Civil Engineering Reference
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Fig. 5.34 Temperature profiles along the x -section from (a1)-(c1) W to E and along the y -section
from (a2)-(c2) S to N of the restricted forcing F01 (a), the full meteorological forcing F03 (b), and
the difference of both (c). Considering full forcing, the upper layers become cooler by around
1.2 C, while close to the thermocline the layers are warmer by 0.8-0.9 C
Surface elevation and u -component at the surface correlate run F01 and run F03
with 1.00, v -component of run F01 and run F03 is correlated by 0.94 with RMSD in
order of 10 3 m/s.
The vertical velocity component w in 12-m depth is highly correlated by 0.99
and shows RMSD along the positions of 2.43E-06 m/s. The contrasts in the
horizontal velocity components, obviously in v -component, with depth are a result
of changes in the temperature, salinity field, and the density field in run F03.
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