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  • 1
    Publikationsdatum: 2009-11-17
    Beschreibung: Efforts to control climate change require the stabilization of atmospheric CO 2 concentrations. This can only be achieved through a drastic reduction of global CO 2 emissions. Yet fossil fuel emissions increased by 29% between 2000 and 2008, in conjunction with increased contributions from emerging economies, from the production and international trade of goods and services, and from the use of coal as a fuel source. In contrast, emissions from land-use changes were nearly constant. Between 1959 and 2008, 43% of each year's CO 2 emissions remained in the atmosphere on average; the rest was absorbed by carbon sinks on land and in the oceans. In the past 50 years, the fraction of CO 2 emissions that remains in the atmosphere each year has likely increased, from about 40% to 45%, and models suggest that this trend was caused by a decrease in the uptake of CO 2 by the carbon sinks in response to climate change and variability. Changes in the CO 2 sinks are highly uncertain, but they could have a significant influence on future atmospheric CO 2 levels. It is therefore crucial to reduce the uncertainties. © 2009 Macmillan Publishers Limited. All rights reserved.
    Print ISSN: 1752-0894
    Digitale ISSN: 1752-0908
    Thema: Geologie und Paläontologie
    Publiziert von Springer Nature
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2009-08-30
    Beschreibung: As particulate organic carbon rains down from the surface ocean it is respired back to carbon dioxide and released into the oceans interior. The depth at which this sinking carbon is converted back to carbon dioxideknown as the remineralization depthdepends on the balance between particle sinking speeds and their rate of decay. A host of climate-sensitive factors can affect this balance, including temperature, oxygen concentration, stratification, community composition and the mineral content of the sinking particles. Here we use a three-dimensional global ocean biogeochemistry model to show that a modest change in remineralization depth can have a substantial impact on atmospheric carbon dioxide concentrations. For example, when the depth at which 63% of sinking carbon is respired increases by 24 m globally, atmospheric carbon dioxide concentrations fall by 10-27 ppm. This reduction in atmospheric carbon dioxide concentration results from the redistribution of remineralized carbon from intermediate waters to bottom waters. As a consequence of the reduced concentration of respired carbon in upper ocean waters, atmospheric carbon dioxide is preferentially stored in newly formed North Atlantic Deep Water. We suggest that atmospheric carbon dioxide concentrations are highly sensitive to the potential changes in remineralization depth that may be caused by climate change. © 2009 Macmillan Publishers Limited. All rights reserved.
    Print ISSN: 1752-0894
    Digitale ISSN: 1752-0908
    Thema: Geologie und Paläontologie
    Publiziert von Springer Nature
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
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