The Three-Layer Model
60p--------------------...... 50
<:
I)
'0~~--~~--~-----L----~----L ---~----~
60
50
40
30
20
10
0
LONGITUDE ( 0 W)
215
Fig. 4.7.3. Different dynamical domains of the flow in the three-layer model for the example
discussed by Luyten et a!. (1983)
-
-06
-0.4
50
40
30
20
10
0 80
70
60
50
40
30
20
10
0
LATITUDE ('W)
LONG! TUDE (•WJ
Fig. 4.7.4. Meridional cross section of the layer thicknesses in the three-layer model of Luyten eta!.
(1983)