Abstract.
Stratospheric
aerosols
play
important
roles
in
Earth’s
radiative
budget
and
heterogeneous
chemistry.
Volcanic
eruptions
modulate
the
stratospheric
aerosol
layer
by
injecting
particles
particle
precursors
like
sulfur
dioxide
(SO2)
into
stratosphere.
Beginning
on
April
9th,
2021,
La
Soufrière
erupted
SO2
tropical
upper
troposphere
lower
stratosphere,
yielding
a
peak
loading
of
0.3–0.4
Tg.
The
resulting
volcanic
plumes
dispersed
predominately
over
northern
hemisphere
(NH),
as
indicated
CALIOP/CALIPSO
satellite
observations
model
simulations.
From
June
to
August
2021
May
July
2022,
NASA
ER-2
high-altitude
aircraft
extensively
sampled
continental
United
States
during
Dynamics
Chemistry
Summer
Stratosphere
(DCOTSS)
mission.
These
in
situ
measurements
provide
detailed
insights
number
concentration,
size
distribution,
spatiotemporal
variations
within
plumes.
Notably,
surface
area
density
were
enhanced
factor
2–4
between
380–500
K
potential
temperature
compared
2022
DCOTSS
observations,
which
minimally
influenced
activity.
Within
plume,
observed
exhibited
significant
meridional
zonal
while
mode
shape
distributions
did
not
vary.
eruption
led
an
increase
concentration
small
(<400
nm),
smaller
effective
diameter
summer
baseline
conditions
regular
profiles
Salina,
Kansas.
A
similar
reduction
was
Palmdale,
California,
possibly
due
already
values
that
region
limited
sampling
period
2022.
modeled
with
SOCOL-AERv2
aerosol-chemistry-climate
model.
enhancement
aligned
well
although
direct
comparison
complicated
issues
related
model’s
background
burden.
This
study
indicates
contributed
at
most
0.6
%
Arctic
Antarctic
ozone
column
depletion
both
is
range
natural
variability.
top-of-atmosphere
one-year
global
average
forcing
-0.08
W/m2
clear-sky
-0.04
all-sky.
effects
concentrated
tropics
NH
midlatitudes
diminished
near-baseline
levels
after
one
year.
Atmospheric chemistry and physics,
Journal Year:
2024,
Volume and Issue:
24(9), P. 5513 - 5548
Published: May 14, 2024
Abstract.
A
growing
number
of
general
circulation
models
are
adapting
interactive
sulfur
and
aerosol
schemes
to
improve
the
representation
relevant
physical
chemical
processes
associated
feedbacks.
They
motivated
by
investigations
climate
response
major
volcanic
eruptions
potential
solar
geoengineering
scenarios.
However,
uncertainties
in
these
not
well
constrained.
Stratospheric
sulfate
is
modulated
emissions
sulfur-containing
species
anthropogenic
natural
origin,
including
activity.
While
effects
have
been
studied
framework
global
model
intercomparisons,
background
conditions
cycle
addressed
such
a
way.
Here,
we
fill
this
gap
analyzing
distribution
main
nine
atmospheric
for
volcanically
quiescent
period.
We
use
observational
data
evaluate
results.
Overall,
agree
that
three
dominant
terms
burdens
(sulfate
aerosol,
OCS,
SO2)
make
up
about
98
%
stratospheric
95
tropospheric
sulfur.
vary
considerably
partitioning
between
species.
Models
emission
SO2
strongly
affects
burden
northern
hemispheric
troposphere,
while
its
importance
very
uncertain
other
regions,
where
much
lower.
Sulfate
deposited
all
models,
but
values
deviate
factor
2.
Additionally,
wet
dry
deposition
fluxes
highly
dependent.
Inter-model
variability
low
tropics
increases
towards
poles.
Differences
largest
dynamically
active
extratropical
region
could
be
attributed
circulation.
The
differences
budget
among
arise
from
both
dynamical
processes,
whose
interplay
complicates
bias
attribution.
Several
problematic
points
identified
individual
related
specifics
chemistry
schemes,
resolution,
cross-tropopause
transport
extratropics.
Further
intercomparison
research
needed
with
focus
on
clarification
reasons
biases,
given
topic
injection
studies.
Atmospheric measurement techniques,
Journal Year:
2024,
Volume and Issue:
17(7), P. 2025 - 2054
Published: April 9, 2024
Abstract.
A
new
algorithm
was
developed
to
infer
particle
size
distribution
parameters
from
the
Stratospheric
Aerosol
and
Gas
Experiment
II
(SAGE
II)
SAGE
III
on
International
Space
Station
III/ISS)
extinction
spectra
using
a
lookup
table
(LUT)
approach.
