Study on the variability of the Kuroshio at the entrance into the East China Sea
Study on the variability of the Kuroshio at the entrance into the East China Sea
批准号:
17540414
负责人:
MOMOKI Koga
金额:
$2.14万
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (C)
财政年份:
2005
资助国家:
日本
项目状态:
已结题
起止时间:
2005 至 2007
中文摘要
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英文摘要
The variability of the Kuroshio at the entrance into the East China Sea (ECS) is studied mainly using the OKITAI submarine cable voltage data along with satellite altimetry data and drifter-derived surface current data etc. The cable voltage data of about 9 years can monitor the variability of the Kuroshio transport downstream side near the entrance. Other data show wide spatial distributions of surface currents etc. The following results are obtained. (1) The Kuroshio transport varies according to the presence of mesoscale ocean eddies off east coast of Taiwan upstream side. Warm (anti-cyclonic) eddies can increase the transport and cold (cyclonic) eddies decrease the transport. Cold eddies make larger variation than warm eddies. Mesoscale eddies propagating from the east appear rather randomly ; several numbers (2~3) per year. Since the lifetime of each eddy is about several months (1~3), the transport is under the influence of mesoscale eddies almost half of a year. (2) Seasonal var … More iations of the transport and flow field around the entrance are examined using monthly means of these data. There are two typical modes in the variations ; "winter mode" and "summer mode". In winter mode (Dec.-Mar.), the Kuroshio transport upstream side off Luzon increases and some of it flows into the South China Sea (SCS) through the Luzon strait bringing the transport decrease off Taiwan. The variation of the transport in ECS is not so large as that of the upstream side, and shows somewhat regional variation. There is some outflow from ECS to the Pacific Ocean through Ryukyu Islands, which contributes the recirculation to the Kurosho. In summer mode (Jun.last half-Aug.), the transport off Luzon decreases with no flow into SCS. In ECS, there is no special outflow for the recirculation. These seasonal variations seem to be consistent with wind fields. (3) Several studies related to the above are additionally tried ; Sea surface temperature observation using a ferry service connecting Okinawa to Taiwan in ECS crossing the Kuroshio, Data and model analysis of surface Ekman currents in ECS, Climatology of sea surface heat flux, clouds and rain fall under the influence of the Kuroshio in ECS. Less
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「やわらかい南の学と思想-琉球大学の知への誘い」(山里勝己他編)第VI章「4.海底電話線による海流観測」(p.286-294)分担
《软南方研究与思考-琉球大学知识邀请》(山里胜美等编)第六章“4.利用海底电话线观测洋流”(第286-294页)
DOI:
--
发表时间:
2008
期刊:
影响因子:
--
作者:
[Koga, M., 小賀百樹]
通讯作者:
小賀百樹
Chap.6, Section4 'Ocean current observation using a submarine telephone cable'(in Japanese)
第 6 章第 4 节“利用海底电话电缆进行海流观测”(日语)
DOI:
--
发表时间:
2008
期刊:
Yawarakai Minamino Gaku to Shisou-Ryukyu Daigaku no Ti heno Izanai(ed.K.Yamazato et al.)(Okinawa Times)
影响因子:
--
作者:
[Koga, M.]
通讯作者:
M.
「やわらかい南の学と思想 -琉球大学の知への誘い」(第VI章「4.海底電話線による海流観測」(刷り上り:6ページ分)分担執筆
《软南方研究与思考——琉球大学知识邀请函》(第六章“4.利用海底电话线观测洋流”(印数:6页)合着)
DOI:
--
发表时间:
2008
期刊:
影响因子:
--
作者:
[山里勝己, 他編]
通讯作者:
他編
定期フェリー観測資料から見た琉球諸島周辺域の海面水温変動
从定期渡轮观测数据看琉球群岛周边海面温度波动
DOI:
--
发表时间:
2005
期刊:
日本気象学会沖縄支部研究会誌 第34号
影响因子:
--
作者:
[西田浩平, 小賀百樹, 栽吉信, 小賀百樹]
通讯作者:
小賀百樹
Variation of sea surface temperature around Ryukyu Islands observed using a ferry service(in Japanese)
利用渡轮观测到的琉球群岛周边海面温度变化(日语)
DOI:
--
发表时间:
2005
期刊:
J.Okinawa meteor.soc. No.34
影响因子:
--
作者:
[Koga, M.]
通讯作者:
M.
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