Earth system science data,
Journal Year:
2024,
Volume and Issue:
16(8), P. 3821 - 3849
Published: Aug. 28, 2024
Abstract.
This
article
is
devoted
to
the
presentation
of
MAP-IO
observation
program.
program,
launched
in
early
2021,
has
enabled
nearly
700
d
measurements
over
Indian
and
Southern
Ocean
with
equipment
17
meteorological
oceanographic
scientific
instruments
on
board
ship
Marion
Dufresne.
Several
observational
techniques
have
been
developed
respond
difficulties
observations
ship,
particular
for
passive
remote
sensing
data,
as
well
quasi-autonomous
data
acquisition
transfer.
The
first
made
it
possible
draw
up
unprecedented
climatological
regarding
size
distribution
optical
thickness
aerosols,
concentration
trace
gases
greenhouse
gases,
UV,
integrated
water
vapor.
High-resolution
phytoplankton
surface
waters
also
shown
a
great
variability
latitude
terms
abundance
community
structure
(diversity).
operational
success
this
program
these
unique
results
together
establish
proof
concept
underline
need
transform
into
permanent
observatory.
multi-year
rotations
will
enable
us
assess
trends
seasonal
phytoplankton,
ozone,
marine
aerosols
sensitive
poorly
documented
climatic
region.
Without
being
exhaustive,
should
make
better
understand
biological
carbon
pump,
study
region
that
relation
main
anthropogenic
sources,
monitor
transport
stratospheric
ozone
by
Brewer–Dobson
circulation.
set
publicly
available
at
https://www.aeris-data.fr/catalogue-map-io/
(last
access:
26
August
2024)
(atmospheric
data)
https://doi.org/10.17882/89505
(Thyssen
et
al.,
2022a)
(phytoplankton
data).
Earth system science data,
Journal Year:
2023,
Volume and Issue:
15(8), P. 3747 - 3760
Published: Aug. 22, 2023
Abstract.
We
present
a
global
multiyear
height-resolved
data
set
of
aerosol-type-specific
cloud
condensation
nuclei
concentrations
(nCCN)
estimated
from
the
spaceborne
lidar
aboard
Cloud-Aerosol
Lidar
and
Infrared
Pathfinder
Satellite
Observation
(CALIPSO)
satellite.
For
estimating
nCCN,
we
apply
recently
introduced
Optical
Modelling
CALIPSO
Aerosol
Microphysics
(OMCAM)
algorithm
to
Level
2
Profile
product.
The
nCCN
are
then
gridded
into
uniform
latitude–longitude
grid
2∘×5∘,
vertical
resolution
60
m
surface
an
altitude
8
km,
temporal
1
month.
span
total
186
months,
June
2006
December
2021.
In
addition,
provide
3D
climatology
produced
using
complete
time
series.
further
highlight
some
potential
applications
in
context
aerosol–cloud
interactions.
can
be
accessed
at
https://doi.org/10.1594/PANGAEA.956215
(Choudhury
Tesche,
2023).
Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(4), P. 2631 - 2648
Published: Feb. 28, 2025
Abstract.
Cloud
condensation
nuclei
(CCN)
play
a
fundamental
role
in
determining
the
microphysical
properties
of
low-level
clouds
that
are
crucial
for
defining
energy
budget
over
Southern
Ocean
(SO).
However,
many
aspects
CCN
SO
remains
poorly
understood,
including
synoptic
meteorology.
In
this
study,
we
classify
six
distinct
regimes
Kennaook
/
Cape
Grim
Observatory
(CGO)
and
examine
their
influence
on
seasonal
cycle
concentration
(NCCN).
Three
“winter”
dominant
when
subtropical
ridge
(STR)
is
strong
centered
at
lower
latitudes,
while
three
“summer”
prevail
STR
shifts
to
higher
latitudes.
Distinct
winter
summer
“baseline”
patterns
contribute
NCCN,
with
baseline
regime
characterized
by
heavier
precipitation
(0.10
vs.
0.03
mm
h−1),
deeper
boundary
layer
(850
900
hPa),
NCCN
(71
137
cm−3)
than
one.
Across
these
two
regimes,
observe
significant
inverse
relationship
between
underscoring
contribution
reducing
SO.
An
analysis
air
mass
back-trajectories,
specifically
free-troposphere
level,
supports
distinction,
wintertime
masses
originating
more
frequently
from
The
summertime
seen
as
barrier
Antarctic
reaching
latitude
CGO.
Conversely,
found
pass
continental
Australia
before
CGO,
consistent
enhanced
radon
concentrations.
