| Œ¤‹†Žºƒ�ƒ“ƒo�[ |
| Šw�¶ | ||
|---|---|---|
| D3�iŽÐ‰ï�l�j | �¬’Ë �W | |
| M2 | ˆä�ã –«•j | �@�@ |
| M1 | Š�ŽR —Å•ã | �@�@ |
| M1 | îàŽR ˜Ðˆ¨ | �@�@ |
| �@ OB/OG | ||
| �`2020/3 | �¼–ì Œ’ | “Á”C‹³Žö�i2017/4�`2020/3�j
‹³Žö�i�`2017/3�j |
| �`2025/3 | Žðˆä �HŠG | ”ŽŽm‰Û’ö’PˆÊŽæ“¾‘ÞŠw
|
| �`2026/3 | ‰¤ �_“¯ | �CŽm‰Û’ö�C—¹
“ú–{ŠC‚ÌŠC—m•Ï“®‚ÉŠÖ‚í‚é•—‰ž—͂̎ž‹óŠÔ•Ï“® |
| �`2026/3 | �_‘º �«�¶ | �CŽm‰Û’ö�C—¹
ƒ‹ƒ\ƒ“ŠC‹¬“Œ‘¤ŠC—ä‚Å”�¶‚·‚é“à•”’ªŽ¬‚Ì“Á�«‚ÉŠÖ‚·‚錤‹† |
| �`2025/3 | �΋´ Œ÷�¬ | �CŽm‰Û’ö�C—¹
LADCPŠÏ‘ª‚ÉŠî‚Â’ÃŒyŠC‹¬�¼•û‚̋ߊµ�«“à•””g‚ÉŠÖ‚·‚錤‹† |
| �`2025/3 | ‹´Œû ‘å‹P | �CŽm‰Û’ö�C—¹
Argoƒtƒ��[ƒgƒf�[ƒ^‚ÉŠî‚“ú–{ŠC’†‘w�…‚ÌŽž‹óŠÔ•Ï“®‚ÉŠÖ‚·‚錤‹† |
| �`2024/3 | ’J‘º ’q | �CŽm‰Û’ö�C—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’ö�C—¹
’n‹…‰·’g‰»‚ɂƂà‚È‚¤“ú–{ŠC�ã•”ŒÅ—L�…‚̕ϓ®‚ÉŠÖ‚·‚錤‹† |
| �`2021/3 | �‚Žæ ‘å’m | �CŽm‰Û’ö�C—¹
ƒgƒJƒ‰ŠC‹¬‚ÅŠÏ‘ª‚³‚ꂽ“à•”’ªŽ¬‚Ƌߊµ�«“à•”�d—Í”g‚ÉŠÖ‚·‚錤‹† |
| �`2021/3 | œA‰ª ‘ñ–ç | �CŽm‰Û’ö�C—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“¡ �ç�ä | �CŽm‰Û’ö�C—¹
‰Q”S�«ŒW�”‚ÉŠî‚Âæ|‘�˜p‚ÌŠO•”’ªŽ¬‚¨‚æ‚Ñ“à•”’ªŽ¬‚Ì•ª—£‚ÉŠÖ‚·‚錤‹† |
| �`2018/3 | �¬�ì �rŽ÷ | �CŽm‰Û’ö�C—¹
“ŒƒVƒiŠC—¤’Iˆæ’ê‹«ŠE‘w‚É‚¨‚¯‚錜‘÷—±Žq‚Ì’¾�~‘¬“x�„’è |
| �`2017/3 | —› �ªŸÈ | ”ŽŽm‰Û’ö�C—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’ö�C—¹
—L–¾ŠC‚É‚¨‚¯‚é’ªŽ¬�U•�‚¨‚æ‚щÍ�ì—¬—Ê‚Æ�¬‘w�\‘¢�E—n‘¶Ž_‘f”Z“x‚Ƃ̊֌W |
| �`2015/9 | “n•Ó �r‹P | ”ŽŽm‰Û’ö�C—¹
�¼•”ŽR‰A‰ˆŠÝ‚É‚¨‚¯‚é�…‰·‚̕ϓ®“Á�«‚ÉŠÖ‚·‚錤‹† |
| �`2015/3 | •y�Î —I‘¾ | �CŽm‰Û’ö�C—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, ”ŽŽm�i—�Šw�jŽæ“¾
Study on characteristics and behavior of the outer shelf water in the East China Sea |
| �`2012/3 | ’ç ‰p•ã | ”ŽŽm‰Û’ö�C—¹, Šw�pŒ¤‹†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’ö�C—¹
—�—¬Œv‘ª‚ÉŠî‚¢‚½“ú–{ŠC�[‘w‚̉”’¼�\‘¢‚ÉŠÖ‚·‚錤‹† |
| �`2011/3 | �VŒ´ ãĈê | �CŽm‰Û’ö�C—¹
ŽRŒûŒ§�¼•ûŠCˆæ‚ÅŠÏ‘ª‚³‚ê‚é‹˜Ž•�ó�…‰·•Ï“®‚ÉŠÖ‚·‚錤‹† |
| �`2010/9 | ‘åŒc ‘¥”V | ”ŽŽm‰Û’ö�C—¹
”\“o”¼“‡‰ˆŠÝ‚É‚¨‚¯‚é‹}’ª‚Ì”�¶�E“`”d‰ß’ö‚ÉŠÖ‚·‚錤‹† |
| �`2010/9 | Yanlin Cui | ”ŽŽm‰Û’ö�C—¹
Long-term trend and interdecadal oscillation in the Japan Sea proper water |
| �`2007/9 | —› Ÿ²çñ | ”ŽŽm‰Û’ö�C—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’ö�C—¹, Šw�pŒ¤‹†ˆõ
“ú–{ŠC�[‘wˆæ‚É‚¨‚¯‚é‹ßе�«�d—Í”g‚ÉŠÖ‚·‚錤‹† |
| �`2006/3 | —é–Ø —m•½ | �CŽm‰Û’ö�C—¹ ‰Ä‹G‚Ì“ŒƒVƒiŠC—¤’Iˆæ‚É‚¨‚¯‚éƒNƒ�ƒ�ƒtƒBƒ‹‹É‘å‘w‚ÌŒ`�¬�EˆÛŽ�‹@�\‚ɂ‚¢‚Ä |
| �`2005/3 | ”~“c —²Žj | �CŽm‰Û’ö�C—¹ —L–¾ŠC‚É‚¨‚¯‚é—�—¬ƒGƒlƒ‹ƒM�[ˆíŽU—¦ƒÃ‚ÌŒv‘ª‚ÉŠî‚¢‚½’ª—¬‚Ì‘Šˆá‚É‚æ‚é�¬‘w�\‘¢‚Æ’ê‘wŽ_‘f”Z“x•ω»‚ÌŒ©�Ï‚è |
| �`2005/3 | ‰|–{ ”Ž•¶ | �CŽm‰Û’ö�C—¹ ’·�]—¬—ʂ̕ϓ®‚É”º‚¤‘ΔnŠC‹¬‚̉–•ª•ω»‚ÉŠÖ‚·‚錤‹† |
| �`2004/3 | •l“c �W‹K | �CŽm‰Û’ö�C—¹ —�—¬ƒGƒlƒ‹ƒM�[ˆíŽU—¦ƒÃ‚ÌŒv‘ª‚É‚æ‚é—L–¾ŠC‚Ì’ªŽ¬�¬�‡‚ÉŠÖ‚·‚錤‹† |