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Directory UMM :Data Elmu:jurnal:A:Agricultural & Forest Meterology:Vol105.Issue4.Dec2000:

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Fig. 1. The single-layer/single-bucket representation: Ts, Ta and T0 are the surface, reference and aerodynamic air temperatures, respectively;θ0 is the initial water content; za, d and zom are the reference, displacement and roughness heights, respectively; rs is the surface resistance; χis an empirical factor linking Ts, Ta and T0.
Fig. 2. Time series of storm/interstorm events.
Fig. 4. Simplified description of the successive profiles of soil water content: top — snapshot at date te, showing the instantaneous fuxes, exfiltration and percolation on the left and infiltration i on the right; bottom — after a time lag of dt, showing the cumulative fluxes corresponding to themovement of the ‘S’-shaped capillary fringe and the rectangular piston, cumulative exfiltration E is represented on the left and infiltration I onthe right).
Fig. 5. The relationship between the capacity and the actual flux according to the TCA.
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