Abstract.
In
situ
cloud
probe
data
from
the
NASA
ObseRvations
of
Aerosols
above
CLouds
and
their
intEractionS
(ORACLES)
field
campaign
were
used
to
estimate
effective
radius
(Re),
optical
thickness
class="inline-formula">Ï),
droplet
concentration
class="inline-formula">Nc)
for
marine
stratocumulus
over
southeast
Atlantic
Ocean.
The
in
Re,
class="inline-formula">Ï,
class="inline-formula">Nc
compared
with
co-located
Moderate
Resolution
Imaging
Spectroradiometer
(MODIS)
retrievals
class="inline-formula">Re
class="inline-formula">Ï
MODIS-derived
class="inline-formula">Nc.
For
145
profiles,
a
MODIS
retrieval
was
time
gap
less
than
1âh.
On
average,
(11.3âµm
11.7)
1.6âR)
0.77
0.73,
respectively.
average
(151.5âcmâ3)
within
1âcmâ3
an
class="inline-formula">R
0.90.
profiles
classified
into
67
contact
where
aerosol
class="inline-formula">Na)
greater
500âcmNa
up
tops.
Contact
had
(by
88âcmâ3),
2.5),
lower
2.2âµm)
profiles.
These
differences
associated
aerosolâcloud
interactions
(ACI),
estimates
5âcmâ3,
0.5,
0.2âRe>15âÏ>25
removed.
agreement
between
changes
ACI
driven
by
small
biases
properties
relative
measurements
across
different
regimes.
Thus,
combined
location
concentration,
can
be
study
larger
domains
longer
timescales
possible
using
data.
Abstract.
In
situ
cloud
probe
data
from
the
NASA
ObseRvations
of
Aerosols
above
CLouds
and
their
intEractionS
(ORACLES)
field
campaign
were
used
to
estimate
effective
radius
(Re),
optical
thickness
class="inline-formula">τ),
droplet
concentration
class="inline-formula">Nc)
for
marine
stratocumulus
over
southeast
Atlantic
Ocean.
The
in
Re,
class="inline-formula">τ,
class="inline-formula">Nc
compared
with
co-located
Moderate
Resolution
Imaging
Spectroradiometer
(MODIS)
retrievals
class="inline-formula">Re
class="inline-formula">τ
MODIS-derived
class="inline-formula">Nc.
For
145
profiles,
a
MODIS
retrieval
was
time
gap
less
than
1
h.
On
average,
(11.3
class="inline-formula">µm
11.7)
1.6
2.3
higher
Pearson's
correlation
coefficients
class="inline-formula">R)
0.77
0.73,
respectively.
average
(151.5
cm−3)
within
class="inline-formula">−3
an
class="inline-formula">R
0.90.
profiles
classified
into
67
contact
where
aerosol
class="inline-formula">Na)
greater
500
sampled
100
m
tops
78
separated
class="inline-formula">Na
up
tops.
Contact
had
(by
88
class="inline-formula">−3),
2.5),
lower
2.2
class="inline-formula">µm)
profiles.
These
differences
associated
aerosol–cloud
interactions
(ACI),
estimates
5
class="inline-formula">−3,
0.5,
0.2
when
class="inline-formula">Re>15
or
class="inline-formula">τ>25
removed.
agreement
between
changes
ACI
driven
by
small
biases
properties
relative
measurements
across
different
regimes.
Thus,
combined
location
concentration,
can
be
study
larger
domains
longer
timescales
possible
using
data.
Abstract.
In
situ
cloud
probe
data
from
the
NASA
ObseRvations
of
Aerosols
above
CLouds
and
their
intEractionS
(ORACLES)
field
campaign
were
used
to
estimate
effective
radius
(Re),
optical
thickness
class="inline-formula">Ï),
droplet
concentration
class="inline-formula">Nc)
for
marine
stratocumulus
over
southeast
Atlantic
Ocean.
The
in
Re,
class="inline-formula">Ï,
class="inline-formula">Nc
compared
with
co-located
Moderate
Resolution
Imaging
Spectroradiometer
(MODIS)
retrievals
class="inline-formula">Re
class="inline-formula">Ï
MODIS-derived
class="inline-formula">Nc.
For
145
profiles,
a
MODIS
retrieval
was
time
gap
less
than
1âh.
On
average,
(11.3âµm
11.7)
1.6âR)
0.77
0.73,
respectively.
average
(151.5âcmâ3)
within
1âcmâ3
an
class="inline-formula">R
0.90.
profiles
classified
into
67
contact
where
aerosol
class="inline-formula">Na)
greater
500âcmNa
up
tops.
Contact
had
(by
88âcmâ3),
2.5),
lower
2.2âµm)
profiles.
These
differences
associated
aerosolâcloud
interactions
(ACI),
estimates
5âcmâ3,
0.5,
0.2âRe>15âÏ>25
removed.
agreement
between
changes
ACI
driven
by
small
biases
properties
relative
measurements
across
different
regimes.
Thus,
combined
location
concentration,
can
be
study
larger
domains
longer
timescales
possible
using
data.