Towards a climate-dependent paradigm of ammonia emission and deposition
Existing descriptions of bi-directional ammonia (NH3) land–atmosphere exchange incorporate temperature and moisture controls, and are beginning to be used in regional chemical transport models. However, such models have typically applied simpler emission factors to upscale the main NH3 emission term...
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Published in | Philosophical transactions of the Royal Society of London. Series B. Biological sciences Vol. 368; no. 1621; p. 20130166 |
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Main Authors | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
England
The Royal Society
05.07.2013
Royal Society, The |
Subjects | |
Online Access | Get full text |
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Summary: | Existing descriptions of bi-directional ammonia (NH3) land–atmosphere exchange incorporate temperature and moisture controls, and are beginning to be used in regional chemical transport models. However, such models have typically applied simpler emission factors to upscale the main NH3 emission terms. While this approach has successfully simulated the main spatial patterns on local to global scales, it fails to address the environment- and climate-dependence of emissions. To handle these issues, we outline the basis for a new modelling paradigm where both NH3 emissions and deposition are calculated online according to diurnal, seasonal and spatial differences in meteorology. We show how measurements reveal a strong, but complex pattern of climatic dependence, which is increasingly being characterized using ground-based NH3 monitoring and satellite observations, while advances in process-based modelling are illustrated for agricultural and natural sources, including a global application for seabird colonies. A future architecture for NH3 emission–deposition modelling is proposed that integrates the spatio-temporal interactions, and provides the necessary foundation to assess the consequences of climate change. Based on available measurements, a first empirical estimate suggests that 5°C warming would increase emissions by 42 per cent (28–67%). Together with increased anthropogenic activity, global NH3 emissions may increase from 65 (45–85) Tg N in 2008 to reach 132 (89–179) Tg by 2100. |
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Bibliography: | href:rstb20130166.pdf One contribution of 15 to a Discussion Meeting Issue ‘The global nitrogen cycle in the twenty-first century’. istex:326F85F709FD14AC7082B780C419B2268939EEE2 ark:/67375/V84-DHJ3WC7F-S ArticleID:rstb20130166 Discussion Meeting Issue 'The global nitrogen cycle in the twenty-first century' organised and edited by David Fowler, John A. Pyle, John A. Raven and Mark A. Sutton ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0962-8436 1471-2970 1471-2970 |
DOI: | 10.1098/rstb.2013.0166 |