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  1. The 50-year global CO2 record led the way in establishing a scientific fact: modern civilization is changing important properties of the global atmosphere, oceans and biosphere. The evidence on which this scienti...

    Authors: Georgii A Alexandrov, Martin Heimann, Chris D Jones and Pieter Tans

    Citation: Carbon Balance and Management 2007 2:11

    Content type: Editorial

    Published on:

  2. A simulation model that relies on satellite observations of vegetation cover from the Landsat 7 sensor and from the Moderate Resolution Imaging Spectroradiometer (MODIS) was used to estimate net primary produc...

    Authors: Christopher Potter, Peggy Gross, Vanessa Genovese and Marie-Louise Smith

    Citation: Carbon Balance and Management 2007 2:9

    Content type: Research

    Published on:

  3. Tillage practices greatly affect carbon (C) stocks in agricultural soils. Quantification of the impacts of tillage on C stocks at a regional scale has been challenging because of the spatial heterogeneity of s...

    Authors: Zhengxi Tan, Shuguang Liu, Zhengpeng Li and Thomas R Loveland

    Citation: Carbon Balance and Management 2007 2:7

    Content type: Research

    Published on:

  4. Changes in the timing of phenological events may cause the annual carbon budget of deciduous forests to change. Therefore, one should take such events into account when evaluating the effects of global warming...

    Authors: Motomu Toda, Masayuki Yokozawa, Akihiro Sumida, Tsutomu Watanabe and Toshihiko Hara

    Citation: Carbon Balance and Management 2007 2:6

    Content type: Research

    Published on:

  5. Understanding the relationship between the age of a forest stand and its biomass is essential for managing the forest component of the global carbon cycle. Since biomass increases with stand age, postponing ha...

    Authors: Georgii A Alexandrov

    Citation: Carbon Balance and Management 2007 2:4

    Content type: Research

    Published on:

  6. The African continent has a large and growing role in the global carbon cycle, with potentially important climate change implications. However, the sparse observation network in and around the African continen...

    Authors: Christopher A Williams, Niall P Hanan, Jason C Neff, Robert J Scholes, Joseph A Berry, A Scott Denning and David F Baker

    Citation: Carbon Balance and Management 2007 2:3

    Content type: Review

    Published on:

  7. The repeated freeze-thaw events during cold season, freezing of soils in autumn and thawing in spring are typical for the tundra, boreal, and temperate soils. The thawing of soils during winter-summer transiti...

    Authors: Irina Kurganova, Robert Teepe and Norman Loftfield

    Citation: Carbon Balance and Management 2007 2:2

    Content type: Research

    Published on:

  8. Global carbon stocks in forest biomass are decreasing by 1.1 Gt of carbon annually, owing to continued deforestation and forest degradation. Deforestation emissions are partly offset by forest expansion and in...

    Authors: Georg E Kindermann, Michael Obersteiner, Ewald Rametsteiner and Ian McCallum

    Citation: Carbon Balance and Management 2006 1:15

    Content type: Research

    Published on:

  9. The main task is to estimate the qualitative and quantitative contribution of urban territories and precisely of the process of urbanization to the Global Carbon Cycle (GCC). Note that, on the contrary to many...

    Authors: Anastasia Svirejeva-Hopkins and Hans-Joachim Schellnhuber

    Citation: Carbon Balance and Management 2006 1:8

    Content type: Research

    Published on:

  10. Dynamic Global Vegetation Models (DGVMs) compute the terrestrial carbon balance as well as the transient spatial distribution of vegetation. We study two scenarios of moderate and strong climate change (2.9 K ...

    Authors: Wolfgang Lucht, Sibyll Schaphoff, Tim Erbrecht, Ursula Heyder and Wolfgang Cramer

    Citation: Carbon Balance and Management 2006 1:6

    Content type: Research

    Published on:

  11. Anthropogenic CO2 uptake by the ocean decreases the pH of seawater, leading to an 'acidification' which may have potential detrimental consequences on marine organisms [1]. Ocean warming or circulation alteration...

    Authors: Ben I McNeil and Richard J Matear

    Citation: Carbon Balance and Management 2006 1:2

    Content type: Research

    Published on:

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