Observations of frazil ice formation and upward sediment transport in the Sea of Okhotsk: A possible mechanism of iron supply to sea ice-Reference-Cited by-同舟云学术

Observations of frazil ice formation and upward sediment transport in the Sea of Okhotsk: A possible mechanism of iron supply to sea ice

Author:

Ito Masato¹²^ORCID,Ohshima Kay I.³⁴^ORCID,Fukamachi Yasushi³⁴^ORCID,Mizuta Genta¹,Kusumoto Yoshimu⁵,Nishioka Jun³⁴^ORCID

Affiliation:

1. Graduate School of Environmental Science; Hokkaido University; Sapporo Japan

2. Research Fellowship for Young Scientist, Japan Society for the Promotion of Science, Tokyo, Japan

3. Institute of Low Temperature Science, Hokkaido University; Sapporo Japan

4. Arctic Research Center, Hokkaido University; Sapporo Japan

5. Hydro Systems Development Incorporation; Tokyo Japan

Funder

JSPS Research Fellow

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Reference63 articles.

4. Deines , K. L. 1999 Proceedings of the IEEE Sixth Working Conference on Current Measurement (Cat. No.99CH36331) 10.1109/CCM.1999.755249

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