Interception loss, I, the amount of precipitation intercepted by forests and evaporated back to the atmosphere plays important roles in the water balance and the climate system by removing approximately one quarter of the annual precipitation from the terrestrial hydrologic cycle. Models are critical for simulating I and its components; the canopy storage, S, and the evaporation rate during the storm, Er. The energy and the water balance methods commonly yield different Er assessments. Hence, there is an urgent need for further model development, testing, and simplification in order to independently evaluate I, S, and Er. The objectives of this study were to: (i) develop an independent model to assess I, S and Er; (ii) compare the model based on its fitness to cumulative and event based measured data of I; and (iii) identify the strengths and limitations of the proposed model. By breaking the linear and power regression equations commonly fitted to the I vs. P, gross precipitation, relationship, the model analytically isolates S and Ep (L L−1) as a function of P. Field measurements of 44 I case studies collected from Mexico and classified into arid & semi-arid, A&S (N = 13), tropical montane cloud, TMC (N = 6), temperate, T (N = 4), and tropical dry, TD (N = 21), forests were used to calibrate the model. Results showed that even though the model was constructed independently of the common equations; it isolates S, Er and Ep and reproduces remarkably well the conventional empirical linear and power regression equations of I vs. P; and simulates unbiased cumulative and individual-storm I values. When coupled with the function of rainfall duration, the model projects lower Er rates than previously anticipated using other empirical approaches. Statistical analysis revealed the likely oscillation of the I vs. P relationship between the linear and power functions depending on rainfall, canopy and climate conditions. The model represents an important advancement in forest hydrology by analytically isolating S, Er, Ep and simulating compatible I values for individual as well as for assemblages of storms. It further clarifies the large variability of Er and helps to explain the role of forests in the water budget and the climate system.
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