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EUA future prices 2005–2011
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Variations in topsoil organic carbon content across Europe
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The map shows the percentage of organic carbon content in the surface horizon of soils in Europe.
The darker regions correspond to soils with high values of organic carbon. The darkest colours, especially in Estonia, Fennoscandinavia, Ireland and the United Kingdom, denote peatlands.
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Projected changes in soil organic carbon for cropland 1990-2080
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Predicted changes in soil organic carbon for croplands 1990–2080. The image on the left shows changes due to climate change only while the map on the right shows changes as a result of variations in net primary production and the advent of new technologies related to crop management (e.g. machinery, pesticides, herbicides, agronomic knowledge of farmers) and breeding (development of higher yielding varieties through improved stress resistance and/or yield potential) that result in yield increases.
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Changes in soil organic carbon content across England and Wales between 1978 and 2003
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The map shows the difference in soil organic carbon content
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Traffic related toxics (2004): Distance to target for lead and carbon monoxide at urban and traffic stations
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The limit value is shown as a bold line, with observed concentrations as columns
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Evolution of carbon in above- and below-ground woody biomass
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Reference Waterbase - Monitoring stations for rivers and lakes
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Water quality monitoring stations in rivers and lakes
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Reference Waterbase - Monitoring stations for rivers and lakes
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Water quality monitoring stations in rivers and lakes
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Inter-annual variation in European carbon fluxes from the biosphere to the atmosphere
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Note: The lines represent the results of two ecosystem models (LPJ and SLAVE), and the range (minimum, mean, maximum) of calculated terrestrial C flux (based on so-called inversed calculations considering atmospheric CO2 calculation)
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Carbon balance of the terrestrial biosphere
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Notes: Atmospheric carbon (in the form of CO2) is absorbed by plants in the process of photosynthesis
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