| Œ¤‹†Žºƒƒ“ƒo[ |
| Šw¶ | ||
|---|---|---|
| D3iŽÐ‰ïlj | ¬’Ë W | |
| M2 | ˆäã –«•j | @@ |
| M1 | ŠŽR —Å•ã | @@ |
| M1 | îàŽR ˜Ðˆ¨ | @@ |
| @ OB/OG | ||
| `2020/3 | ¼–ì Œ’ | “Á”C‹³Žöi2017/4`2020/3j
‹³Žöi`2017/3j |
| `2025/3 | Žðˆä HŠG | ”ŽŽm‰Û’ö’PˆÊŽæ“¾‘ÞŠw
|
| `2026/3 | ‰¤ _“¯ | CŽm‰Û’öC—¹
“ú–{ŠC‚ÌŠC—m•Ï“®‚ÉŠÖ‚í‚é•—‰ž—͂̎ž‹óŠÔ•Ï“® |
| `2026/3 | _‘º «¶ | CŽm‰Û’öC—¹
ƒ‹ƒ\ƒ“ŠC‹¬“Œ‘¤ŠC—ä‚Å”¶‚·‚é“à•”’ªŽ¬‚Ì“Á«‚ÉŠÖ‚·‚錤‹† |
| `2025/3 | ΋´ Œ÷¬ | CŽm‰Û’öC—¹
LADCPŠÏ‘ª‚ÉŠî‚Â’ÃŒyŠC‹¬¼•û‚̋ߊµ«“à•””g‚ÉŠÖ‚·‚錤‹† |
| `2025/3 | ‹´Œû ‘å‹P | CŽm‰Û’öC—¹
Argoƒtƒ[ƒgƒf[ƒ^‚ÉŠî‚“ú–{ŠC’†‘w…‚ÌŽž‹óŠÔ•Ï“®‚ÉŠÖ‚·‚錤‹† |
| `2024/3 | ’J‘º ’q | CŽm‰Û’öC—¹
—¬ŠÇƒ‚ƒfƒ‹‚É‚æ‚é“ú–{ŠC[‘w‚Ì–§“x—¬‚ÌŒ¤‹† |
| `2023/3 | ˆî•x ’¼•F | ”ŽŽm‰Û’ö’PˆÊŽæ“¾‘ÞŠw
|
| `2022/9 | •t ‰x | CŽm‰Û’ö(G30)C—¹
Moored ADCP measurements of the dissipation rate of turbulent kinetic energy in the Kuroshio |
| `2022/3 | ‰–“c K•½ | CŽm‰Û’öC—¹
’n‹…‰·’g‰»‚ɂƂà‚È‚¤“ú–{ŠCã•”ŒÅ—L…‚̕ϓ®‚ÉŠÖ‚·‚錤‹† |
| `2021/3 | ‚Žæ ‘å’m | CŽm‰Û’öC—¹
ƒgƒJƒ‰ŠC‹¬‚ÅŠÏ‘ª‚³‚ꂽ“à•”’ªŽ¬‚Ƌߊµ«“à•”d—Í”g‚ÉŠÖ‚·‚錤‹† |
| `2021/3 | œA‰ª ‘ñ–ç | CŽm‰Û’öC—¹
——¬”÷×\‘¢ŠÏ‘ª‚ɊC’ê‹ß–T‚ł̉”’¼‰Q”S«EŠgŽUŒW”‚Ì„’è |
| `2020/9 | ‘K ‹Ê | CŽm‰Û’ö(G30)C—¹
Study on long-term warming trends in the upper portion of the Japan Sea Proper Water based on Argo float data |
| `2020/3 | ¼“¡ çä | CŽm‰Û’öC—¹
‰Q”S«ŒW”‚ÉŠî‚Âæ|‘˜p‚ÌŠO•”’ªŽ¬‚¨‚æ‚Ñ“à•”’ªŽ¬‚Ì•ª—£‚ÉŠÖ‚·‚錤‹† |
| `2018/3 | ¬ì rŽ÷ | CŽm‰Û’öC—¹
“ŒƒVƒiŠC—¤’Iˆæ’ê‹«ŠE‘w‚É‚¨‚¯‚錜‘÷—±Žq‚Ì’¾~‘¬“x„’è |
| `2017/3 | —› ªŸÈ | ”ŽŽm‰Û’öC—¹, ƒeƒNƒjƒJƒ‹ƒXƒ^ƒbƒt
A role of vertical mixing on nutrient supply into the subsurface chlorophyll maximum in the East China Sea |
| `2016/3 | âŒû ãĈê | CŽm‰Û’öC—¹
