeneity
over
Radiation
Measurement
(ARM)
Southern
Great
Plains
(SGP)
using
data
collected
from
Holistic
Interactions
Shallow
Clouds,
Aerosols
Land
Ecosystems
(HI-SCALE)
campaign.
The
profiles
meteorological
physiochemical
properties
up
2500
m
above
38
flights
conducted
during
HI-SCALE
SGP
show
strong
seasonal
variabilities.
concentrations
at
surface
highest
due
emissions
level.
general,
mode
diameter
summer
(∼
100
nm)
larger
than
that
spring
30
nm),
result
enhanced
condensational
growth
enriched
volatile
organic
compounds
summer.
concentration
below
nm
boundary
layer
(BL)
(e.g.,
1000
m)
higher
summer,
stronger
new
particle
formation
(NPF)
events
reduced
condensation
sink
spring.
BL,
size
gradually
increases
with
altitude
cloud
processing.
chemical
composition
remained
similar,
organics
sulfates
representing
59.8
±
2.2
%
22.7
2.1
%,
respectively,
total
mass
BL.
Through
properties,
observed
NPF
upper
BL
7
out
research
flights,
where
newly
formed
particles
continue
grow
they
mixed
down
surface.
There
also
an
indication
deep
convection
brings
free
troposphere
(FT)
surface,
contribute
nuclei
(CCN).
Overall,
dynamics
(new
formation,
growth,
processing)
transport
(mixing
entrainment,
convective
downward
transport).
Case
studies
showing
influence
factors
discussed.