Designing and building hi-fi furniture by Jeff Markell

By Jeff Markell

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E. carbon taken up by photosynthesis minus carbon lost during plant respiration. , the photic zone, because water strongly absorbs sunlight. The photic zone rarely extends more than 200m. Microscopic phytoplankton drives the biological cycle in the photic zone and deeper in the oceans. They take their CO 2 from that dissolved in the seawater around them. The phytoplankton are grazed by zooplankton that package most of their fast products into faecal pellets, which in return are consumed and decomposed by other organisms.

3 Different expressions exist in literature concerning this feedback process: ice-albedo feedback and snow-climate feedback .. , due to a lower value of the solar constant, the average snow- and ice cover increases, reflecting more of the solar radiation and reducing the absorption of solar radiation and, hence, decreasing the effective radiating temperature. This creates a positive feedback whenever the lower radiating temperature also implies a lower surface temperature4 . , a temperature decrease in a completely ice-covered planet is not enhanced by the albedo-temperature feedback.

2. 15). The albedo of clouds strongly varies with latitude because the albedo of liquid water strongly increases with a decreasing solar elevation. e. the path of a sunray in a cloud. In this respect also the amount of liquid water and the amount of ice-crystals in a cloud are important. Ice-crystals are formed at very low temperature and, hence, depend on the altitude of the cloud. Also the downward backradiation varies with the cloud-level because long-wave radiation emitted by clouds depends on temperature.

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