Figure Page 



51. Topography in dynamic meters. 1.000-m level adjusted to wind-driven geo- 



strophic transport. Ekman divergence considered. May 1963. Drag coeffi- 

 cient 0.0012: meaned stresses from twice-daily reports of pressure 87 



52. Topography in dynamic meters. 2.000-m level adjusted to wind-driven geo- 



strophic transport. Ekman divergence considered, May 1963. Drag coeffi- 

 cient 0.0012: meaned stresses from twice-daily reports of pressure 88 



53. Topography in dynamic meters, 4,000-m level adjusted to wind-driven geo- 



strophic transport, Ekman divergence considered. May 1963. Drag coeffi- 

 cient 0.0012: meaned stresses from twice-daily reports of pressure 89 



54. Topography in dynamic meters, 5,000-m level adjusted to wind-driven geo- 



strophic transport, Ekman divergence considered, May 1963. Drag coeffi- 

 cient 0.0012; meaned stresses from twice-daily reports of pressure 90 



55. Variation of vertical velocity with depth at indicated latitudes along approxi- 



mately 170° W 91 



56. Depth of no zonal motion, 160° W, 1961 92 



57. Depth of no zonal motion, 177° W, 1961 93 



58. Depth of no meridional motion, 169° W, 1961 94 



59. Depth of no zonal motion. 160° W. 1962 95 



60. Depth of no zonal motion, 165° W, May 1963 96 



61. Depth of no zonal motion, 180° W. May 1963 97 



62. Depth of no meridional motion, 172° W. May 1963 98 



63. Annual variations in zonal velocity at 4,000 m 99 



64. Variation with latitude of integrated total transport, September 1961 100 



65. Variation with latitude of zonal Ekman transport, September 1961 101 



66. Variation with latitude of zonal Ekman transport, September 1961 102 



67. Variation with longitude of meridional Ekman transport, September 1961 103 



68. Variation with latitude of integrated geostrophic transport, September 1961... 104 



vin 



