192
a)
10
IT
e...
~
~ 0.5
0
Z
-<
w
a:
~ a: 0
w
a..
::::!!
w
t-0.5
~
~
a ~ ~ ~ ~ ~ ~ ~ ~ ~ ~
b) SST
TIME [al
30
60
90
120
150
1~
·150
·120
·80
·60
Figure 11: The interdecadal coupled mode of Latif and Barnett (1994). (a) Time series
of model SST in region 150° E -180° E and 25° N - 35° N (b) SST regressed on time series
in (a).
have decadal modes which, through the working of the wind on the water,
can drive decadal motions in the ocean. It would be very difficult to tell
such driven motions from modes.
a)
10
IT
e...
~
~ 0.5
0
Z
-<
w
a:
~ a: 0
w
a..
::::!!
w
t-0.5
~
~
a ~ ~ ~ ~ ~ ~ ~ ~ ~ ~
b) SST
TIME [al
30
60
90
120
150
1~
·150
·120
·80
·60
Figure 11: The interdecadal coupled mode of Latif and Barnett (1994). (a) Time series
of model SST in region 150° E -180° E and 25° N - 35° N (b) SST regressed on time series
in (a).
have decadal modes which, through the working of the wind on the water,
can drive decadal motions in the ocean. It would be very difficult to tell
such driven motions from modes.