32
Chapter 3: Climate Spectra and Stochastic Climate Models
Figure 3.2: Top: Spectrum ofsensible-plus-latent heat flux at Ocean Weather
Station P (50 0 N, 145°W) over the period 1958-1967. The error bars represent
95% confidence intervals; the continuous line shows the white noise level.
Bottom: corresponding sea-surface temperature spectrum. The continuous
curve is the stochastic model prediction. (From Frankignoul, 1979).
f"
E 2103
N
~
ct
a:
~
u
LU
a.
Vl
x
10 3
>u
Z
LU
::J
0
LU
a:
"Q I
10- 4
0.20
N 0.15
~
ct
Ir
~
t:: 0.10
a.
Vl
X
>~ 0.05
LU
::J
o
LU
e: 0.00
LATENT + SENSIBLE HEAT FLUX
(OWS P, 50 o N, 145°W)
1958-1967
t t ~ t t t t t t
t +t
t
I
t
10- 3
10- 2
10- 1
FREOUENCY (CYCLES/OAY)
SEA SURFACE TEMPERATURE
(OWS P, 50·N, 145·W)
1958-1967
-'--*14.62.3
++ttf
-0.05 1
1
10- 4
10-3
FREOUENCY (CYCLES /OAY)
1
10
10
Chapter 3: Climate Spectra and Stochastic Climate Models
Figure 3.2: Top: Spectrum ofsensible-plus-latent heat flux at Ocean Weather
Station P (50 0 N, 145°W) over the period 1958-1967. The error bars represent
95% confidence intervals; the continuous line shows the white noise level.
Bottom: corresponding sea-surface temperature spectrum. The continuous
curve is the stochastic model prediction. (From Frankignoul, 1979).
f"
E 2103
N
~
ct
a:
~
u
LU
a.
Vl
x
10 3
>u
Z
LU
::J
0
LU
a:
"Q I
10- 4
0.20
N 0.15
~
ct
Ir
~
t:: 0.10
a.
Vl
X
>~ 0.05
LU
::J
o
LU
e: 0.00
LATENT + SENSIBLE HEAT FLUX
(OWS P, 50 o N, 145°W)
1958-1967
t t ~ t t t t t t
t +t
t
I
t
10- 3
10- 2
10- 1
FREOUENCY (CYCLES/OAY)
SEA SURFACE TEMPERATURE
(OWS P, 50·N, 145·W)
1958-1967
-'--*14.62.3
++ttf
-0.05 1
1
10- 4
10-3
FREOUENCY (CYCLES /OAY)
1
10
10