Hemispherical photography
Hemispherical photography, also known as canopy photography, is a technique to estimate solar radiation and characterize plant canopy geometry using photographs taken looking upward through an extreme wide-angle lens or a fisheye lens. Typically, the viewing angle approaches or equals 180-degrees, such that all sky directions are simultaneously visible. The resulting photographs record the geometry of visible sky, or conversely the geometry of sky obstruction by plant canopies or other near-ground features. This geometry can be measured precisely and used to calculate solar radiation transmitted through plant canopies, as well as to estimate aspects of canopy structure such as leaf area index. Detailed treatments of field and analytical methodology have been provided by Paul Rich and Robert Pearcy.
History
The hemispherical lens was originally designed by Robin Hill to view the entire sky for meteorological studies of cloud formation. Foresters and ecologists conceived of using photographic techniques to study the light environment in forests by examining the canopy geometry. In particular, Evans and Coombe estimated sunlight penetration through forest canopy openings by overlaying diagrams of the sun track on hemispherical photographs. Later, Margaret Anderson provided a thorough theoretical treatment for calculating the transmission of direct and diffuse components of solar radiation through canopy openings using hemispherical photographs. At that time hemispherical photograph analysis required tedious manual scoring of overlays of sky quadrants and the track of the sun. With the advent of personal computers, researchers developed digital techniques for rapid analysis of hemispherical photographs. In recent years, researchers have started using digital cameras in favor of film cameras, and algorithms are being developed for automated image classification and analysis. Various commercial software programs have become available for hemispherical photograph analysis, and the technique has been applied for diverse uses in ecology, meteorology, forestry, and agriculture.Applications
Hemispherical photography has been used successfully in a broad range of applications involving microsite characterization and estimation of the solar radiation near the ground and beneath plant canopies. For example, hemispherical photography has been used to characterize winter roosting sites for monarch butterflies, effects of forest edges, influence of forest treefall gaps on tree regeneration, spatial and temporal variability of light in tropical rainforest understory, impacts of hurricanes on forest ecology, leaf area index for validation of remote sensing, canopy architecture of boreal forests, light environment in old growth temperate rain forests, and management of vineyard trellises to make better wine.Theory
Solar Radiation Calculations
Direct and diffuse components of solar radiation are calculated separately. Direct radiation is calculated as the sum of all direct radiation originating from visible sky directions along the path of the sun. Similarly, diffuse solar radiation is calculated as the sum of all diffuse radiation originating from any visible sky directions. The sum of direct and diffuse components gives global radiation.These calculations require theoretical or empirical distributions of direct and diffuse radiation in the open, without canopy or other sky obstruction. Usually calculations are performed for either photosynthetically active radiation or insolation integrated over all wavelengths, measured in kilowatt-hours per square meter.
The fundamental assumption is that most solar radiation originates from visible sky directions, a strong first order effect, and that reflected radiation from the canopy or other near-ground features is negligible, a small second order effect. Another assumption is that the geometry of visible sky does not change over the period for which calculations are performed.
Canopy Calculations
Canopy indices, such as leaf area index, are based on calculation of gap fraction, the proportion of visible sky as a function of sky direction. Leaf area index is typically calculated as the leaf area per unit ground area that would produce the observed gap fraction distribution, given an assumption of random leaf angle distribution, or a known leaf angle distribution and degree of clumping. The calculation of the LAI using this indirect Method can be very imprecise. For further explanation see leaf area index.Indices
Direct Site Factor is the proportion of direct solar radiation at a given location relative to that in the open, either integrated over time or resolved according to intervals of time of day and/or season.Indirect Site Factor is the proportion of diffuse solar radiation at a given location relative to that in the open, either integrated over time for all sky directions or resolved by sky sector direction.
Global Site Factor is the proportion of global solar radiation at a given location relative to that in the open, calculated as the sum of DSF and ISF weighted by the relative contribution of direct versus diffuse components. Sometimes this index is also called Total Side Factor.
Indices may be uncorrected or corrected for angle of incidence relative to a flat intercepting surface. Uncorrected values weight solar radiation originating from all directions equally. Corrected values weight solar radiation by the cosine of the angle of incidence, accounting for actual interception from directions normal to the intercepting surface.
Leaf Area Index is the total leaf surface area per unit ground area.
Gap Fraction is the amount in percent of canopy in relation to the whole measuring zone.
Methodology
Hemispherical photography entails five steps: photograph acquisition, digitization, registration, classification, and calculation. Registration, classification, and calculation are accomplished using dedicated hemispherical photography analysis software.Photograph acquisition
Upward-looking hemispherical photographs are typically acquired under uniform sky lighting, early or late in the day or under overcast conditions. Known orientation is essential for proper registration with the analysis hemispherical coordinate system. Even lighting is essential for accurate image classification. A self-leveling mount can facilitate acquisition by ensuring that the camera is oriented to point straight up toward the zenith. The camera is typically oriented such that north is oriented toward the top of the photograph.The lens used in hemispherical photography is generally a circular fisheye, such as the Nikkor 8mm fisheye lens. Full-frame fisheye are not suitable for hemispherical photography, as they only capture a full 180° across the diagonal, and do not provide a complete hemispherical view.
In the early years of the technique, most hemispherical photographs were acquired with 35 mm cameras using high contrast, high ASA black-and-white film. Later, use of color film or slides became common. Recently most photographs are acquired using digital cameras.
When images are acquired from locations with large differences in openness it is essential to control camera exposure. If the camera is allowed to automatically adjust exposure, the result is that small openings in closed conditions will be bright, whereas openings of the same size in open conditions will be darker. This means that during image analysis the same-sized holes will be interpreted as "sky" in a closed-canopy image and "canopy" in the open-canopy image. Without controlling exposure, the real differences between closed- and open-canopy conditions will be underestimated.