Civil Engineering Reference
In-Depth Information
Table 3.3 Overview of HAMSOM simulations meteorologically forced with METRAS for
TOS-01 and TOS-02
Overview
simulations
Description, explanation, characteristics,
usage
TOS-01
T012ug08 TS01HD60F01 Master simulation
T012ug05 TS01HD60F01 Wind speed analysis
T012ug16 TS01HD60F01 Wind speed analysis
T048ug08 TS01HD60F01 Wind farm analysis
T080ug08 TS01HD60F01 Wind farm analysis
T160ug08 TS01HD60F01 Wind farm analysis
T012ug08 TS01HD60F02 Consistency analysis
T012ug08 TS01HD60F03 Effect of met. forcing
T012ug08 TS01HD60F04 Brostr ¨ m approach
T012ug08 TS01HD30F01 Intensity in depth
T012ug08 TS03HD30F01 WEGA adaption
TOS-01-src
T012ug08
TS01HD60F01_BTM
T012ug08
TS02HD60F01_src*
Physical analysis, different assumptions in
source code
TOS-02 T8590ug08wd000 Effect by const. N wind
T8590ug08wd045 Effect by const. NE wind
T8590ug08wd090 Effect by const. E wind
T8590ug08wd135 Effect by const. SE wind
T8590ug08wd180 Effect by const. S wind
T8590ug08wd225 Effect by const. SW wind
T8590ug08wd270 Effect by const. W wind
T8590ug08wd315 Effect by const. NW wind
T8590S01 Effect based on real meteorological situation,
June 2010
Main adjustments are based on number of wind turbines, meteorological forcing, and start fields.
Each listed simulation here has got its pondo or counterpart without wind turbines
Abbreviations : T # turbine; ug geostrophic wind [m/s]; TS 01—common start field, 02—two-layer
start field, 03—WEGA start field; HD HAMSOM ocean depth [m]; F METRAS forcing, 01—only
wind, 02—full meteorological forcing, 03—on/off forcing, 04—Brostr¨m run; BTM barotropic
mode; src* source code manipulation; wd wind direction [ ]; S01 summer season
References
Arakawa A, Lamb VR (1977) Computational design of the basic dynamical processes of the
UCLA general circulation model. Methods Comput Phys 17:173
Backhaus J (1985) A three-dimensional model for the simulation of shelf sea dynamics. Ocean
Dyn 38:165-187. doi: 10.1007/BF02328975
Backhaus J, Hainbucher D (1987) A finite difference general circulation model for shelf seas and
its application to low frequency variability on the North European shelf. Elsevier Oceanogra-
phy Series. Elsevier, Amsterdam, pp 221-244
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