2020
DOI: 10.3390/w12051274
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Consistent Boundary Conditions for Age Calculations

Abstract: Age can be evaluated at any time and position to understand transport processes taking place in the aquatic environment, including for reactive tracers. In the framework of the Constituent-oriented Age and Residence time Theory (CART), the age of a constituent or an aggregate of constituents, including the water itself, is usually defined as the time elapsed since leaving the boundary where the age is set or reset to zero. The age is evaluated as the ratio of the age concentration to the concentration, which a… Show more

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Cited by 10 publications
(7 citation statements)
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“…The transport terms in both equations are discretized with a flux-limited linear advection scheme providing positivity preserving solutions for c and α. It must be noted, however, that for the mean-particle age a computed as the quotient of α and c, positivity of the solution is generally not guaranteed unless a more strict flux-limiting criterion is used (Deleersnijder et al, 2020).…”
Section: Model Descriptionmentioning
confidence: 99%
“…The transport terms in both equations are discretized with a flux-limited linear advection scheme providing positivity preserving solutions for c and α. It must be noted, however, that for the mean-particle age a computed as the quotient of α and c, positivity of the solution is generally not guaranteed unless a more strict flux-limiting criterion is used (Deleersnijder et al, 2020).…”
Section: Model Descriptionmentioning
confidence: 99%
“…Deleersnijder et al [7] investigate the boundary conditions for age calculations. In CART, the mean age is computed as the ratio of the "age concentration" to the concentration of a numerical tracer.…”
Section: Timescale-focused Contributionsmentioning
confidence: 99%
“…Furthermore, this intensive data-generating capacity enriches our awareness and understanding of individual processes operating over a broad range of spatial and temporal scales, but the net effect-the "upshot"-of those processes and their interactions may be challenging to identify. Techniques for distilling, simplifying, and extracting the essence from large, complex environmental datasets have arguably never been more necessary [5][6][7].…”
mentioning
confidence: 99%
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“…The age of a water particle is set to zero at the moment it enters the domain through inlet Γ in . The incoming-flux condition reads [36]:…”
Section: Water Age Distribution Functionmentioning
confidence: 99%