<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>The greenhouse gas balance of European grasslands</dc:title>
  <dc:creator>Chang, J. F.</dc:creator>
  <dc:creator>Ciais, P.</dc:creator>
  <dc:creator>Viovy, N.</dc:creator>
  <dc:creator>Vuichard, N.</dc:creator>
  <dc:creator>/Sultan, Benjamin</dc:creator>
  <dc:creator>Soussana, J. F.</dc:creator>
  <dc:subject>European grassland</dc:subject>
  <dc:subject>grassland management</dc:subject>
  <dc:subject>greenhouse gases balance</dc:subject>
  <dc:subject>livestock</dc:subject>
  <dc:subject>ORCHIDEE</dc:subject>
  <dc:description>The greenhouse gas (GHG) balance of European grasslands (EU-28 plus Norway and Switzerland), including CO2, CH4 and N2O, is estimated using the new process-based biogeochemical model ORCHIDEE-GM over the period 1961-2010. The model includes the following: (1) a mechanistic representation of the spatial distribution of management practice; (2) management intensity, going from intensively to extensively managed; (3) gridded simulation of the carbon balance at ecosystem and farm scale; and (4) gridded simulation of N2O and CH4 emissions by fertilized grassland soils and livestock. The external drivers of the model are changing animal numbers, nitrogen fertilization and deposition, land-use change, and variable CO2 and climate. The carbon balance of European grassland (NBP) is estimated to be a net sink of 15 +/- 7gCm(-2)year(-1) during 1961-2010, equivalent to a 50-year continental cumulative soil carbon sequestration of 1.0 +/- 0.4PgC. At the farm scale, which includes both ecosystem CO2 fluxes and CO2 emissions from the digestion of harvested forage, the net C balance is roughly halved, down to a small sink, or nearly neutral flux of 8gCm(-2)year(-1). Adding CH4 and N2O emissions to net ecosystem exchange to define the ecosystem-scale GHG balance, we found that grasslands remain a net GHG sink of 19 +/- 10g C-CO2 equiv. m(-2)year(-1), because the CO2 sink offsets N2O and grazing animal CH4 emissions. However, when considering the farm scale, the GHG balance (NGB) becomes a net GHG source of -50gC-CO2 equiv. m(-2)year(-1). ORCHIDEE-GM simulated an increase in European grassland NBP during the last five decades. This enhanced NBP reflects the combination of a positive trend of net primary production due to CO2, climate and nitrogen fertilization and the diminishing requirement for grass forage due to the Europe-wide reduction in livestock numbers.</dc:description>
  <dc:date>2015</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010065272</dc:identifier>
  <dc:identifier>fdi:010065272</dc:identifier>
  <dc:identifier>Chang J. F., Ciais P., Viovy N., Vuichard N., Sultan Benjamin, Soussana J. F.. The greenhouse gas balance of European grasslands. 2015, 21 (10),  3748-3761</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>EUROPE</dc:coverage>
</oai_dc:dc>
