Sea surface height and transport stream function of the South China Sea from a variable-grid global ocean circulation model

2003 ◽  
Vol 46 (2) ◽  
pp. 139 ◽  
Author(s):  
Zexun WEI
Keyword(s):  
South China Sea ◽  
Stream Function ◽  
Ocean Circulation ◽  
South China ◽  
Circulation Model ◽  
Sea Surface ◽  
Global Ocean ◽  
Ocean Circulation Model ◽  
Transport Stream ◽  
Global Ocean Circulation

scholarly journals Impact of partial steps and momentum advection schemes in a global ocean circulation model at eddy-permitting resolution

2006 ◽  
Vol 56 (5-6) ◽  
pp. 543-567 ◽  
Author(s):  
Barnier Bernard ◽  
Gurvan Madec ◽  
Thierry Penduff ◽  
Jean-Marc Molines ◽  
Anne-Marie Treguier ◽  
...  
Keyword(s):  
Ocean Circulation ◽  
Circulation Model ◽  
Global Ocean ◽  
Ocean Circulation Model ◽  
Advection Schemes ◽  
Global Ocean Circulation

scholarly journals An evaluation of the barotropic and internal tides in a high-resolution global ocean circulation model

2012 ◽  
Vol 117 (C10) ◽  
pp. n/a-n/a ◽  
Author(s):  
J. F. Shriver ◽  
B. K. Arbic ◽  
J. G. Richman ◽  
R. D. Ray ◽  
E. J. Metzger ◽  
...  
Keyword(s):  
High Resolution ◽  
Ocean Circulation ◽  
Circulation Model ◽  
Internal Tides ◽  
Global Ocean ◽  
Ocean Circulation Model ◽  
Global Ocean Circulation

A multi-resolution ocean simulation of the anthropogenic radiocarbon transient

2021 ◽  
Author(s):  
Martin Butzin ◽  
Dmitry Sidorenko ◽  
Peter Köhler
Keyword(s):  
Ocean Circulation ◽  
Circulation Model ◽  
Horizontal Resolution ◽  
Global Ocean ◽  
Ocean Circulation Model ◽  
Ocean Modelling ◽  
Computational Costs ◽  
Bomb Radiocarbon ◽  
Modelling Studies ◽  
Global Ocean Circulation

<p>We have implemented <sup>14</sup>C and further abiotic tracers (<sup>39</sup>Ar, CFC-12, and SF<sub>6</sub>) into the state-of-the-art ocean circulation model FESOM2. Different to other global ocean circulation models, FESOM2 employs unstructured meshes with variable horizontal resolution. This approach allows for improvements in areas which are commonly poorly resolved in global ocean modelling studies such as upwelling regions, while keeping the overall computational costs still sufficiently moderate. Here, we present results of a transient simulation running from 1850-2015 CE tracing the evolution of the bomb radiocarbon pulse with a focus on the evolution of marine radiocarbon ages. In addition we explore the potential of <sup>39</sup>Argon to complement <sup>14</sup>C dating of marine waters.</p>

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