Here,
SAGE-based
ratios
were
matched
LUT
values,
and,
these
matches,
weighted
statistics
calculated
median
values
higher-moment
as
well
quantify
uncertainty
in
estimates.
This
carried
out
by
solving
for
both
single-mode
bimodal
lognormal
distributions.
The
work
presented
herein
falls
under
two
general
headings:
(1)
theoretical
study
determine
accuracy
of
this
methodology,
(2)
solution
applied
III/ISS
records
with
brief
case
analysis
2022
Hunga
Tonga
eruption.
methodology
demonstrated
be
≈
25
%
accurate
mode
radius
has
minor
dependence
composition.
While
solutions
obtained
algorithm,
we
provide
conclusive
demonstration
how
why
estimates
are
inherently
unstable
alone.
Finally,
aerosol
plume
evolved
regard
transport
over
18
months
after
(PSD)
estimates,
parameters,
uncertainties
products
within
Level
2
(L2)
products,
currently
available
download,
will
merged
into
main
release
subsequent
L2
release.
The
2022
Hunga
volcanic
eruption
injected
a
significant
quantity
of
water
vapor
into
the
stratosphere
while
releasing
only
limited
sulfur
dioxide.
It
has
been
proposed
that
this
excess
could
have
contributed
to
global
warming,
potentially
pushing
temperatures
beyond
1.5
°C
threshold
Paris
Climate
Accord.
However,
given
cooling
effects
sulfate
aerosols
and
contrasting
impacts
ozone
loss
(cooling)
versus
gain
(warming),
assessing
eruption's
net
radiative
effect
is
essential.
Here,
we
quantify
Hunga-induced
perturbations
in
stratospheric
vapor,
aerosols,
using
satellite
observations
transfer
simulations.
Our
analysis
shows
these
components
induce
clear-sky
instantaneous
energy
losses
at
both
top
atmosphere
near
tropopause.
In
2022,
Southern
Hemisphere
experienced
forcing
-0.55
±
0.05
W
m⁻²
-0.52
By
2023,
values
decreased
-0.26
0.04
-0.25
m⁻²,
respectively.
Employing
two-layer
balance
model,
estimate
resulted
about
-0.10
0.02
K
by
end
2023.
Thus,
conclude
cooled
rather
than
warmed
during
period.
Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
51(11)
Published: June 11, 2024
Abstract
Approximately
150
Tg
of
water
vapor
and
0.42
sulfur
dioxide
were
injected
directly
into
the
stratosphere
by
January
2022
Hunga
volcanic
eruption,
which
represents
largest
injection
in
satellite
era.
A
comparison
numerical
simulations
to
balloon‐borne
observations
water‐rich
plume
suggests
that
particle
coagulation
contributed
aerosol's
effective
dry
radius
increase
from
0.2
μm
February
around
0.4
March.
Our
model
stratospheric
aerosol
is
persistently
perturbed
for
years
moderate
large‐magnitude
events,
whereas
extreme
wildfire
events
show
limited
impact
on
background
size.
analysis
further
both
optical
efficiency
aerosols'
lifetime
explain
Hunga's
unusually
large
depth
per
unit
SO
2
injection,
as
compared
with
Pinatubo
eruption.
Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(6), P. 3717 - 3736
Published: March 27, 2025
Abstract.
Stratospheric
aerosol
size
distribution
parameters
are
derived
from
the
multiple-wavelength
extinction
retrievals
of
SAGE
III/M3M
instrument
(Stratospheric
Aerosol
and
Gas
Experiment
III
on
Russian
satellite
Meteor-3M)
analyzed
for
their
evolution
between
2002
2005.
The
broad
wavelength
spectrum
measurements
enables
us
to
derive
all
three
within
an
assumed
monomodal
lognormal
distribution.
2002–2005
stratospheric
layer
was
mostly
at
close
background
conditions
but
included
moderate-magnitude
tropical
volcanic
eruptions
(Ruang,
Reventador,
Manam).
measured
only
middle
high
latitudes,
particle
(PSD)
indicate
a
reduction
in
increase
number
concentration
after
eruptions.
In
addition
this
likely
effect
PSD,
influence
seasonal
polar
winter
condensation
events
including
meteoric
smoke
particles
is
possible,
especially
due
long-lasting
low
temperatures
during
northern
winters
2002/2003
2004/2005.
During
same
winters,
clouds
(PSCs)
were
observed
by
instrument.
