Copyright © The Oceanographic Society of Japan. Re-Estimation of Annual Anthropogenic Carbon Input from Oyashio into North Pacific Intermediate Water

annual transport of anthropogenic carbon (Canth) to the North Pacific Interme-diate Water (NPIW) from the Western Subarctic Gyre (WSG) has been re-estimated by using newly estimated Oyashio transport and Canth concentration, the latter calcu-lated by the recently-established “∆C* ” method with some...

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Bibliographic Details
Main Authors: Tsuneo Ono, Katsuyuki Sasaki, Ichiro Yasuda
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.623.2641
http://www.terrapub.co.jp/journals/JO/pdf/5906/59060883.pdf
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Summary:annual transport of anthropogenic carbon (Canth) to the North Pacific Interme-diate Water (NPIW) from the Western Subarctic Gyre (WSG) has been re-estimated by using newly estimated Oyashio transport and Canth concentration, the latter calcu-lated by the recently-established “∆C* ” method with some modifications. Estimated annual Canth transport through the nearshore Oyashio west of 146°E was 0.020 ± 0.010 GtC y–1, closely approximating the previous estimation based on a 1-D model calibrated with the CFC vertical distribution. The present study, however, found that an additional 0.025 ± 0.010 GtC y–1 of Canth was transported into NPIW in the region east of 146°E. Total Canth transport, 0.045 GtC y–1, contributes about 35 % of annual Canth accumulation of the whole temperate North Pacific. tions, Ono et al. (2000) estimated that at least 0.023–0.026 GtC y–1 of Canth are transported from the subarctic North Pacific to the NPIW through the K/O Zone. Andreev et al. (2001), on the other hand, estimated that 0.014 GtC y–1 of Canth is transported into the NPIW through the