2003
DOI: 10.1016/s0378-1127(01)00813-1
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Optical stratification porosity as a measure of vertical canopy structure in a Japanese coastal forest

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Cited by 42 publications
(20 citation statements)
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“…This converter provided with a simple polar projection or an equiangular projection of the tree elements. In order to get the image with higher resolution, monochrome hemispherical photographs were taken during the calm, overcast days (Saito 1996;Zhu et al 2003). The observed heights for the estimation of canopy openness were established at 1.0 m from the forest floor.…”
Section: Sampling Methodologymentioning
confidence: 99%
“…This converter provided with a simple polar projection or an equiangular projection of the tree elements. In order to get the image with higher resolution, monochrome hemispherical photographs were taken during the calm, overcast days (Saito 1996;Zhu et al 2003). The observed heights for the estimation of canopy openness were established at 1.0 m from the forest floor.…”
Section: Sampling Methodologymentioning
confidence: 99%
“…The lens was set to a small aperture and focused on infinity (Frazer et al 2001;Zhu et al 2003). The top of the image was oriented toward the magnetic north.…”
Section: Procedures Of Hpmmentioning
confidence: 99%
“…It is difficult, however, to find the best aerodynamic porosity related to windbreak effectiveness. Recently developed optical stratification porosity methods for estimating aerodynamic porosity may help determine the appropriate amount of pruning for the dense deciduous windbreak (Zhu et al 2003). Pruning should also be approached carefully in the aspect of period and the quantity because of potential damage on habitats for diverse wildlife (Leal et al 2013).…”
Section: Resultsmentioning
confidence: 99%
“…Beyond that, in the wake zone, turbulence increases with eddy size and wind speed returns to upwind scale (McNaughton 1988). The windbreak porosity, which is defined as the ratio or percentage of pore space to the space occupied by tree stems, braches, twigs, and leaves (Loeffler et al 1992, Zhu et al 2003, mediates the effectiveness of wind speed reduction and the extent of the two different zones by influencing the rate of airflow passing through the windbreak pores (McNaughton 1988. Therefore, although height is important, porosity is considered the most important factor in determining horizontal patterns of wind speed reduction such as the position of minimum wind speed and the recovery rate of wind speed (Heisler and Dewalle 1988, Cleugh 1998).…”
Section: Study Site and Field Measurementsmentioning
confidence: 99%