Provenance, structure, and formation of the mud wedge along inner continental shelf of the East China Sea: A synthesis of the Yangtze dispersal system

2012 ◽  
Vol 291-294 ◽  
pp. 176-191 ◽  
Author(s):  
Kehui Xu ◽  
Anchun Li ◽  
J. Paul Liu ◽  
John D. Milliman ◽  
Zuosheng Yang ◽  
...  
Keyword(s):  
Continental Shelf ◽  
East China Sea ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
Inner Continental Shelf

Environmental record from the mud area on the inner continental shelf of the East China Sea since the mid-Holocene

2011 ◽  
Vol 30 (4) ◽  
pp. 43-52 ◽  
Author(s):  
Shengfa Liu ◽  
Xuefa Shi ◽  
Yanguang Liu ◽  
Yonghua Wu ◽  
Gang Yang
Keyword(s):  
Continental Shelf ◽  
East China Sea ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
Inner Continental Shelf ◽  
Mud Area

SEDIMENTATION RATE OF MUD AREA IN THE EAST CHINA SEA INNER CONTINENTAL SHELF

2010 ◽  
Vol 29 (6) ◽  
pp. 1-8 ◽  
Author(s):  
Shengfa LIU ◽  
Xuefa SHI ◽  
Yanguang LIU ◽  
Aimei ZHU ◽  
Gang YANG
Keyword(s):  
Continental Shelf ◽  
East China Sea ◽  
Sedimentation Rate ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
Inner Continental Shelf ◽  
Mud Area

pCO2 distribution and CO2 flux on the inner continental shelf of the East China Sea during summer 2011

2013 ◽  
Vol 31 (5) ◽  
pp. 1088-1097 ◽  
Author(s):  
Baoxiao Qu ◽  
Jinming Song ◽  
Xuegang Li ◽  
Huamao Yuan ◽  
Ning Li ◽  
...  
Keyword(s):  
Continental Shelf ◽  
East China Sea ◽  
Co2 Flux ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
Inner Continental Shelf

scholarly journals Variability of the nutrient stream near Kuroshio's origin

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Chen-Tung Arthur Chen ◽  
Ting-Hsuan Huang ◽  
Chi-Hsuan Wu ◽  
Haiyan Yang ◽  
Xinyu Guo
Keyword(s):  
Pacific Ocean ◽  
Continental Shelf ◽  
East China Sea ◽  
Kuroshio Extension ◽  
Subsurface Water ◽  
East China ◽  
The East China Sea ◽  
High Productivity ◽  
China Sea ◽  
The Kuroshio

AbstractThe Kuroshio—literally “the Black Stream”—is the most substantial current in the Pacific Ocean. It was called the Black Stream because this oligotrophic current is so nutrient-poor in its euphotic zone that the water appears black without the influence of phytoplankton and the associated, often colored dissolved organic matter. Yet, below the euphotic layer, nutrient concentrations increase with depth while current speed declines. Consequently, a core of maximum nutrient flux, the so-called nutrient stream, develops at a depth of roughly between 200 and 800 m. This poorly studied nutrient stream transports nutrients to and supports high productivity and fisheries on the East China Sea continental shelf; it also transports nutrients to and promotes increased productivity and fisheries in the Kuroshio Extension and the subarctic Pacific Ocean. Three modes of the Kuroshio nutrient stream are detected off SE Taiwan for the first time: one has a single-core; one has two cores that are apparently separated by the ridge at 120.6–122° E, and one has two cores that are separated by a southward flow above the ridge. More importantly, northward nutrient transports seem to have been increasing since 2015 as a result of a 30% increase in subsurface water transport, which began in 2013. Such a nutrient stream supports the Kuroshio's high productivity, such as on the East China Sea continental shelf and in the Kuroshio Extension SE of Japan.

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