jjg OBSERVATIONS AND RESULTS IN PHYSICAL OCEANOGRAPHY 



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Fig. 22 — Current-chart, Pacific Ocean, from observations of salinity and temperature 



of sea water by the Carnegie. 1928-1929 138 



Fig. 23- -Pacific currents in northern summer from preliminary sketch by A.Mertz 138 



Fig. 24- -Schematic representation possible fields density and pressure, vicinity of 



equator, from Carnegie results, 1928-1929 139 



Fig.25- -Profile isobar ic surfaces, from Carnegie results, 1929 139 



Fig.26 — Vertical distribution density, north-south section crossing equator, from 



Carnegie results, 1929 140 



Fig. 27- -Vertical distribution salinity, north-south section crossing equator, from 



Carnegie results, 1929 140 



Fig.28- -Vertical distribution temperature, north- south section crossing equator, from 



Carnegie results, 1929 141 



Fig.29--Vertical distribution oxygen, north-south section crossing equator, from 



Carnegie results. 1929 141 



Fig. 30- -Profile isobaric surfaces, from Carnegie results. 1929 142 



Fig.31--Vertical distribution density, north-south section crossing equator, from 



Carnegie results. 1929 142 



Fig.32--Vertical distribution salinity, north-south section crossing equator, from 



Carnegie results. 1929 143 



Fig.33--Vertical distribution temperature, north-south section crossing equator, from 



Carnegie results, 1929 143 



Fig.34--Current-chart, Pacific Ocean, at surface relative to assumed zero current 



at 2000 meters, from Carnegie results, 1928-1929 144 



Fig.35--Current-chart, Pacific Ocean, at 100 meters relative to assumed zero current 



at 2000 meters, from Carnegie results, 1928-1929 145 



Fig.36--Current-chart, Pacific Ocean, at 200 meters relative to assumed zero current 



at 2000 meters, from Carnegie results, 1928-1929 146 



Fig. 37 — Current-chart, Pacific Ocean, at 400 meters relative to assumed zero current 



at 2000 meters, from Carnegie results, 1928-1929 147 



Fig.38--Current-chart, Pacific Ocean, at 700 meters relative to assumed zero current 



at 2000 meters, from Carnegie results, 1928-1929 148 



