CMS-Flow:Boundary Conditions

Tidal Constituent

The water level predictions are based on a harmonic equation with several arguments

$\eta (t)=\sum _{i=1}^{N}f_{i}A_{i}\cos(\omega _{i}t+V_{i}^{0}+u_{i}-\kappa _{i})$

(1)

where $A$ is the constituent mean amplitude, $f$ is a factor that reduces the mean amplitude and varies in time, $V_{0}+u$ are the constituents equilibrium phase and $\kappa$ is the constituent phase lag or epoch. Table 1 shows a list of the currently supported tidal constituents in CMS.

Constituent	Speed	Constituent	Speed	Constituent	Speed
SA	0.041067	SSA	0.082137	MM	0.54438	MSF	1.0159
MF	1.098	2Q1	12.8543	Q1	13.3987	RHO1	13.4715
O1	13.943	M1	14.4967	P1	14.9589	S1	15
K1	15.0411	J1	15.5854	OO1	16.1391	2N2	27.8954
MU2	27.9682	N2	28.4397	NU2	28.5126	M2	28.9841
LDA2	29.4556	L2	29.5285	T2	29.9589	S2	30
R2	30.0411	K2	30.0821	2SM2	31.0159	2MK3	42.9271
M3	43.4762	MK3	44.0252	MN4	57.4238	M4	57.9682
MS4	58.9841	S4	60	M6	86.9523	S6	90
M8	115.9364

Flux

The water flux is specified as m^3/sec per cell along the cell string. This value is multiplied by the number of cells in the cell string to obtain the total flux. The total flux is then redistributed along the boundary according to

$q_{i}={\frac {Q_{b}}{\sum \Delta s_{i}h_{i}^{1+r}/n_{i}}}{\frac {h_{i}^{1+r}}{n_{i}}}$

(2)

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Symbol	Description
$t$	Time
$A$	Constituent mean amplitude
$f$	Constituent nodal factor
$V^{0}$	Constituent equilibrium argument
$u$	Constituent equilibrium argument
$\kappa$	Constituent phase or epoch

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