Earth and Space Science,
Journal Year:
2025,
Volume and Issue:
12(5)
Published: April 30, 2025
Abstract
Visible/infrared
imagery
from
passive
satellites
is
commonly
relied
upon
to
study
low
cloud
microphysics
over
oceanic
regions,
including
for
the
Southern
Ocean
(SO),
but
relatively
little
validation
has
been
undertaken
SO.
In
this
article,
we
compare
low‐cloud
effective
radius
(
r
e
),
droplet
number
concentration
N
d
)
and
liquid
water
path
(LWP)
retrievals
NASA
Moderate
Imaging
Spectroradiometer
(MODIS)
with
surface
measurements
collected
during
Macquarie
Island
Cloud
Radiation
Experiment
(MICRE).
MODIS
3.7‐μm
band
show
bias
moderately
good
correlation
relative
MICRE
liquid‐phase
clouds
when
restricted
Solar
Zenith
Angles
<65°
on
spatial
scales
of
50–100
km.
However,
overall
in
3.7
partly
results
cancellation
errors:
overestimated
non‐to‐lightly
precipitating
clouds,
underestimated
heavier
drizzling
by
∼1–1.5
μm.
1.6‐μm
2.1‐μm
are
biased
high.
may
likewise
be
slightly
under‐
or
depending
concentration,
there
insufficient
data
provide
confidence
result.
Interestingly,
a
composite
2002
2020
distinct
region
enhanced
cover
(and
lower
wake
associated
orographic
formation.
aerosol
optical
depth
(AOD)
Angstrom
Exponent
(AE)
upwind
downwind
island
do
not
differ
significantly.
Comparison
suggests
that
Collection
6
AOD
reasonable,
while
AE
problematically
large.
Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(22), P. 14603 - 14630
Published: Nov. 17, 2022
Abstract.
The
Southern
Ocean
radiative
bias
continues
to
impact
climate
and
weather
models,
including
the
Australian
Community
Climate
Earth
System
Simulator
(ACCESS).
bias,
characterised
by
too
much
shortwave
radiation
reaching
surface,
is
attributed
incorrect
simulation
of
cloud
properties,
frequency
phase.
To
identify
regimes
important
Ocean,
we
use
k-means
histogram
clustering,
applied
a
satellite
product
then
fitted
nudged
simulations
latest-generation
ACCESS
atmosphere
model.
We
instances
when
model
correctly
or
incorrectly
simulates
same
type
as
for
any
point
in
time
space.
evaluate
biases
these
instances.
find
that
type,
property
equivalent,
some
cases
greater,
magnitude
remain
compared
types
are
simulated.
Furthermore,
even
appear
small
on
average,
biases,
such
liquid
ice
water
paths
fractions,
large.
Our
results
suggest
simply
getting
right
(or
macrophysics)
not
enough
reduce
bias.
where
small,
it
may
be
so
wrong
reasons.
Considerable
effort
still
required
improve
microphysics,
with
particular
focus
Atmospheric chemistry and physics,
Journal Year:
2024,
Volume and Issue:
24(10), P. 6305 - 6322
Published: May 29, 2024
Abstract.
Antarctica
and
the
Southern
Ocean
(SO)
are
most
pristine
areas
of
globe
represent
ideal
places
to
investigate
aerosol–climate
interactions
in
an
unperturbed
atmosphere.
In
this
study,
we
present
submicrometer
aerosol
(PM1)
source
apportionment
for
two
sample
sets
collected
parallel
at
British
Antarctic
Survey
stations
Signy
Halley
during
austral
summer
2018–2019.
Water-soluble
organic
matter
(WSOM)
is
a
major
component
both
sites
(37
%
29
water-soluble
PM1,
on
average,
Halley,
respectively).
Remarkable
differences
between
pelagic
(open-ocean)
sympagic
(influenced
by
sea
ice)
air
mass
histories
related
sources
found.
The
application
factor
analysis
techniques
series
spectra
obtained
means
proton-nuclear
magnetic
resonance
(H-NMR)
spectroscopy
samples
allows
identification
five
(OA)
sources:
primary
(POA)
types,
characterized
sugars,
polyols,
degradation
products
lipids
associated
with
open-ocean
sympagic/coastal
waters,
respectively;
secondary
(SOA)
one
enriched
methanesulfonic
acid
(MSA)
dimethylamine
(DMA)
waters
other
trimethylamine
(TMA)
linked
environments;
fifth
unclear
origin,
possibly
atmospheric
aging
emissions.
Overall,
our
results
strongly
indicate
that
emissions
from
ecosystems
affect
variability
composition
study
area,
circulation
establishing
marked
latitudinal
gradients
only
some
components
(e.g.,
components)
while
distributing
others
and/or
aged
maritime
inner
regions.
