摘要: Using altimetry data, we analyze the spatiotemporal variations of Kuroshio in the East China Sea. The transport across the shore-side edge of Kuroshio better reflects its exchange with shelf. Kuroshio intrusion varies due to flow-topography interaction on the shore-side of the jet....
(1988) Meander of the Kuroshio front and current variability in the East China Sea. J. Oceanogr. Soc. Japan 44: pp. 125-135Sugimoto, T., S. Kimura and K. Miyaji (1988) Meander of the Kuroshio front and current variability in the East China Sea. J. Oceanogr. Soc. Japan , 44 , ...
A time-dependent, three-dimensional primitive-equation model is used here to study meanders that develop upstream of a western boundary current along a con... LY Oey,C Ping - 《J.phys.oceanogr》 被引量: 890发表: 1991年 Dynamics of subtidal flow in the Taiwan Strait The mean flow is pro...
The path of the Tsushima and Kuroshio Current and Extension around Japan. Tsushima current nomenclature (TWC-1 to 3) is from Tada et al. (2014). The position of the Kuroshio meanders is adapted from Kubo et al. (2004). Base map adapted from General Bathymetric Chart of the Oceans (GEBCO...
1978. Occurrence of small “trigger” meanders in the Kuroshio off southern Kyushu. Journal of the Oceanographical Society of Japan, 34(3): 81–84. doi: 10.1007/BF02109256 [37] Song Tao, Wang Zihe, Xie Pengfei, et al. 2020. A novel dual path gated recurrent unit model for sea surface...
Generation of Small Meanders of the Kuroshio South of Kyushu in a High-Resolution Ocean General Circulation Model the Kuroshio path to the longitude of the Kii Peninsula, which is similar to the so-called trigger meanders for the formation of the large-meander of ... Y Masumoto - 《Journal ...
When the Kuroshio takes the nearshore nonlarge meander path or typical large meander path and resultantly goes through the deeper channel (about 2500 m) of the Izu-Ogasawara Ridge, the KE path adopts a relatively stable state with the two quasi-stationary meanders. On the other hand, when ...
Previous numerical simulations suggest that the Kuroshio path meanders in the northern Okinawa Trough become nonstationary in variance because of changes in background states of the Kuroshio in the northern Okinawa Trough, but a detailed analysis based on observed data has yet to be performed. The ...
By taking correlation with the sea surface dynamic height anomaly observed by satellite altimeters, these Kuroshio variations in the East China Sea are found to be induced by merging of mesoscale eddies from the east at 21掳 N and by coincident Kuroshio meanders east of Taiwan....
In the LM formation stage, the variation of the Kuroshio axis is small west of the Tokara Islands but large to the east due to a small meander of the Kuroshio. In the LM decay stage, the Kuroshio meanders greatly south of Kyushu and is located stably near the coast southeast of Kyushu....