Warming and oxygen decrease of intermediate water in the northwestern North Pacific, originating from the Sea of Okhotsk, 1955-2004

On the basis of all available data, it is found that intermediate water temperature on the 26.8–27.4σθ isopycnals in the northwestern North Pacific has significantly increased during the past 50 years. The largest warming area exists in the western part of the Sea of Okhotsk with a 0.68°C/50-yr temp...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Nakanowatari, Takuya, Ohshima, Kay I., Wakatsuchi, Masaaki
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union
Subjects:
452
Online Access:http://hdl.handle.net/2115/20028
https://doi.org/10.1029/2006GL028243