Journal of Geophysical Research Atmospheres,
Journal Year:
2022,
Volume and Issue:
127(18)
Published: Sept. 9, 2022
Abstract
The
Southern
Ocean
is
often
identified
as
a
pristine
aerosol
environment,
being
distant
from
anthropogenic
sources.
We
investigate
anomalies
in
loading
over
the
due
to
stratospheric
ozone
depletion
historical
simulations
performed
for
sixth
Coupled
Model
Intercomparison
Project.
explore
direct
influences
of
on
aerosols
via
enhanced
ultraviolet‐induced
production
oceanic
dimethyl
sulfide
(DMS),
and
indirect
changes
Hemisphere
westerly
jet,
which
impacts
wind‐driven
fluxes.
identify
wind
key
driver
change
austral
summertime
aerosol,
leading
increases
optical
depth
up
24%
compared
with
pre–ozone
hole
era.
In
contrast
previous
studies,
ultraviolet
fluxes
are
less
obvious.
Our
results
show
that
environment
cannot
be
considered
representative
conditions
because
has
indirectly
increased
marine
Environmental Science Atmospheres,
Journal Year:
2023,
Volume and Issue:
3(10), P. 1513 - 1532
Published: Jan. 1, 2023
Ice
nucleating
particles
(INPs)
in
sea
spray
aerosol
(SSA)
are
important
for
ice
formation
clouds
over
oceans.
We
found
that
SSA
INP
concentrations
during
a
phytoplankton
bloom
were
degraded
with
exposure
to
3
8
days
of
atmospheric
oxidation.
Geoscientific model development,
Journal Year:
2022,
Volume and Issue:
15(10), P. 4055 - 4076
Published: May 25, 2022
Abstract.
An
Earth
system
model
(ESM)
aerosol–cloud
diagnostics
package
is
developed
to
facilitate
the
routine
evaluation
of
aerosols,
clouds,
and
interactions
simulated
by
Energy
Exascale
System
Model
(E3SM)
from
US
Department
(DOE).
The
first
version
focuses
on
comparing
aerosol
properties
with
aircraft,
ship,
surface
measurements,
which
are
mostly
measured
in
situ.
currently
cover
six
field
campaigns
four
geographical
regions:
eastern
North
Atlantic
(ENA),
central
(CUS),
northeastern
Pacific
(NEP),
Southern
Ocean
(SO).
These
regions
produce
frequent
liquid-
or
mixed-phase
extensive
measurements
available
Atmospheric
Radiation
Measurement
(ARM)
program
other
agencies.
Various
types
metrics
performed
for
number,
size
distribution,
chemical
composition,
cloud
condensation
nuclei
(CCN)
concentration,
various
meteorological
quantities
assess
how
well
E3SM
represents
observed
across
spatial
scales.
Overall,
qualitatively
reproduces
number
composition
reasonably
well,
but
it
overestimates
Aitken-mode
aerosols
underestimates
accumulation-mode
over
CUS
ENA
regions,
suggesting
that
processes
related
particle
growth
coagulation
might
be
too
weak
model.
current
struggles
reproduce
new
formation
events
frequently
both
indicating
missing
parameterizations.
coded
organized
a
way
can
extended
campaign
datasets
adapted
higher-resolution
simulations.
Journal of Geophysical Research Atmospheres,
Journal Year:
2023,
Volume and Issue:
128(2)
Published: Jan. 7, 2023
Abstract
Anthropogenic
activities
have
drastically
impacted
the
climate
system
since
Industrial
Revolution.
However,
to
what
extent
anthropogenic
emissions
influence
cloud
droplet
number
concentration
(
N
d
),
critical
parameter
for
understanding
aerosol‐cloud
interactions,
is
poorly
known
on
hemispheric
scale
due
considerable
retrieval
uncertainty.
We
employed
multiple
widely
used
sampling
methods
evaluate
long‐term
trend
in
contrast
(Δ
d(NH‐SH)
)
between
Northern
Hemisphere
(NH)
and
Southern
(SH).
Here
we
show
that
Δ
was
halved
from
2003
2020
using
different
channels,
even
though
range
of
magnitudes
large.
Such
dramatic
changes
are
dominated
by
significantly
decreased
over
NH
(∼20%)
emission
reductions
compared
relatively
stable
pristine
nature
SH.
Aerosol
optical
depth
(AOD)
aerosol
index
(AI)
correlate
with
based
trends,
they
replicate
trends.
This
poor
correlation
partly
contributed
stratospheric
smoke
wildfires
Australia
had
little
The
northwest
Atlantic
shows
largest
contribution,
∼38%,
trend,
whereas
Pacific
dominates
change
AOD
AI,
contributing
more
than
60%
∼50%
AI
NH.
Our
results
imply
reduced
provide
strong
observational
evidence
extensively
altered
liquid
clouds
last
two
decades.