Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Yoshifumi Kuroda"'
Autor:
Yuji Kashino, Takuya Hasegawa, Yasuhisa Ishihara, Yoshifumi Kuroda, Tatsuya Fukuda, Takanori Horii, Iwao Ueki, Yukio Masumoto, Yosuke Fujii, Motoki Nagura, Keisuke Mizuno, Kentaro Ando
Publikováno v:
Journal of Oceanography. 73:403-426
The Triangle Trans‐Ocean Buoy Network (TRITON) project by the Japan Agency for Marine-Earth Science and Technology began with deployment in the western tropical Pacific Ocean in 1998 and has shifted to steady, long-term observations since 1999. Aft
Publikováno v:
Journal of Geophysical Research: Oceans. 118:6543-6560
[1] The structure and variability of the Halmahera and Mindanao Eddies (HE and ME), which are thought to be quasi-stationary eddies, are described based on onboard and time-series observations in the gateway region of the Indonesian Throughflow (ITF)
Autor:
Tomoki Ushiyama, Masanori Yoshizaki, Mikiko Fujita, Ayako Seiki, Yukio Masumoto, Qoosaku Moteki, Kazuaki Yasunaga, Tomoki Miyakawa, Kunio Yoneyama, Hideaki Hase, Ali Shareef, Yoshifumi Kuroda, Kentaro Ando, Keisuke Mizuno, Iwao Ueki, Masaki Katsumata, Naoki Sato, Takanori Horii, Ryuichi Shirooka, Yasushi Fujiyoshi, V. S. N. Murty, Chie Yokoyama, Yukari N. Takayabu, Michael J. McPhaden, Hiroyuki Yamada
Publikováno v:
Bulletin of the American Meteorological Society. 89:1889-1904
The Mirai Indian Ocean cruise for the Study of the Madden-Julian oscillation (MJO)-convection Onset (MISMO) was a field experiment that took place in the central equatorial Indian Ocean during October–December 2006, using the research vessel Mirai,
Publikováno v:
Journal of Physical Oceanography. 38:1780-1793
Velocity at depths of 700–800 m was measured between September 1998 and October 2002 at 2.5°S, 142°E off the New Guinea coast and at 0°, 138°E to examine the New Guinea Coastal Undercurrent (NGCUC) and the current on the equator carrying Antarc
Publikováno v:
Journal of Oceanography. 63:545-559
We investigated variability in the ocean surface-subsurface layer north of New Guinea using Triangle Trans-Ocean Buoy Network (TRITON) buoys at 2°N, 138°E and 0°N, 138°E during the period from October 1999 to July 2004. Both North and South Pacif
Pathways and variability of the Antarctic Intermediate Water in the western equatorial Pacific Ocean
Autor:
Walter Zenk, Yoshifumi Kuroda, Jürgen Holfort, Gerold Siedler, Toru Miyama, Yuji Kashino, Thomas J Müller, Akio Ishida
Publikováno v:
Progress in Oceanography, 67 . pp. 245-281.
In the western equatorial Pacific the low-salinity core of Antarctic Intermediate Water (AAIW) is found at about 800 m depth between potential density levels σθ = 27.2 and 27.3. The pathways of AAIW and the degradation of its core are studied, from
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers. 52:1121-1137
Two moorings were deployed at 168°30′E (Sta. WPW) and 169°30′E (WPE) on 18°20′N in Wake Island Passage (WIP) to measure the velocity of the eastern branch of the deep western boundary current (DWBC) in the North Pacific. We obtained hourly v
Autor:
Iwao Ueki, Tetsuya Nagahama, Yasushi Takatsuki, Takeo Matsumoto, Yoshifumi Kuroda, Kentaro Ando
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 22:282-291
The temperature and conductivity drift (time change of the characteristics) of moored SBE37IM conductivity and temperature (CT) sensors was investigated by pre- and postdeployment calibration of the Triangle TransOcean Buoy Network (TRITON). This buo
Autor:
Kentaro Ando, Yoshifumi Kuroda
Publikováno v:
Journal of Oceanography. 58:599-609
The characteristics of temperature and salinity variation in the Pacific warm pool were investigated using Empirical Orthogonal Function (EOF) analysis on one year's temperature and salinity data in the surface layer (0–50 m) obtained from the Tria
Autor:
Yoshifumi Kuroda
Publikováno v:
Journal of Oceanography. 56:103-116
The variability of the New Guinea Coastal Current (NGCC) and New Guinea Coastal Undercurrent (NGCUC) were examined from one year time series of current data from ADCP moorings at 2°S, 142°E and 2.5°S, 142°E. Change in the hydrographic structure i