<s>
Geophysical	B-Application
Fluid	I-Application
Dynamics	I-Application
Laboratory	I-Application
Coupled	I-Application
Model	I-Application
(	O
GFDL	O
CM2.5	O
)	O
is	O
a	O
coupled	O
atmosphere	O
–	O
ocean	O
general	B-Application
circulation	I-Application
model	I-Application
(	O
AOGCM	B-Application
)	O
developed	O
at	O
the	O
NOAA	O
Geophysical	O
Fluid	O
Dynamics	O
Laboratory	O
in	O
the	O
United	O
States	O
.	O
</s>
<s>
However	O
,	O
as	O
is	O
the	O
case	O
with	O
most	O
AOGCMs	B-Application
run	O
without	O
flux	O
adjustment	O
,	O
the	O
models	O
fail	O
to	O
capture	O
the	O
cold	O
upwelling	O
zones	O
along	O
the	O
eastern	O
boundaries	O
of	O
the	O
Pacific	O
and	O
Atlantic	O
,	O
and	O
tend	O
to	O
produce	O
an	O
overly	O
dry	O
Amazon	O
basin	O
.	O
</s>
