scholarly journals Cross-shelf water exchange in the East China Sea as estimated by satellite altimetry and in situ hydrographic measurement

2016 ◽  
Vol 121 (9) ◽  
pp. 7192-7211 ◽  
Author(s):  
Ruibin Ding ◽  
Daji Huang ◽  
Jiliang Xuan ◽  
Bernhard Mayer ◽  
Feng Zhou ◽  
...  
Keyword(s):  
East China Sea ◽  
Satellite Altimetry ◽  
Water Exchange ◽  
East China ◽  
Shelf Water ◽  
The East China Sea ◽  
China Sea

scholarly journals Effectiveness of stocking Sparus macrocephalus fry in situ in the East China Sea

2019 ◽  
Vol 4 (2) ◽  
pp. 74-79
Author(s):  
Qingsong Hu ◽  
Ning Bao ◽  
Hafiz Abdur Rahman ◽  
Yazhou Jiang ◽  
Shouyu Zhang ◽  
...  
Keyword(s):  
East China Sea ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
Sparus Macrocephalus

Characteristics of outer shelf water in the East China Sea

2013 ◽  
Vol 69 (2) ◽  
pp. 245-258 ◽  
Author(s):  
Shigefumi Yanao ◽  
Takeshi Matsuno
Keyword(s):  
East China Sea ◽  
Outer Shelf ◽  
East China ◽  
Shelf Water ◽  
The East China Sea ◽  
China Sea

scholarly journals Water Exchange across Isobaths over the Continental Shelf of the East China Sea

2017 ◽  
Vol 47 (5) ◽  
pp. 1043-1060 ◽  
Author(s):  
Jing Zhang ◽  
Xinyu Guo ◽  
Liang Zhao ◽  
Yasumasa Miyazawa ◽  
Qun Sun
Keyword(s):  
Continental Shelf ◽  
East China Sea ◽  
Water Exchange ◽  
Bottom Layer ◽  
Taiwan Strait ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
The Taiwan Strait ◽  
The Kuroshio

AbstractOnshore and offshore currents and the associated volume transport across three isobaths (50, 100, and 200 m) over the continental shelf of the East China Sea were examined using daily reanalysis data in 1993–2012. After being averaged along the isobaths, the velocities across 100 and 50 m are onshore in the bottom layer but offshore in the surface layer. In contrast, those across the 200-m isobath are onshore in the surface and bottom layers but without a clear direction in the midlayer, suggesting a three-layer structure. The surface offshore current across the 100-m isobath mainly arises from the Taiwan Strait Current, while the surface onshore current across the 200-m isobath mainly arises from the Kuroshio, both of which converge in the area between the 100- and 200-m isobaths and flow toward the Tsushima Strait. The control of bottom Ekman dynamics on the onshore bottom currents is important at the 100-m isobath, partly important at the 200-m isobath, and slightly important at the 50-m isobath. The seasonal variations of onshore and offshore currents in the surface layers across the three isobaths are likely caused by local winds, the Taiwan Strait Current, and the Changjiang discharge, while those in midlayer across the 200-m isobath demonstrate a strong geostrophic control and can be interpreted from a traditional viewpoint on the Kuroshio intrusion over the entire water column across the shelf slope. The close connection of bottom onshore currents across the three isobaths suggests that the bottom layer is an important pathway for water exchange of shelf water and the open sea.

Satellite-derived SST validation based on in-situ data during summer in the East China Sea and western North Pacific

2010 ◽  
Vol 45 (3) ◽  
pp. 159-170 ◽  
Author(s):  
Eun Jin Kim ◽  
Sok Kuh Kang ◽  
Sung-Tae Jang ◽  
Jae Hak Lee ◽  
Young Ho Kim ◽  
...  
Keyword(s):  
East China Sea ◽  
North Pacific ◽  
Western North Pacific ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
In Situ Data
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