East China Sea extends to the east to the chain of theRyukyu Islands; north toKyushu, which is the southernmost ofJapan’s main islands; northwest toCheju IslandoffSouth Korea; and hence west to China. This northern boundary, roughly a line from Cheju Island to the mouth of theYangtze ...
BoundaryPhosphateTransportEastChinaSeaBiologicalProcessThe East China Sea (ECS) is one of the largest marginal seas in the Northwest Pacific, and also one of the most productive regions of the global ocean. Using a three-dimensional Pacific physical-biological model, we investigate the interannual var...
To determine the influence of increasing nutrient transports in the TS, satellite chlorophylladata around the boundary between the TS and the ECS are used to the evaluate long-term biological activity there (Fig.4g). The 24-month moving average anomalous of satellite chlorophylladata were used to ...
In the event, the core of this dispute around the oil and gas field in the East China Sea relates to issues of maritime boundary delimitation and issues of resources acquisition with both states. Chinese policy on oil and gas development is to first consider development issues in accordance ...
East Boundary of the Collision Belt Between Sion-Korean and Yangtze Plates in Eastern China and Their Extension in the Sea 来自 Semantic Scholar 喜欢 0 阅读量: 40 作者:B Yue,J Liao,H Liu,J Zeng,J Shi 摘要: This study tries to summarize various standpoints on the Collision belts of Sino...
Matsu Island, small island under the jurisdiction of Taiwan in the East China Sea, lying off the Min River estuary of mainland China and about 130 miles (210 km) northwest of Chi-lung (Keelung), Taiwan. Matsu is the main island of a group of 19, the Mats
East China SeaKuroshio frontal wavecross‐frontal transportFVCOMPOMone‐way nested model[1] The Finite Volume Coastal Ocean Model (FVCOM) is used to estimate the onshore cross-frontal transport at the shelf break of the East China Sea. Boundary conditions of FVCOM are provided by the Princeton ...
China draws its maritime boundary based on the nine-dash-line that it first pronounced in 1947 and later submitted to the UN Commission on the Continental Shelf in 2009. However, China has never articulated its nine-dash-line’s precise latitudinal and longitudinal location. Therefore, all...
Besides, the high precipitation also extends to Northwestern China due to orbital forcing, corresponding to a slight northwestward shift of the EASM northern boundary over 95°E−110°E (Fig. 3, Fig. 5). The underlying mechanisms may be related to the distribution of the divergence at the ...
The Yangtze Bank Front forms a ring-shaped structure off the Yangtze River estuary in winter, and creates a boundary between the cold shelf water over the Yangtze Shoal and the warm Kuroshio water. The China Coastal Front evolves in winter along the 50-m isobath from the northern ECS south...