Section 3.4: Sea Surface Temperature Anomalies
43
Figure 3.9: Predicted correlation between H' and T' in (3.20) for different
atmospheric feedbacks. It was assumed that q' and m' can be modeled as
first-order Markov processes with 4-day decay time, that q' (or, to first order,
H') has twice the variance of m' and is uncorrelated with it, and that A =
(80 day)-l. (From Frankignoul, 1985) .
. 3
z
o .2
.-
w .1
0::
0::
---_ /
~~~
-8 o~----------------~~----------------~
(J)
(J) _ I
o .
0::
u -.2
-100
--- -~- -.. ~-o
LAG (day)
50
100
43
Figure 3.9: Predicted correlation between H' and T' in (3.20) for different
atmospheric feedbacks. It was assumed that q' and m' can be modeled as
first-order Markov processes with 4-day decay time, that q' (or, to first order,
H') has twice the variance of m' and is uncorrelated with it, and that A =
(80 day)-l. (From Frankignoul, 1985) .
. 3
z
o .2
.-
w .1
0::
0::
---_ /
~~~
-8 o~----------------~~----------------~
(J)
(J) _ I
o .
0::
u -.2
-100
--- -~- -.. ~-o
LAG (day)
50
100