Three-dimensional Lagrangian Tracer Modelling in Wadden Sea ...
Three-dimensional Lagrangian Tracer Modelling in Wadden Sea ...
Three-dimensional Lagrangian Tracer Modelling in Wadden Sea ...
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CHAPTER 2. THEORY 35<br />
2.4.2.4 Implementation<br />
The random walk model implemented <strong>in</strong>to GETM and GOTM is based on<br />
the scheme proposed by Hunter et al. [1993]. A diffusive step is carried out<br />
each macro time step ∆t for the <strong>in</strong>ternal mode of GETM and the particle<br />
position is updated accord<strong>in</strong>g to (2.4.63)-(2.4.65) with a slight modification:<br />
the random numbers Z1, Z2, Z3 are not taken from the standard normal<br />
distribution but from a uniform distribution with zero mean and a variance<br />
of 1<br />
3<br />
(i.e. the uniform random numbers vary between +1 and −1). Accord<strong>in</strong>g<br />
to the L<strong>in</strong>deberg-Feller central limit theorem (Feller [1935]) the distribution<br />
of a normal form variate<br />
Znorm =<br />
Z<br />
� 〈(Z − 〈Z〉) 2 〉 , (2.4.66)<br />
where Z is a random variable with zero mean and f<strong>in</strong>ite variance 〈(Z − 〈Z〉) 2 〉,<br />
tends to the normal distribution with zero mean and unit variance N (0, 1).<br />
In order to <strong>in</strong>clude Znorm = Z/ � 1/3 the random walk model (2.4.63)-<br />
(2.4.65) becomes<br />
xn+1 = xn + ∂Ax(�xn)<br />
∂x<br />
yn+1 = yn + ∂Ay(�xn)<br />
∆t + Z2<br />
∂y<br />
zn+1 = zn + ∂ν′ (�xn)<br />
∆t + Z3<br />
∂z<br />
�<br />
∆t + Z1 6 Ax(�xn) ∆t (2.4.67)<br />
�<br />
6 Ay(�xn) ∆t (2.4.68)<br />
� 6 ν ′ (�xn) ∆t. (2.4.69)<br />
In the application of the random walk model to the <strong>Wadden</strong> <strong>Sea</strong>, horizontal<br />
diffusion is not <strong>in</strong>cluded. The horizontal diffusivities Ax, Ay are set to<br />
zero s<strong>in</strong>ce the shear dispersion (comb<strong>in</strong>ation of vertical mix<strong>in</strong>g and shear)<br />
is the major horizontal dispersion mechanism. The vertical diffusivity ν ′ is<br />
calculated by the turbulence model us<strong>in</strong>g the Kolmogorov-Prandtl relation<br />
(Burchard and Bold<strong>in</strong>g [2002])<br />
ν ′ = c ′ k<br />
µ<br />
2<br />
. (2.4.70)<br />
ε<br />
Here, k is the turbulent k<strong>in</strong>etic energy, ε is the dissipation rate, and c ′<br />
µ is a<br />
so-called stability function depend<strong>in</strong>g on shear, stratification and turbulent<br />
time scale, τ = k/ε. The vertical eddy diffusivity is located on the Eulerian<br />
grid at the position of the vertical velocity component w. Therefore it is<br />
easy to l<strong>in</strong>early <strong>in</strong>terpolate ν ′ to the <strong>in</strong>stantaneous vertical position zn of a<br />
tracer <strong>in</strong> the grid box with <strong>in</strong>dex (i, j, k) and update the position accord<strong>in</strong>g