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  1. Subpolar marginal seas fuel the North Pacific through the intermediate water at the termination of the global ocean circulation
  2. Responses of phytoplankton assemblages to iron availability and mixing water masses during the spring bloom in the Oyashio region, NW Pacific
  3. Distribution of Dissolved Zinc in the Western and Central Subarctic North Pacific
  4. Importance of Ekman transport and gyre circulation change on seasonal variation of surface dissolved iron in the western subarctic North Pacific
  5. Dissolved iron distribution in the western and central subarctic Pacific: HNLC water formation and biogeochemical processes
  6. Observations of frazil ice formation and upward sediment transport in the Sea of Okhotsk: A possible mechanism of iron supply to sea ice
  7. Intensive mixing along an island chain controls oceanic biogeochemical cycles