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. 2019 Nov 26;10:2722. doi: 10.3389/fmicb.2019.02722

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Copyright © 2019 Shiozaki, Hirose, Hamasaki, Kaneko, Ishikawa and Harada.

This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

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(A) Location of station S1 in the northwestern North Pacific Ocean. (B) Seasonal variations in satellite-derived (MODIS Aqua) chlorophyll a (chl a), sea surface temperature, and Argo-derived mixed layer depth (MLD) (Hosoda et al., 2010) at station S1 (1° × 1° area), averaged between January 2003 and December 2012. Colored bars indicate the months in which the cruises took place. (C) Vertical profiles of temperature, salinity, dissolved oxygen, nitrate, and chl a during each cruise.