PLAN341 Lecture Notes - Lecture 23: Landscape Architecture, Cloud Condensation Nuclei, Hygroscopy

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Variation in solar heating related to slope and surface conditions. Eee at a particular wavelength (in vacuum) has an associated frequency (f) and photon energy (e: related according to equation c = frequency x wave length. C is speed of light, h is planck"s constant. Electromagnetic radiation: classified by frequency of wave. Radio, micro, terahertz, infrared, visible light, uv radiation, x-ray, Solar radiation gamma rays: radiant energy emitted by the sun, consists of visible short-wave, the near infrared and the ultraviolet part of. Solar constant: amount of incoming solar radiation per unit area, measured on outer surface of atmosphere, in a plane perpendicular to rays, includes all types, not just visible light, measured by satellite, sun"s power is 1. 740x10^17w. Variation in radiation intensity: relationship with sun angle and curvature of earth. Dependant on the angle of the sun influenced by distance of travel through atmosphere. Seasonal change in sun angle relationship between 23. 5-degree tilt of earth influence temperature patterns.

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