Abstract
North-south temperature, salinity, and oxygen sections for the eastern North Pacific Ocean were constructed from data obtained during the 1957 and 1958 cruises of the M.V. Brown Bear and have been compared with data obtained 29 years earlier by the Carnegie. Long-term changes in distribution of these properties have been investigated by using all the pertinent data available for the years between the Carnegie and Brown Bear expeditions. No significant trends appear in the subarctic water; however, there is a possibility of a shifting of the transition zone between the subarctic and equatorial waters.
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