Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Keiichiro Sakaoka"'
Autor:
Aya Omata, Kenshi Kuma, Nanako Hioki, Satoko Ishikawa, Ren Uchida, Yoshihiko Kamei, Keiichiro Sakaoka, Shohgo Takagi, Hiromichi Ueno, Yutaka Isoda
Publikováno v:
Journal of Geophysical Research: Oceans. 118:1257-1271
[1] We measured water-column iron concentrations from west to east along 47°N in the subarctic North Pacific, and in the Bering Sea. In the North Pacific dissolved Fe (D-Fe) showed surface depletion, mid-depth maxima at 1000–1500 m (west, 1.3–1.
Publikováno v:
Oceanography in Japan. 14:513-525
Suga et al. (2003)は180°断面で観測される亜表層の水温極小水の起源がベーリング海西部の冬季混合層にあることを示した。アラスカ湾においても水温極小が存在しており, この水塊の存在は
Publikováno v:
Journal of Geophysical Research. 116
Autor:
Keiichiro Sakaoka, Yoshihiko Kamei, Kenshi Kuma, Eri Manabe, Shohgo Takagi, Hyoe Takata, Kenji Toya, Koji Sugie, Yutaka Isoda, Saori Kitayama, Sei-Ichi Saitoh
Publikováno v:
Journal of Geophysical Research. 114
1
Autor:
Sei-Ichi Saitoh, Keiichiro Sakaoka, Yutaka Isoda, Kenshi Kuma, Hyoe Takata, Shohgo Takagi, Mitsuru Chikira, Yukiyo Saitoh
Publikováno v:
Geophysical Research Letters. 33
An edited version of this paper was published by AGU. Copyright 2006, American Geophysical Union, Geophysical Research Letters, 2006
Labile dissolved Fe (
Labile dissolved Fe (
Publikováno v:
Journal of Geophysical Research, Oceans. 116:C02021
[1] Multiyear (2003–2008) time series observations along the A line provided information on the temporal variability of the dissolved iron (diss-Fe) concentration in the Oyashio region of the western subarctic Pacific, and the data indicated that t