—L–¾ŠC‚É‚¨‚¯‚é’ªŽ¬U•‚¨‚æ‚щÍì—¬—ʂƬ‘w\‘¢E—n‘¶Ž_‘f”Z“x‚Ƃ̊֌W |
| `2015/9 | “n•Ó r‹P | ”ŽŽm‰Û’öC—¹
¼•”ŽR‰A‰ˆŠÝ‚É‚¨‚¯‚é…‰·‚̕ϓ®“Á«‚ÉŠÖ‚·‚錤‹† |
| `2015/3 | •yÎ —I‘¾ | CŽm‰Û’öC—¹
‘ΔnŠC‹¬Žü•Ó‚É‚¨‚¯‚é…‰·E‰–•ª‚Ì’ZŽüŠú•Ï“® |
| `2013/9 | ìŠÝ а | ”ŽŽm‰Û’ö’PˆÊŽæ“¾‘ÞŠw
—L–¾ŠC‚Ì•nŽ_‘f…‰ò‚ÌŒ`¬‹@\‚ɂ‚¢‚Ä |
| `2013/3 | –ö”ö –Ε¶ | ”ŽŽm‰Û’ö’PˆÊŽæ“¾‘ÞŠw(`2010/3)Œã, ”ŽŽmi—ŠwjŽæ“¾
Study on characteristics and behavior of the outer shelf water in the East China Sea |
| `2012/3 | ’ç ‰p•ã | ”ŽŽm‰Û’öC—¹, ŠwpŒ¤‹†ˆõ @Œ»: ŽŽ™“‡‘åŠw…ŽYŠw•” •‹³
Study on turbulent mixing and tidal currents under the stratified conditions in the Ariake Sea |
| `2012/3 | ¼‘º ½ŽŸ | CŽm‰Û’öC—¹
——¬Œv‘ª‚ÉŠî‚¢‚½“ú–{ŠC[‘w‚̉”’¼\‘¢‚ÉŠÖ‚·‚錤‹† |
| `2011/3 | VŒ´ ãĈê | CŽm‰Û’öC—¹
ŽRŒûŒ§¼•ûŠCˆæ‚ÅŠÏ‘ª‚³‚ê‚é‹˜Ž•ó…‰·•Ï“®‚ÉŠÖ‚·‚錤‹† |
| `2010/9 | ‘åŒc ‘¥”V | ”ŽŽm‰Û’öC—¹
”\“o”¼“‡‰ˆŠÝ‚É‚¨‚¯‚é‹}’ª‚Ì”¶E“`”d‰ß’ö‚ÉŠÖ‚·‚錤‹† |
| `2010/9 | Yanlin Cui | ”ŽŽm‰Û’öC—¹
Long-term trend and interdecadal oscillation in the Japan Sea proper water |
| `2007/9 | —› Ÿ²çñ | ”ŽŽm‰Û’öC—¹ A numerical study on the intrusion of Kuroshiro water onto the continental shelf of the East China Sea |
| `2006/3 | X N•ã | ”ŽŽm‰Û’öC—¹, ŠwpŒ¤‹†ˆõ
“ú–{ŠC[‘wˆæ‚É‚¨‚¯‚é‹ßе«d—Í”g‚ÉŠÖ‚·‚錤‹† |
| `2006/3 | —é–Ø —m•½ | CŽm‰Û’öC—¹ ‰Ä‹G‚Ì“ŒƒVƒiŠC—¤’Iˆæ‚É‚¨‚¯‚éƒNƒƒƒtƒBƒ‹‹É‘å‘w‚ÌŒ`¬EˆÛŽ‹@\‚ɂ‚¢‚Ä |
| `2005/3 | ”~“c —²Žj | CŽm‰Û’öC—¹ —L–¾ŠC‚É‚¨‚¯‚é——¬ƒGƒlƒ‹ƒM[ˆíŽU—¦ƒÃ‚ÌŒv‘ª‚ÉŠî‚¢‚½’ª—¬‚Ì‘Šˆá‚É‚æ‚鬑w\‘¢‚Æ’ê‘wŽ_‘f”Z“x•ω»‚ÌŒ©Ï‚è |
| `2005/3 | ‰|–{ ”Ž•¶ | CŽm‰Û’öC—¹ ’·]—¬—ʂ̕ϓ®‚É”º‚¤‘ΔnŠC‹¬‚̉–•ª•ω»‚ÉŠÖ‚·‚錤‹† |
| `2004/3 | •l“c W‹K | CŽm‰Û’öC—¹ ——¬ƒGƒlƒ‹ƒM[ˆíŽU—¦ƒÃ‚ÌŒv‘ª‚É‚æ‚é—L–¾ŠC‚Ì’ªŽ¬¬‡‚ÉŠÖ‚·‚錤‹† |