A
comparison
dataset
with
balloon-borne
situ
Kiruna,
Sweden,
shows
generally
good
agreement,
there
systematic
differences
below
roughly
15
km
altitude.
Finally,
necessary
assumption
PSD
shape
derivation
remote
sensing
instruments
shown
discussed.
Atmospheric chemistry and physics,
Journal Year:
2024,
Volume and Issue:
24(10), P. 5765 - 5782
Published: May 21, 2024
Abstract.
The
21
June
2019
Raikoke
eruption
(48°
N,
153°
E)
generated
one
of
the
largest
amounts
sulfur
emission
to
stratosphere
since
1991
Mt.
Pinatubo
eruption.
Satellite
measurements
indicate
a
consensus
best
estimate
1.5
Tg
for
dioxide
(SO2)
injected
at
an
altitude
around
14–15
km.
The
peak
Northern
Hemisphere
(NH)
mean
525
nm
stratospheric
aerosol
optical
depth
(SAOD)
increased
0.025,
factor
3
higher
than
background
levels.
Volcano
Response
(VolRes)
initiative
provided
platform
community
share
information
about
this
which
significantly
enhanced
coordination
efforts
in
days
after
A
multi-platform
satellite
observation
subgroup
formed
prepare
initial
report
present
parameters
including
SO2
emissions
and
their
vertical
distribution
modeling
community.
It
allowed
us
make
first
what
would
be
SAOD
1
week
using
simple
volcanic
model.
In
retrospective
analysis,
we
show
that
revised
injection
profiles
yield
mass.
This
highlights
difficulties
accurately
representing
moderate
explosive
eruptions
lowermost
due
limited
sensitivity
current
sensors
(±2
km
accuracy)
low
horizontal
resolution
lidar
observations.
We
also
lifetime
initially
assumed
model
was
overestimated
by
66
%,
pointing
challenges
models
capture
how
life
cycle
gases
aerosols
depends
on
magnitude,
latitude,
height.
Using
profile,
results
NH
monthly
0.024,
excellent
agreement
with
observations,
associated
global
radiative
forcing
−0.17
W
m−2
resulting
annual
surface
temperature
anomaly
−0.028
K.
Given
relatively
small
magnitude
forcing,
it
is
unlikely
response
can
dissociated
from
variability.
Atmospheric measurement techniques,
Journal Year:
2024,
Volume and Issue:
17(12), P. 3669 - 3678
Published: June 18, 2024
Abstract.
This
work
uses
multispectral
measurements
of
vertically
resolved
aerosol
extinction
coefficients
from
the
Stratospheric
Aerosol
and
Gas
Experiment
(SAGE)
III
on
International
Space
Station
(ISS)
to
demonstrate
how
use
Ångström
exponent
for
interpolation
data
between
two
different
wavelengths
creates
a
bias.
An
empirical
relationship
is
derived
magnitude
this
bias
at
several
SAGE
wavelengths.
can
thus
be
used
as
correction
factor
other
studies,
such
multi-instrument
intercomparisons
or
merging,
that
wish
convert
one
wavelength
another
using
applicable
all
stratospheric
non-cloud
except
highly
aged
particles
are
evaporating
altitudes
above
Junge
layer.
Abstract.
The
Hunga
volcano
violently
erupted
on
January
15th,
2022,
and
produced
the
largest
stratospheric
aerosol
layer
perturbation
of
last
30
years.
One
notable
effect
eruption
was
significant
modification
size
distribution
(SD)
with
respect
to
background
conditions
other
recent
moderate
eruptions,
larger
mean
particles
smaller
SD
spread
for
Hunga.
Starting
from
satellite-based
retrievals,
assumption
pure
sulphate
layers,
in
this
work
we
calculate
optical
properties
both
Hunga-perturbed
scenarios
using
a
Mie
code.
We
found
that
intensive
(i.e.,
single
scattering
albedo,
asymmetry
parameter,
extinction
per
unit
mass
broad-band
average
Ångström
exponent)
were
not
significantly
perturbed
by
eruption,
conditions.
calculated
exponent
consistent
multi-instrument
satellite
observations
same
parameter.
Thus,
basic
impact
an
increase
(or
depth),
without
any
shortwave
longwave
relative
absorption,
angular
spectral
trend
extinction,
background.
This
highlights
marked
difference
those
like
Pinatubo
1991
El
Chichon
1982.
With
simplified
radiative
forcing
estimations,
show
likely
3–10
times
more
effective
producing
net
cooling
climate
system
due
scattering.
As
are
seldom
directly
measured,
e.g.
satellite,
our
calculations
can
support
estimation
effects
or
offline
models.