scholarly journals How stationary are the internal tides in a high-resolution global ocean circulation model?

2014 ◽  
Vol 119 (5) ◽  
pp. 2769-2787 ◽  
Author(s):  
Jay F. Shriver ◽  
James G. Richman ◽  
Brian K. Arbic
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 ◽  
...  

2016 ◽  
Vol 97 ◽  
pp. 16-26 ◽  
Author(s):  
Hans E. Ngodock ◽  
Innocent Souopgui ◽  
Alan J. Wallcraft ◽  
James G. Richman ◽  
Jay F. Shriver ◽  
...  

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

2021 ◽  
Author(s):  
Martin Butzin ◽  
Dmitry Sidorenko ◽  
Peter Köhler

<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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