32 research outputs found
Carbon-nitrogen interactions in European forests and semi-natural vegetation - Part 1: Fluxes and budgets of carbon, nitrogen and greenhouse gases from ecosystem monitoring and modelling
The impact of atmospheric reactive nitrogen (N) deposition on carbon (C) sequestration in soils and biomass of unfertilized, natural, semi-natural and forest ecosystems has been much debated. Many previous results of this dC/dN response were based on changes in carbon stocks from periodical soil and ecosystem inventories, associated with estimates of N deposition obtained from large-scale chemical transport models. This study and a companion paper (Flechard et al., 2020) strive to reduce uncertainties of N effects on C sequestration by linking multi-annual gross and net ecosystem productivity estimates from 40 eddy covariance flux towers across Europe to local measurement-based estimates of dry and wet N deposition from a dedicated collocated monitoring network. To identify possible ecological drivers and processes affecting the interplay between C and N inputs and losses, these data were also combined with in situ flux measurements of NO, NO and CH fluxes; soil NO̅ leaching sampling; and results of soil incubation experiments for N and greenhouse gas (GHG) emissions, as well as surveys of available data from online databases and from the literature, together with forest ecosystem (BASFOR) modelling. Multi-year averages of net ecosystem productivity (NEP) in forests ranged from -70 to 826 gCm yr at total wet+dry inorganic N deposition rates (N) of 0.3 to 4.3 gNm yr and from -4 to 361 g Cm yr at N rates of 0.1 to 3.1 gNm yr in short semi-natural vegetation (moorlands, wetlands and unfertilized extensively managed grasslands). The GHG budgets of the forests were strongly dominated by CO exchange, while CH and NO exchange comprised a larger proportion of the GHG balance in short semi-natural vegetation. Uncertainties in elemental budgets were much larger for nitrogen than carbon, especially at sites with elevated N where N leaching losses were also very large, and compounded by the lack of reliable data on organic nitrogen and N losses by denitrification. Nitrogen losses in the form of NO, NO and especially NO̅ were on average 27%(range 6 %–54 %) of N at sites with N 3 gNm yr. Such large levels of N loss likely indicate that different stages of N saturation occurred at a number of sites. The joint analysis of the C and N budgets provided further hints that N saturation could be detected in altered patterns of forest growth. Net ecosystem productivity increased with N deposition up to 2–2.5 gNm yr, with large scatter associated with a wide range in carbon sequestration efficiency (CSE, defined as the NEP = GPP ratio). At elevated N levels (> 2.5 gNm yr), where inorganic N losses were also increasingly large, NEP levelled off and then decreased. The apparent increase in NEP at low to intermediate N levels was partly the result of geographical cross-correlations between N and climate, indicating that the actual mean dC/dN response at individual sites was significantly lower than would be suggested by a simple, straightforward regression of NEP vs. N
The quality of European (EU-15) greenhouse gas inventories from agriculture
The European Community is the only regional economic integration organization that has joined the United Nations Framework Convention on Climate Change (UNFCCC) as a party. The EU-15 has committed itself to report annually on greenhouse gas inventories within the area covered by its EU-15 Member States. The quality of the EC-inventory depends strongly on the quality of the national greenhouse gas inventories, including the comparability of the methodologies used and the definitions applied. This paper reviews the actual quality of the national inventory reports of the EU-15 Member States submitted in 2005 and the resulting quality of the EU-inventory, focusing on the sector `agriculture¿ of the Common Reporting Format. For this sector, a workshop to improve inventory quality was organized at the Joint Research Centre (European Commission). The most uncertain source category in the majority of greenhouse gas inventories is N2O emissions from agricultural soils. Even though the body of information on factors influencing the magnitude of this emission source is already considerable, well designed experimental studies, particularly in southern and eastern European climate regions are needed. Still, it will be unlikely that measurement programmes alone will be sufficient to reduce the uncertainty in this source category. Rather the use of process based models will have to play a role in the future in the inventory process for estimating N2O emissions directly or in the frame of a broader modelling framework that ensures a holistic view of the impact of agriculture on the environmen