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The Royal Society, Philosophical Transactions of the Royal Society B: Biological Sciences, 1621(368), p. 20130166, 2013

DOI: 10.1098/rstb.2013.0166

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Towards a climate-dependent paradigm of ammonia emission and deposition

Journal article published in 2013 by John R. Walker, John T. Walker, Mark A. Sutton, Stefan Reis, Stuart N. Riddick, Wim de Vries, Ulrike Dragosits, Eiko Nemitz, Mark Richard Theobald, Y. Sim Tang, Sarah Wanless, Yi Sim Tang ORCID, Robert F. Mitchell, Christine F. Braban, Francis Daunt and other authors.
This paper is made freely available by the publisher.
This paper is made freely available by the publisher.

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Abstract

Existing descriptions of bi-directional ammonia (NH 3 ) 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 NH 3 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 NH 3 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 NH 3 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 NH 3 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 NH 3 emissions may increase from 65 (45–85) Tg N in 2008 to reach 132 (89–179) Tg by 2100.