Ozone - the persistent menace: interactions with the N cycle and climate change
(2014) In Current Opinion in Environmental Sustainability 9–10. p.9-19- Abstract
- Tropospheric ozone is involved in a complex web of interactions with other atmospheric gases and particles, and through ecosystem interactions with the N-cycle and climate change. Ozone itself is a greenhouse gas, causing warming, and reductions in biomass and carbon sequestration caused by ozone provide a further indirect warming effect. Ozone also has cooling effects, however, for example, through impacts on aerosols and diffuse radiation. Ecosystems are both a source of ozone precursors (especially of hydrocarbons, but also nitrogen oxides), and a sink through deposition processes. The interactions with vegetation, atmospheric chemistry and aerosols are complex, and only partially understood. Levels and patterns of global exposure to... (More)
- Tropospheric ozone is involved in a complex web of interactions with other atmospheric gases and particles, and through ecosystem interactions with the N-cycle and climate change. Ozone itself is a greenhouse gas, causing warming, and reductions in biomass and carbon sequestration caused by ozone provide a further indirect warming effect. Ozone also has cooling effects, however, for example, through impacts on aerosols and diffuse radiation. Ecosystems are both a source of ozone precursors (especially of hydrocarbons, but also nitrogen oxides), and a sink through deposition processes. The interactions with vegetation, atmospheric chemistry and aerosols are complex, and only partially understood. Levels and patterns of global exposure to ozone may change dramatically over the next 50 years, impacting global warming, air quality, global food production and ecosystem function. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/4862814
- author
- Simpson, David ; Arneth, Almut LU ; Mills, Gina ; Solberg, Sverre and Uddling, Johan
- publishing date
- 2014
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Current Opinion in Environmental Sustainability
- volume
- 9–10
- pages
- 9 - 19
- publisher
- Elsevier
- external identifiers
-
- scopus:84905511437
- ISSN
- 1877-3443
- DOI
- 10.1016/j.cosust.2014.07.008
- language
- English
- LU publication?
- no
- id
- df64651c-093a-48cf-b7ba-93a7cc6baf71 (old id 4862814)
- date added to LUP
- 2016-04-01 10:32:52
- date last changed
- 2022-04-27 23:09:48
@article{df64651c-093a-48cf-b7ba-93a7cc6baf71,
abstract = {{Tropospheric ozone is involved in a complex web of interactions with other atmospheric gases and particles, and through ecosystem interactions with the N-cycle and climate change. Ozone itself is a greenhouse gas, causing warming, and reductions in biomass and carbon sequestration caused by ozone provide a further indirect warming effect. Ozone also has cooling effects, however, for example, through impacts on aerosols and diffuse radiation. Ecosystems are both a source of ozone precursors (especially of hydrocarbons, but also nitrogen oxides), and a sink through deposition processes. The interactions with vegetation, atmospheric chemistry and aerosols are complex, and only partially understood. Levels and patterns of global exposure to ozone may change dramatically over the next 50 years, impacting global warming, air quality, global food production and ecosystem function.}},
author = {{Simpson, David and Arneth, Almut and Mills, Gina and Solberg, Sverre and Uddling, Johan}},
issn = {{1877-3443}},
language = {{eng}},
pages = {{9--19}},
publisher = {{Elsevier}},
series = {{Current Opinion in Environmental Sustainability}},
title = {{Ozone - the persistent menace: interactions with the N cycle and climate change}},
url = {{http://dx.doi.org/10.1016/j.cosust.2014.07.008}},
doi = {{10.1016/j.cosust.2014.07.008}},
volume = {{9–10}},
year = {{2014}},
}