Abstract.
As
a
long-standing
problem
in
climate
models,
large
positive
shortwave
radiation
biases
exist
at
the
surface
over
Southern
Ocean,
impacting
accurate
simulation
of
sea
temperature,
atmospheric
circulation,
and
precipitation.
Underestimations
low-level
cloud
fraction
liquid
water
content
are
suggested
to
predominantly
contribute
these
biases.
Most
model
evaluations
for
focus
on
summer
rely
satellite
products,
which
have
their
own
limitations.
In
this
work,
we
use
surface-based
observations
Macquarie
Island
provide
first
long-term,
seasonal
evaluation
both
downwelling
longwave
Australian
Community
Climate
Earth
System
Simulator
Atmosphere-only
Model
Version
2
(ACCESS-AM2)
Ocean.
The
capacity
Clouds
Earth’s
Radiant
Energy
(CERES)
product
simulate
is
also
investigated.
We
utilise
novel
lidar
simulator,
Automatic
Lidar
Ceilometer
Framework
(ALCF)
all-sky
camera
investigate
how
influenced
by
properties.
Overall,
find
an
overestimation
+9.5
±
33.5
W
m−2
fluxes
underestimation
-2.3
13.5
ACCESS-AM2
conditions,
with
more
pronounced
+25.0
48.0
occurring
summer.
CERES
presents
+8.0
18.0
-12.1
12.2
conditions.
For
radiative
effect
(CRE)
biases,
there
+4.8
28.0
-7.9
20.9
CERES.
An
associated
fraction.
occurrence
less
clear
suggest
that
modelled
phase
having
impact
Our
results
show
require
further
development
reduce
not
just
but
clear-sky
Earth and Space Science,
Journal Year:
2023,
Volume and Issue:
10(9)
Published: Sept. 1, 2023
Abstract
Insufficient
in
situ
observations
from
the
Antarctic
marginal
ice
zone
(MIZ)
limit
our
understanding
and
description
of
relevant
mechanical
thermodynamic
processes
that
regulate
seasonal
sea
cycle.
Here
we
present
high‐resolution
thermal
images
ocean
surface
complementary
measurements
atmospheric
variables
were
acquired
underway
during
one
austral
winter
spring
expedition
Atlantic
Indian
sectors
Southern
Ocean.
Skin
temperature
data
cover
used
to
estimate
partitioning
heterogeneous
calculate
heat
fluxes
compare
with
ERA5
reanalyses.
The
MIZ
was
composed
different
but
relatively
regularly
distributed
types
sharp
gradients.
surface‐weighted
skin
compared
well
reanalyses
due
a
compensation
errors
between
fraction
floe
temperature.
These
uncertainties
determine
dominant
source
inaccuracy
for
as
computed
observed
variables.
In
spring,
type
distribution
more
irregular,
alternation
large
open
water
fractions
even
400
km
edge.
homogeneous
did
not
produce
substantial
fluxes.
discrepancies
relative
reanalysis
are
however
larger
than
attributed
biases
variables,
downward
solar
radiation
being
most
critical.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(23), P. 14691 - 14714
Published: Nov. 29, 2023
Abstract.
As
a
long-standing
problem
in
climate
models,
large
positive
shortwave
radiation
biases
exist
at
the
surface
over
Southern
Ocean,
impacting
accurate
simulation
of
sea
temperature,
atmospheric
circulation,
and
precipitation.
Underestimations
low-level
cloud
fraction
liquid
water
content
are
suggested
to
predominantly
contribute
these
biases.
Most
model
evaluations
for
focus
on
summer
rely
satellite
products,
which
have
their
own
limitations.
In
this
work,
we
use
surface-based
observations
Macquarie
Island
provide
first
long-term,
seasonal
evaluation
both
downwelling
longwave
Australian
Community
Climate
Earth
System
Simulator
Atmosphere-only
Model
version
2
(ACCESS-AM2)
Ocean.
The
capacity
Clouds
Earth’s
Radiant
Energy
(CERES)
product
simulate
is
also
investigated.
We
utilize
novel
lidar
simulator,
Automatic
Lidar
Ceilometer
Framework
(ALCF),
all-sky
camera
investigate
how
influenced
by
properties.
Overall,
find
an
overestimation
+9.5±33.5
W
m−2
fluxes
underestimation
-2.3±13.5
ACCESS-AM2
conditions,
with
more
pronounced
+25.0±48.0
occurring
summer.
CERES
presents
+8.0±18.0
-12.1±12.2
conditions.
For
radiative
effect
(CRE)
biases,
there
+4.8±28.0
-7.9±20.9
CERES.
