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global O
climate O
change O
. O
Large B-climate-models
eddy I-climate-models
simulation I-climate-models
( O
LES B-climate-models
) O
models O
have O
supplied O
insight O
into O
these O
cloudtopped B-climate-nature
boundary I-climate-nature
layers I-climate-nature
( O
CTBLs B-climate-nature
) O
and O
show O
that O
cloud B-climate-nature
macroscopic O
properties O
such O
as O
cloud B-climate-properties
base I-climate-properties
, O
height B-climate-properties
, O
and O
fraction O
result O
from O
a O
delicate O
balance O
between O
surface B-climate-nature
fluxes I-climate-nature
, O
cloud B-climate-nature
radiative I-climate-nature
fluxes I-climate-nature
, O
large O
scale O
subsidence B-climate-nature
, O
and O
when O
present O
, O
precipitation B-climate-nature
in O
the O
form O
of O
drizzle B-climate-nature
. O
In O
this O
study O
the O
US B-climate-models
Navy I-climate-models
Coupled I-climate-models
Ocean I-climate-models
/ I-climate-models
Atmosphere I-climate-models
Mesoscale I-climate-models
Prediction I-climate-models
System I-climate-models
( O
COAMPS I-climate-models
†† O
; O
Hodur O
1997 O
) O
has O
been O
applied O
to O
a O
case O
of O
coastal O
California O
summer O
season O
stratocumulus B-climate-nature
. O