Oxygen isotopic composition and its application to the study of tracing oceanographical process in Bering Sea and Chukchi Sea

In this paper, the (18)O distribution of surface water from the central sea areas of the Bering Sea and the Chukchi Sea was studied. The δ(18)O value of surface water from the Bering Sea is averagely -0.5‰; the δ(18)O contents of the Chukchi Sea are distributionally lower in northeast and higher in...

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Bibliographic Details
Main Authors: Mingduan, Yin, Xianzhang, Zheng, Wenyi, Zeng, Shiyan, Wu, Chuntan, Shi
Format: Article in Journal/Newspaper
Language:English
Published: Polar Research Institute of China - PRIC 2002
Subjects:
Bering Sea
Chukchi Sea
Advances in Polar Science
Chukchi
Polar Science
Online Access:http://library.arcticportal.org/2234/
http://library.arcticportal.org/2234/1/200201006.pdf
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Summary:In this paper, the (18)O distribution of surface water from the central sea areas of the Bering Sea and the Chukchi Sea was studied. The δ(18)O value of surface water from the Bering Sea is averagely -0.5‰; the δ(18)O contents of the Chukchi Sea are distributionally lower in northeast and higher in southwest;

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