Abstract
The deposition of fog to a wind-exposed 3 m tall Puerto Rican cloud forest at 1010 m elevation was studied using the water budget and eddy covariance methods. Fog deposition was calculated from the water budget as throughfall plus stemflow plus interception loss minus rainfall corrected for wind-induced loss and effect of slope. The eddy covariance method was used to calculate the turbulent liquid cloud water flux from instantaneous turbulent deviations of the surface-normal wind component and cloud liquid water content as measured at 4 m above the forest canopy. Fog deposition rates according to the water budget under rain-free conditions (0.11 ± 0.05 mm h
| Original language | English |
|---|---|
| Pages (from-to) | 2669-2692 |
| Journal | Hydrological Processes |
| Volume | 20 |
| DOIs | |
| Publication status | Published - 2006 |
Bibliographical note
DOI: 10.1002/hyp.6065UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 6 Clean Water and Sanitation
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