High-Resolution Hydrographic Surveys near the Shelfbreak in the East China Sea: Joint Studies with National Taiwan University as Part of the Quantifying, Predicting, and Exploiting Uncertainty DRI

2009 ◽  
Author(s):  
Glen Gawarkiewicz
Keyword(s):  
High Resolution ◽  
East China Sea ◽  
East China ◽  
The East China Sea ◽  
China Sea

scholarly journals High-Resolution Vertical Observations of Phytoplankton Groups Derived From an in-situ Fluorometer in the East China Sea and Tsushima Strait

2022 ◽  
Vol 8 ◽  
Author(s):  
Qian Xu ◽  
Shengqiang Wang ◽  
Chiho Sukigara ◽  
Joaquim I. Goes ◽  
Helga do Rosario Gomes ◽  
...  
Keyword(s):  
High Resolution ◽  
Water Column ◽  
East China Sea ◽  
Green Algae ◽  
Brown Algae ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
Tsushima Strait

Vertical distribution of phytoplankton composition in the East China Sea (ECS) and Tsushima Strait (TS) was highly variable in the region where the Changjiang River diluted water (CDW), Kuroshio water (KW), and Tsushima water (TW) intersected. An in-situ multiple excitation fluorometer was used to obtain the high-resolution phytoplankton groups data from every meter of the water column. Sharp differences were noted in the distribution of phytoplankton groups in the CDW, KW, and TW. In the CDW, brown algae were generally present ~60% of all depths with exception of subsurface chlorophyll-a maximum (SCM), whereas cyanobacteria (>40%) and green algae plus cryptophytes (>40%) were found above and below the SCM, respectively. In TW, where chlorophyll a (CHL) was lower than in the CDW, brown algae predominated the water column (>60%) and SCM (>80%), except the surface layer where cyanobacteria dominated. In KW, a high fraction of cyanobacteria (>40%) extended up to 40 m, while brown and green algae dominated (>60%) the deeper waters below 40 m at western and eastern stations, respectively. These results can be further related to water property and nutrient concentration of the water masses in each region. This new data show that the in-situ multiple excitation fluorometer can be a powerful tool to estimate high-resolution vertical profiles of phytoplankton groups on a large scale in marine environments.

Quantitative reconstruction of the East Asian Winter Monsoon evolution over the past 100 years: Evidence from high-resolution sedimentary records of the inner continental shelf of the East China Sea

The Holocene ◽  
2020 ◽  
Vol 30 (7) ◽  
pp. 1053-1062
Author(s):  
Xilin Zhang ◽  
Dejiang Fan ◽  
Yuan Tian ◽  
Zhilei Sun ◽  
Bin Zhai ◽  
...  
Keyword(s):  
High Resolution ◽  
East China Sea ◽  
East Asian ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
Asian Winter Monsoon ◽  
Sedimentary Records ◽  
The Past ◽  
Inner Continental Shelf

The East Asian Monsoon (EAM) is a regional factor affecting the East Asian climate and the oceanographic processes of the marginal seas along the Western Pacific. Finding proxies for the EAM intensity and reconstructing the interannual and interdecadal variations of the EAM using high-resolution records are necessary to improve our understanding of the EAM’s role in the global climate system and for predicting climate change. In this paper, high-resolution sedimentary records of sedimentary core C0702 obtained from the inner continental shelf of the East China Sea were comprehensively analyzed using a laser particle size analyzer, an ItraxTM core scanner, and a 210Pb and 137Cs radionuclide analyzer to explore potential proxies for the East Asian Winter Monsoon (EAWM). By combining the obtained results with instrumental observations of the EAM, we established a quantitative formula for the EAWM, which enables to reconstruct the evolution trend of the EAWM during the past 130 years. The sensitive grain-size component F2, with a grain-size range of 14.35–230 µm, and principal component PC1 of the sedimentary deposits of the East China Sea inner shelf can be used as EAWM proxies. The evolution of EAWM in 1880–1950 could be roughly divided into two stages: a weak EAWM period from 1882 to 1900 and a strong EAWM period from 1900 to 1945. This study improves our understanding of the variations in the EAWM on interannual and interdecadal temporal scales.

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