Civil Engineering Reference
In-Depth Information
Table 5.1 Overview of runs for the sensitivity study, commonly based on TOS-01 (Box-Model)
Main run Description
i) Analysis of Barotropic Cause [temperature and salinity start field: TS01]
T000ug08 TS01HD60F01
T012ug08 TS01HD60F01
Full HAMSOM model code with 3d baroclinic primitive
equations and diffusion, advection scheme, called master
run
T000ug08 TS01HD60F01_BTM
T012ug08 TS01HD60F01_BTM
Master simulation but no baroclinic pressure component,
TS changes barotrop, abbreviation BTM
ii) Analyses of Barotropic Cause [temperature and salinity start field: TS02]
T000ug08 TS02HD60F01_src50
T012ug08 TS02HD60F01_src50
Like master simulation but with TS02, no exchange limi-
tation, called normal run
T000ug08 TS02HD60F01_src51
T012ug08 TS02HD60F01_src51
No vertical exchange of momentum
T000ug08 TS02HD60F01_src52
T012ug08 TS02HD60F01_src52
No vertical TS diffusion
T000ug08 TS02HD60F01_src53
T012ug08 TS02HD60F01_src53
No horizontal TS diffusion
T000ug08 TS02HD60F01_src54
T012ug08 TS02HD60F01_src54
No vertical TS advection
T000ug08 TS02HD60F01_src55
T012ug08 TS02HD60F01_src55
No horizontal TS advection
T000ug08 TS02HD60F01_src56
T012ug08 TS02HD60F01_src56
No vertical TS advection & diffusion
T000ug08 TS02HD60F01_src57
T012ug08 TS02HD60F01_src57
No horizontal TS advection & diffusion
T000ug08 TS02HD60F01_src58
T012ug08 TS02HD60F01_src58
No horizontal exchange of momentum, no Smagorinsky
diffusion
T000ug08 TS02HD60F01_src60
T012ug08 TS02HD60F01_src60
No vertical exchange
T000ug08 TS02HD60F01_src61
T012ug08 TS02HD60F01_src61
No horizontal exchange
T000
8 m/s of prescribed geostrophic wind, TS01 &
TS02 prescribed temperature and salinity field, HD60
¼
no OWF, T012
¼
12-turbine OWF, ug08
¼
¼
ocean depth of 60 m, F01
¼
only wind and
atmospheric surface pressure forcing
5.2.1 Analysis of Dynamical Pattern Under Barotropic
Conditions
Investigation of the ocean
s reaction on operating OWF under barotropic conditions
helps to strike a statement of the triggering of the vertical motion.
Generally, the barotropic conditions of an ocean system are mostly identified in
the relative homogeneous deep layer. Physically, a barotropic ocean means paral-
lelism of isopycnic and isobar surfaces having a constant slope with depth. The
horizontal pressure gradient, as well as the geostrophic flow, is constant with the
depth.
'
 
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