| human | Q5 |
| P496 | ORCID iD | 0000-0003-1723-9344 |
| P69 | educated at | Hokkaido University | Q1057199 |
| P108 | employer | Hokkaido University | Q1057199 |
| P106 | occupation | researcher | Q1650915 |
| Q73372841 | A mesoscale iron enrichment in the western subarctic Pacific induces a large centric diatom bloom |
| Q113351119 | Biogeochemical and physical linkages between the Arctic Ocean and Sub-Arctic Pacific through marginal seas |
| Q120587361 | Different responses of phytoplankton to Fe manipulation in Fe-limited waters with contrasting surface mixed layer depths in the western subarctic Pacific |
| Q117735941 | Dissolved Iron Concentration and the Solubility Inferred by Humic‐Like Fluorescent Dissolved Organic Matter in the Intermediate Water in the North Pacific Including the Marginal Seas |
| Q117922224 | Dissolved iron distribution in the western and central subarctic Pacific: HNLC water formation and biogeochemical processes |
| Q118079425 | Distribution of Dissolved Zinc in the Western and Central Subarctic North Pacific |
| Q113348909 | Fate of dissolved black carbon in the deep Pacific Ocean |
| Q113357013 | High biomass turnover rates of endosymbiotic nitrogen‐fixing cyanobacteria in the western Bering Sea |
| Q114240309 | Importance of Ekman transport and gyre circulation change on seasonal variation of surface dissolved iron in the western subarctic North Pacific |
| Q117743885 | Iron Supply by Subglacial Discharge Into a Fjord Near the Front of a Marine‐Terminating Glacier in Northwestern Greenland |
| Q113349189 | Long‐Range Lateral Transport of Dissolved Manganese and Iron in the Subarctic Pacific |
| Q117738640 | Meltwater Discharge From Marine‐Terminating Glaciers Drives Biogeochemical Conditions in a Greenlandic Fjord |
| Q117921229 | New insights into the biogeochemical cycling of copper in the subarctic Pacific: Distributions, size fractionation, and organic complexation |
| Q58392665 | Nutrient and phytoplankton dynamics during the stationary and declining phases of a phytoplankton bloom induced by iron-enrichment in the eastern subarctic Pacific |
| Q114700393 | Observations of frazil ice formation and upward sediment transport in the Sea of Okhotsk: A possible mechanism of iron supply to sea ice |
| Q120645738 | Role of nutrients and temperature in shaping distinct summer phytoplankton and microzooplankton population dynamics in the western North Pacific and Bering Sea |
| Q117743677 | Slowly Sinking Particles Underlie Dissolved Iron Transport Across the Pacific Ocean |
| Q95932132 | Subpolar marginal seas fuel the North Pacific through the intermediate water at the termination of the global ocean circulation |
| Q125050557 | The Interannual Variability of Sea Ice Area, Thickness, and Volume in the Southern Sea of Okhotsk and Its Likely Factors |
| Q51695194 | The decline and fate of an iron-induced subarctic phytoplankton bloom. |
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