Titlebook: Geoengineering Responses to Climate Change; Selected Entries fro Tim Lenton,Naomi Vaughan Book 2013 Springer Science+Business Media New Yor

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Die Krise des fordistischen Modells,ntended to be mixed with soils. If the solid remains are not suitable for addition to soils, or will be burned as a fuel or used as an aggregate in construction, it is defined as char not biochar. There is a very wide range of potential biochar feedstocks, e.g., wood waste, timber, agricultural resi

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Die Neuordnung des Journalismus CO. is converted to bicarbonate in solution. Research in this field is still focused on increasing the rate of reaction, but the required additional technologies add considerably to the cost of the process. In this entry, the focus is on the optimization of the weathering conditions, by selecting t

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https://doi.org/10.1007/978-3-7091-2191-7ly emerged as a novel and controversial issue in climate governance. It is sometimes proposed as an insurance policy, should either (a) primary efforts to develop sustainable energy and societal systems prove unable to quickly enough overcome the inertia of current ones, or (b) uncertainty in the cl

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Introduction, by decreasing the amount of sunlight absorbed at the Earth’s surface. The technologies discussed are commonly grouped under the term “geoengineering,” defined in a 2009 report by the Royal Society as the “deliberate large-scale manipulation of the planetary environment to counteract anthropogenic c

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Sunshades for Solar Radiation Management,nfluences on the climate system (IPCC 2007). Attempts to curb human emissions of greenhouse gases have so far largely failed; as such, and in an attempt to avoid or delay potential dangerous climate change, several geoengineering schemes have been suggested for modifying Earth’s climate directly. On

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Stratospheric Aerosols for Solar Radiation Management,surface, thereby cooling the surface and counteracting some of the warming from anthropogenic greenhouse gases. The way this is accomplished depends on the specific aerosol used, but the basic mechanism involves backscattering and absorbing certain amounts of solar radiation aloft. Since warming fro

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Ocean Fertilization for Sequestration of Carbon Dioxide from the Atmosphere,ility and biological pump, respectively Fig.5.1) are responsible for the majority of carbon sequestration in the ocean’s interior [1]. The solubility pump relies on ocean circulation – specifically the impact of cooling of the upper ocean at high latitudes both enhances the solubility of carbon diox