Fog deposition in tall tussock grassland, South Island, New Zealand
1997
Cameron, C.S. | Murray, D.L. | Fahey, B.D. | Jackson, R.M. | Kelliher, F.M. | Fisher, G.W.
Hill cloud microphysics was examined with a forward scattering spectrometer probe over tall tussock grassland at Swampy Summit near Dunedin, New Zealand. In a 4-month period, cloud water drop diameter spectra were obtained for 17 cloud-ground intersection events that varied from 1 to 61 h in duration. Rain fell in most events. Easterly conditions made up 60% of the events and had a median cloud drop diameter of 13.9 micrometer and 0.14 g m-3 liquid water content. For southwest winds, median drop diameter and liquid water content were significantly smaller at 9.8 micrometer and 0.05 g m-3. Aerodynamic conductance for momentum transfer, measured with a three-dimensional sonic anemometer, varied linearly with wind speed (R2 = 0.7) between 50 and 70 mm s-1 for wind speeds from 4 to 9 m s-1. Combining this relation with the cloud liquid water content measurements, cloud water deposition rates were estimated onto the 0.8-m-tall tussock canopy of one-sided leaf area index = 3. These estimates were in the range 0.02-0.26 mm h-1 with a median of 0.05 mm h-1 which is the same as the median rate derived from the water balance of a large weighing lysimeter containing eight tussock plants. However, the water balance included a number of small quantities with determination of evaporation and rainfall being particularly difficult. Consequently, the lowest cloud water deposition rates for the water balance were sometimes negative. Nevertheless, even the maximum estimated rates incorporated into an annual calculation suggest cloud water deposition is unlikely to be a significant component of the water balance of a tall tussock grassland catchment. In the uplands of southern New Zealand, changing land use from tall tussock to pastoral agriculture with short vegetation is unlikely to alter streamflows via the cloud water deposition process.
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