A Regional Modeling Study of the South China Sea with High Resolution Hydrostatic and Nonhydrostatic Nested Models of the Luzon Strait

2007 ◽  
Author(s):  
Patrick C. Gallacher
Keyword(s):  
High Resolution ◽  
South China Sea ◽  
South China ◽  
Luzon Strait ◽  
The South China Sea ◽  
Regional Modeling ◽  
The South ◽  
Nested Models ◽  
China Sea ◽  
Modeling Study

Dynamics of dissolved inorganic carbon in the South China Sea: A modeling study

2020 ◽  
Vol 186 ◽  
pp. 102367
Author(s):  
Chuanjun Du ◽  
Jianping Gan ◽  
Chiwing Rex Hui ◽  
Zhongming Lu ◽  
Xiaozheng Zhao ◽  
...  
Keyword(s):  
South China Sea ◽  
South China ◽  
Inorganic Carbon ◽  
Dissolved Inorganic Carbon ◽  
The South China Sea ◽  
The South ◽  
China Sea ◽  
Modeling Study

Seawater Temperature Seasonality in the South China Sea During the Late Holocene Derived From High-Resolution Sr/Ca Ratios of Tridacna Gigas

2015 ◽  
Vol 83 (2) ◽  
pp. 298-306 ◽  
Author(s):  
Hong Yan ◽  
Liguang Sun ◽  
Da Shao ◽  
Yuhong Wang
Keyword(s):  
High Resolution ◽  
South China Sea ◽  
South China ◽  
Late Holocene ◽  
Seawater Temperature ◽  
The South China Sea ◽  
The South ◽  
China Sea ◽  
Tridacna Gigas ◽  
Temperature Seasonality

Temperature seasonality, the difference between summer and winter temperature, has significant influences on global terrestrial and marine ecosystems. However, most of proxy-based climate records are of limited temporal resolution and thus insufficient to quantify the past temperature seasonality. In this study, high-resolution Sr/Ca ratios of modern (live-caught) and fossil (dead-collected) Tridacna gigas shells from the South China Sea (SCS) were used to reconstruct the seawater temperature seasonality during the late Holocene. The averaged seawater temperature seasonality around 2165 ± 75 BC (4.46 ± 1.41°C, derived from the data of 18 yr) were similar to the seasonality of recent decade (4.41 ± 0.82°C during AD 1994–2005), but the temperature seasonality around AD 50 ± 40 (3.69 ± 1.37°C, derived from the data of 48 yr) and AD 990 ± 40 (3.64 ± 0.87°C, derived from the data of 11 yr) was significantly lower than that during AD 1994–2005. The reduced seasonality around AD 990 ± 40 was attributable to the unusually warm winter during the medieval times, probably caused by the weakening of East Asian Winter Monsoon. Our study highlighted the potential of T. gigas shells in providing high-resolution seasonality climate information during the late Holocene.

scholarly journals Holocene ENSO variability in the South China Sea recorded by high-resolution oxygen isotope records from the shells of Tridacna spp.

2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Da Shao ◽  
Yanjun Mei ◽  
Zhongkang Yang ◽  
Yuhong Wang ◽  
Wenqing Yang ◽  
...  
Keyword(s):  
High Resolution ◽  
South China Sea ◽  
Oxygen Isotope ◽  
South China ◽  
The South China Sea ◽  
The South ◽  
Enso Variability ◽  
China Sea
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