. WSI05& 345 350 35 i/-\° 1 1 p â â 1 1 20 - sâ° WS980 Y WS976 ws <??<}â¢' 15*- SJS 100 y ⢠y 300 ⢠⢠10- ⢠⢠"300 15- 10" 345 350 J I I I I 1 1 I 355 _j 1 WS986 o ,00/ ( / 'JOO W5 968 C D Fig- 33- Temperature-salinity relationships at 'William Scoresby' stations, (a) WS 996 and WS 1000 (broken line) off Orange river mouth, survey I. (b) WS 1052 (broken line) and WS 1056 off Orange river mouth, survey II. (c) WS 976 (broken line), WS 979 (dotted line) and WS 980 off Walvis Bay, survey I. (d) WS 986 and WS 988 (broken line) off Sylvia Hill, survey I. Positions of stat
. WSI05& 345 350 35 i/-\° 1 1 p â â 1 1 20 - sâ° WS980 Y WS976 ws <??<}â¢' 15*- SJS 100 y ⢠y 300 ⢠⢠10- ⢠⢠"300 15- 10" 345 350 J I I I I 1 1 I 355 _j 1 WS986 o ,00/ ( / 'JOO W5 968 C D Fig- 33- Temperature-salinity relationships at 'William Scoresby' stations, (a) WS 996 and WS 1000 (broken line) off Orange river mouth, survey I. (b) WS 1052 (broken line) and WS 1056 off Orange river mouth, survey II. (c) WS 976 (broken line), WS 979 (dotted line) and WS 980 off Walvis Bay, survey I. (d) WS 986 and WS 988 (broken line) off Sylvia Hill, survey I. Positions of stations are shown in Figs. 1 and 2. First it should be noted that Bjerknes's theorem applies to currents in which a state of 'stationary motion' is maintained. In other words, it assumes that while the current flows the distribution of mass in the water remains unaltered. This implies that no mixing, or change in properties of the water particles along their path, may take place, and that no vertical translatory movement should occur. On these assumptions the horizontal movement of the water can be related to the distribution
Size: 2045px × 2444px
Photo credit: © The Bookworm Collection / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, booksubjectocean, booksubjectscientificexpediti
