27
Also remarkable are shorter fluctuations which are found both in the measurements and
model predictions. Temperatures at the surface show a distinct daily cycle, while a semi
diurnal (tidal) signal is found near the bottom.
MARNET Station 'Deutsche Bucht'
20
19
U 18
measured (surface)
mo de ltd (surface)
me as ure d (bo tto m)
modelled (bottom)
f:
- ■'»1»■’* .
i . .. - . - A /'*/■'• w v k<: V. ‘:
%' 1 \& .%■ ,>V . i V
: V v V *'* . * . \ SA r: ^
/■ ' _ . T"'5y '
'rtf' ; > ‘ « <^ ■
^rsiv-
r./V
v .
\ ? V'
■f / " t + "* ■ ■
:A rVVA#^ 5
. ‘ " . * *>, ;t tt;\ »•' '
Surface:
No.ofvalues: 1520
Bias: 0.22 °C
Std. Dev.: 0.35 °C
Bottom:
No.ofvalues: 1520
Bias: 0.51 °C
Std. Dev.: 0.13°C
24.07.1999
29.07.1999
03.08.1999
08.08.1999
13.08.1999
1803.1999
Fig. 12: Measured and predicted surface and bottom water temperatures at the
station 'Deutsche Bucht'