An
associated
underestimated
occurrence.
suggest
that
modeled
phase
having
impact
Our
results
show
require
further
development
reduce
not
just
but
clear-sky
Geoscientific model development,
Journal Year:
2024,
Volume and Issue:
17(7), P. 2641 - 2662
Published: April 11, 2024
Abstract.
The
evaluation
and
quantification
of
Southern
Ocean
cloud–radiation
interactions
simulated
by
climate
models
are
essential
in
understanding
the
sources
magnitude
radiative
bias
that
persists
for
this
region.
To
date,
most
methods
focus
on
specific
synoptic
or
cloud-type
conditions
do
not
consider
entirety
Ocean's
cloud
regimes
at
once.
Furthermore,
it
is
difficult
to
directly
quantify
complex
non-linear
role
different
properties
have
modulating
effect.
In
study,
we
present
a
new
method
model
evaluation,
using
machine
learning
can
once
identify
complexities
within
system
individual
contributions.
this,
use
an
XGBoost
(eXtreme
Gradient
Boosting)
predict
nudged
version
Australian
Community
Climate
Earth
System
Simulator
–
Atmosphere-only
model,
property
biases
as
predictive
features.
We
find
explain
up
55
%
from
these
alone.
then
apply
SHAP
(SHapley
Additive
exPlanations)
feature
importance
analysis
each
plays
predicting
bias.
liquid
water
path
largest
contributor
over
Ocean,
though
important
regional
dependencies
exist.
test
usefulness
evaluating
perturbations
clearly
responses,
including
compensating
errors.
Authorea (Authorea),
Journal Year:
2024,
Volume and Issue:
unknown
Published: April 16, 2024
There
are
significant
gaps
in
both
experimental
and
theoretical
understanding
of
mixed-phase
clouds,
their
impacts
on
the
hydrological
cycle
as
well
effects
atmospheric
radiation.
Accurately
identifying
liquid
water
layers
clouds
is
crucial
for
estimating
cloud
radiative
effects.
A
proof-of-concept
study
utilizing
a
machine-learning-based
liquid-layer
detection
method
called
VOODOO
presented.
This
was
applied
alongside
single-column
transfer
model
to
compare
downwelling
shortwave
fluxes
detected
by
standard
Cloudnet
processing
chain
ground-based
pyranometer
observations.
Our
findings
reveal
that
creates
more
realistic
content
distributions
significantly
influences
profiles
heating
rates.
Moreover,
our
demonstrates
substantial
enhancement
estimation
compared
conventional
Cloudnet.
Specifically,
we
observe
remarkable
reduction
mean
absolute
error
simulated
radiation
at
surface
70\%,
particularly
homogeneous
conditions.
The
percentage
SW
between
observations
44\%,
while
VOODOO+Cloudnet
reduces
this
8\%.
Overall,
results
underscore
potential
provide
new
insights
into
deep
which
were
previously
inaccessible
using
traditional
lidar-based
remote
sensing
techniques.
Abstract.
As
a
long-standing
problem
in
climate
models,
large
positive
shortwave
radiation
biases
exist
at
the
surface
over
Southern
Ocean,
impacting
accurate
simulation
of
sea
temperature,
atmospheric
circulation,
and
precipitation.
Underestimations
low-level
cloud
fraction
liquid
water
content
are
suggested
to
predominantly
contribute
these
biases.
Most
model
evaluations
for
focus
on
summer
rely
satellite
products,
which
have
their
own
limitations.
In
this
work,
we
use
surface-based
observations
Macquarie
Island
provide
first
long-term,
seasonal
evaluation
both
downwelling
longwave
Australian
Community
Climate
Earth
System
Simulator
Atmosphere-only
Model
Version
2
(ACCESS-AM2)
Ocean.
The
capacity
Clouds
Earth’s
Radiant
Energy
(CERES)
product
simulate
is
also
investigated.
We
utilise
novel
lidar
simulator,
Automatic
Lidar
Ceilometer
Framework
(ALCF)
all-sky
camera
investigate
how
influenced
by
properties.
Overall,
find
an
overestimation
+9.5
±
33.5
W
m−2
fluxes
underestimation
-2.3
13.5
ACCESS-AM2
conditions,
with
more
pronounced
+25.0
48.0
occurring
summer.
CERES
presents
+8.0
18.0
-12.1
12.2
conditions.
For
radiative
effect
(CRE)
biases,
there
+4.8
28.0
-7.9
20.9
CERES.
An
associated
fraction.
occurrence
less
clear
suggest
that
modelled
phase
having
impact
Our
results
show
require
further
development
reduce
not
just
but
clear-sky