Thalassa; an essay on the depth, temperature, and currents of the ocean . O ^, ON O p, - ? in i-^ c c H„ ^H c ?£?: ^ N « « ?AV/5z o9Si ?N/8Z o^^ ?N/22 ^o£ AN. ,21 0^ o92 •A\. ,9 e9Si•N ,e of 2 ?M ,52 o^Si ?N,8i 0O2 N /2I o^i ?A\ ,9? o^^i N ,ff 0^1 Ai ,^^ o25i ?A\ ,1 o2Si N ,2^^ „ZI ?.V\ ,f o25i ?N/ o •AV/6t „oSi?M,82 ,,6 •A\.,6i „6l7i •N;5f .^ ?AV ,2 „Zii ?A\. / 6 ^61^1•N/*^ o2 •aaaxioNOi aNVaaniixvT o8 8cg„°.^ n n O >^0 O S- ^u^O O O N •>- I ^ ^ tC ^ 8 • ^ ,_ O ^ o o, O ^ O t- J:00CO r^ ^ii ui O O O O -• I O O O I I r-O IJ^ U 10 O-N UNq o o ? o o o y, Lorovo ON „ »? o o->o o o ^
Thalassa; an essay on the depth, temperature, and currents of the ocean . O ^, ON O p, - ? in i-^ c c H„ ^H c ?£?: ^ N « « ?AV/5z o9Si ?N/8Z o^^ ?N/22 ^o£ AN. ,21 0^ o92 •A\. ,9 e9Si•N ,e of 2 ?M ,52 o^Si ?N,8i 0O2 N /2I o^i ?A\ ,9? o^^i N ,ff 0^1 Ai ,^^ o25i ?A\ ,1 o2Si N ,2^^ „ZI ?.V\ ,f o25i ?N/ o •AV/6t „oSi?M,82 ,,6 •A\.,6i „6l7i •N;5f .^ ?AV ,2 „Zii ?A\. / 6 ^61^1•N/*^ o2 •aaaxioNOi aNVaaniixvT o8 8cg„°.^ n n O >^0 O S- ^u^O O O N •>- I ^ ^ tC ^ 8 • ^ ,_ O ^ o o, O ^ O t- J:00CO r^ ^ii ui O O O O -• I O O O I I r-O IJ^ U 10 O-N UNq o o ? o o o y, Lorovo ON „ »? o o->o o o ^. o ^O - ^NO :;? ^^°„ ro,!^ fi< u N O in O viS u c^ao WHaHxosipqq co 00 d 6 z z o H d < u. CO o o < z a < I OS H — D I O < CO OC lO a co z< Z) , g Z a H o UJ o III I o Si H o Z CO • >• (0 CO .1 -> UJ » oc Z D < H ~ < < OC ^ UJ < Q. T ^ UJ 00 t- lO cs 6 z. II CQ 00 From Station 2^j 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 in the shapeof equ
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Keywords: ., bookcentury1800, bookdecade1870, bookidthalassa, booksubjectocean
