Methane and Global Environmental Change

Author:

Reay Dave S.1,Smith Pete2,Christensen Torben R.34,James Rachael H.5,Clark Harry6

Affiliation:

1. School of GeoSciences, University of Edinburgh, Edinburgh EH8 9XP, United Kingdom;

2. Institute of Biological and Environmental Sciences, School of Biological Sciences, University of Aberdeen, Aberdeen AB24 3UU, United Kingdom;

3. Department of Bioscience, Aarhus University, 4000 Roskilde, Denmark

4. Department of Physical Geography and Ecosystem Science, Lund University, 221 00 Lund, Sweden;

5. Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton SO17 1BJ, United Kingdom;

6. Grasslands Research Centre, New Zealand Agricultural Greenhouse Gas Research Centre, Palmerston North 4442, New Zealand;

Abstract

Global atmospheric methane concentrations have continued to rise in recent years, having already more than doubled since the Industrial Revolution. Further environmental change, especially climate change, in the twenty-first century has the potential to radically alter global methane fluxes. Importantly, changes in temperature, precipitation, and net primary production may induce positive climate feedback effects in dominant natural methane sources such as wetlands, soils, and aquatic ecosystems. Anthropogenic methane sources may also be impacted, with a risk of enhanced emissions from the energy, agriculture, and waste sectors. Here, we review the global sources of methane, the trends in fluxes by source and sector, and their possible evolution in response to future environmental change. We discuss ongoing uncertainties in flux estimation and projection, and highlight the great potential for multisector methane mitigation as part of wider global climate change policy.

Publisher

Annual Reviews

Subject

General Environmental Science

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