Abstract
Rainfall interception (I) was measured in 20m tall Puerto Rican tropical forest with complex topography for a 1-year period using totalizing throughfall (TF) and stemflow (SF) gauges that were measured every 2-3days. Measured values were then compared to evaporation under saturated canopy conditions (E) determined with the Penman-Monteith (P-M) equation, using (i) measured (eddy covariance) and (ii) calculated (as a function of forest height and wind speed) values for the aerodynamic conductance to momentum flux (g
Original language | English |
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Pages (from-to) | 1-15 |
Number of pages | 15 |
Journal | Journal of Hydrology |
Volume | 414-415 |
DOIs |
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Publication status | Published - 2012 |