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Fig. 1. Sources of mass errors in ELMS: (a) back-tracking of thecharacteristic lines, with tracking errors in one characteristic lineonly, for a Courant number of 1; (b) use of non-conservative flowfield; and (c) interpolation at the feet of the characteristic lines.
Fig. 2. Continued.
Table 1. Two-dimensional error measures
Fig. 3. Flow Mass errors over a period of three tidal cycles: (a)maximum local mass errors per second, scaled by the elementalvolumes at rest; (b) global mass errors per second in percentage,scaled by the volume of the estuary at rest.
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