2004
DOI: 10.1016/j.atmosenv.2004.04.008
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A temporally and spatially resolved ammonia emission inventory for dairy cows in the United States

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Cited by 75 publications
(62 citation statements)
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“…The seasonal variation of anthropogenic emissions is important for many compounds (e.g. ammonia) especially for those for which the phase partitioning is temperature dependent (Pinder et al, 2004;De Meij et al, 2006). In this work, we take advantage of the stateof-the-art emissions inventory EDGAR-Climate Change and Impact Research (CIRCE), which provides emissions on a high spatial (0.1 × 0.1 • ) and temporal (monthly) resolution, together with a recently developed aerosol scheme implemented within the EMAC model (Pringle et al, 2010a).…”
Section: A Pozzer Et Al: Aerosol Simulation With Emacmentioning
confidence: 99%
“…The seasonal variation of anthropogenic emissions is important for many compounds (e.g. ammonia) especially for those for which the phase partitioning is temperature dependent (Pinder et al, 2004;De Meij et al, 2006). In this work, we take advantage of the stateof-the-art emissions inventory EDGAR-Climate Change and Impact Research (CIRCE), which provides emissions on a high spatial (0.1 × 0.1 • ) and temporal (monthly) resolution, together with a recently developed aerosol scheme implemented within the EMAC model (Pringle et al, 2010a).…”
Section: A Pozzer Et Al: Aerosol Simulation With Emacmentioning
confidence: 99%
“…The majority of urinary N is in the form of urea, which is hydrolysed by faecal urease to NH 3 . About 25% of dairy manure N is lost as NH 3 under current US practices (Pinder et al, 2004), contributing to the total annual NH 3 re-deposition rates of 23 to 40 kg of N per ha (Burkart and James, 1999). Studies that compared crop and livestock production indicated that the efficiency of N use for cereal production was 54%, whereas in the dairy system the efficiency of N use was only 28% (Domburg et al, 2000).…”
Section: Introductionmentioning
confidence: 99%
“…Secondary particles are largely composed of sulfate, nitrate, ammonium and secondary organic aerosols (SOA). The inorganic secondary aerosols are formed in the atmosphere from the oxidation of gas-phase precursors such as sulfur dioxide (SO 2 ) (Seinfeld and Pandis, 1998), nitric oxide (NO) and nitrogen oxides (NO x ) (Pinder et al, 2004). By comparison, SOA formation mechanisms have not been fully understood.…”
Section: Introductionmentioning
confidence: 99%