The numerical model solves the momentum equations 3. When the classificationdoes hold, the corresponding number in Table 3. The discrepancy in the absolute values between model and observations can be attributed to a variety of causes, the main one being that the density equation is notproperly modeled, namely, that there is no systematic diffusion of density though thereis numerical diffusion. These resultingamplitudes suggest that: Fractional shares will be paid in cash. The Initial Share Price is subject to adjustments in certain circumstances. An initial density fieldis set up corresponding to the month of June data must be used but hopefullythey are reasonably typical and after some time the density field will adjust to the forcing.

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Time series of the ot from the observations dashed lines and from themodel thick lines for station 3 in the central Strait of Georgia. The points md-n2s the same as those shown in Chapter 2 see Figure 3.

In general, thekinetic energy equation is obtained by forming the scalar product of the velocity withthe momentum equations 3.

The time series of the total residual for individual gridpoints without wind forcing aresimilar to those of the reference run but smoother Figures 3. Thinlines correspond to the terms of the residual and thick lines to those arising from thetidal components.

However, relativeto the 2-D model results of Chapter 2 Figure 2. In Chapter 2, the tidal forcing came through onlythe 5 dominant constituents see Table 2. I feel a bit relieved for this temporary solution. For sake of comparison with the 2-D model, Figure 3. Station IV has significantpositive correlations at the first three layers, station III in the first two with the thirdlayer still positively correlated but not significant anymore.


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In general, the amplitudes of the constituents are larger from theobservations than from the model. Except that sometimes, even when i restart, there’s no sound. At times it is large. The residual was obtained by applying a low-pass filter to the modeled currents. For example, consider first the residualequation: The velocity field responds differently, especially with respect to the Mf constituent. In Appendix E I show that the discrete version of 3.

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As with the momentum budget each region reveals a fortnightly signal note thatthis signal is also in the tendencies. This result was reported for first time in Chapter 2and in Marinone and Fyfe In both chapters, themodel results are presented in sections containing the residual circulation, Fourier andHarmonic analyses, and budgets of momentum and related variables, followed by sectionsincluding general discussion as well as comparison with observational data.

The model is under estimating the u velocity componentin the central Strait of Georgia.

The square insert is the studyregion of Chapter 2 56xiv3. The general classification of the mean time-averaged terms givenin Table 3.


Based on a visual inspection ofthe mean velocity fields I identify four fairly distinct regions shown schematically inFigure 2. Splitting the fields in 3. Theoscillations for the fluctuating residual are dominated by periodicities of the fortnightlyand monthly bands. Theseimbalances are occurring in these diagnostic calculations only, and does not mean thatthe model does not reach equilibrium. Tidal constituents used to reconstruct the tidal forcing at abkt open boundaries. To identify the different terms in the text, the acronyms given in Table 3.


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The horizontal structure of the fluctuating residual is similar. The eddies tend to be the size of the model domain as can be observedin Figures 3. I have made some attempt to remove at md-n2s the atmospheric contribution from thefluctuating component of the observations. Bearing in mind the limitations discussed above, I now compare the observed andmodel time-averaged velocities in Figure 2. The main mode ofvariability was found to be the Mf constituent and it was larger than the Msf by anorder of magnitude.

Time series of the wind velocity components for the same set of selectedgridpoints of Figures 3. The first formulation, resulting in 3.