. Thalassa; an essay on the depth, temperature, and currents of the ocean. co00IN S/6 09^ f?l BOQOO«K O 1 CO „ N rfoo « g in NO C^ A\ /i c2Si N^ 021 ^^Hin 00M *AV/2z 0rti S 22 082 n°. , O O tn m O ^ °o 1 °-^^°M^ NONO AV £ 02Si N/ o11 £»$si?S&.2! m 00 NN •s/9f o^e *? , , t^tno O O £°r. \ ro <N O Oo • rn NO N AV/6t 0oSiN/82 06 o^OmmO O goo 8 vO00 *AV/22 c^1 •s/6* cee £• 1 1 hhiaonOn 00 NO AV/6t 06ti •N/Se 0z 0N-inininO § & °°. 8^.^in^o «°0»0 on 00 •AV/^s 0z£i *S/^ o9£ Cni^i On NO AV /2 0lfi?N-/« 0S ^§&8^| 0000 •AV,8S 0«£i?S /£ „<* •dnis^l5| O AV/6 06i^iN/i* 02 °to 0 2 8n8 ^^^ 6 0 < j- c
. Thalassa; an essay on the depth, temperature, and currents of the ocean. co00IN S/6 09^ f?l BOQOO«K O 1 CO „ N rfoo « g in NO C^ A\ /i c2Si N^ 021 ^^Hin 00M *AV/2z 0rti S 22 082 n°. , O O tn m O ^ °o 1 °-^^°M^ NONO AV £ 02Si N/ o11 £»$si?S&.2! m 00 NN •s/9f o^e *? , , t^tno O O £°r. \ ro <N O Oo • rn NO N AV/6t 0oSiN/82 06 o^OmmO O goo 8 vO00 *AV/22 c^1 •s/6* cee £• 1 1 hhiaonOn 00 NO AV/6t 06ti •N/Se 0z 0N-inininO § & °°. 8^.^in^o «°0»0 on 00 •AV/^s 0z£i *S/^ o9£ Cni^i On NO AV /2 0lfi?N-/« 0S ^§&8^| 0000 •AV,8S 0«£i?S /£ „<* •dnis^l5| O AV/6 06i^iN/i* 02 °to 0 2 8n8 ^^^ 6 0 < j- co •aanuoMoi aKvacmxixva g , vO 10 «n Ttvo S £ 6 0 h CO •aanxiONOT onvaanxixvi p ?:=o onOh„- 5- g<u in3- ° °« „ ^ c - g«8^20^ g^ ^dO ;qQ ^dO KH3HX0SIM Q H 6 < O o < z CL < X CO H D .J O < CO CC m o co z D P Z a UJ 8 III X O I! 1- O z CO ^ J > CO to _l n UJ •^ cc z D < 1- ~ < < cc £ HI < Q. T Ss UJ CO l- to CM 6 z zO < co. From Station 253 to Station 288. 119 paratively narrow channel between the latter cape and CapePalmas in Africa, and partly to the fact that the northern limit ofthe south-east trades is placed for the greater part of the yearnorth of the equator, a considerable portion of the South AtlanticEquatorial Current is diverted along the north-east coast of SouthAmerica into the Northern Atlantic. On the other hand, nearlythe whole of the South Pacific Equatorial Current remains on itsown side of the equator, hence the western half of the SouthPacific is much warmer than the western half of the SouthAtlantic. Although the North Atlantic receives such an impor-tant contribution from the South Atlantic, the accumulation ofwarm water in its western half is much inferior to that in thewestern half of the North Pacific ; yet, on account of the restrictedarea of the Atlantic, its eastern half, both north and south of theequator, receives a greater quantity of warm water
Size: 1127px × 2217px
Photo credit: © The Reading Room / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookauthorwild, bookcentury1800, bookdecade1870, booksubjectocean
