a
c
68
Homogeneous Models of the Ocean Circulation
b
d
RE• 40
RE = 60
Fig. 2.12.2a-d. Sequence of calculations by Bryan (1963) with lateral friction but with no bottom
friction and with boundary conditions of no slip. a 6/ 6M = 1. b 6/ 6M = 2. c 6/ 6M = 4. d 6/ 6M = 8
c
68
Homogeneous Models of the Ocean Circulation
b
d
RE• 40
RE = 60
Fig. 2.12.2a-d. Sequence of calculations by Bryan (1963) with lateral friction but with no bottom
friction and with boundary conditions of no slip. a 6/ 6M = 1. b 6/ 6M = 2. c 6/ 6M = 4. d 6/ 6M = 8