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Nitrous oxide and methane in a changing Arctic Ocean
- Source :
- Ambio
- Publication Year :
- 2021
- Publisher :
- Springer Science and Business Media LLC, 2021.
-
Abstract
- Human activities are changing the Arctic environment at an unprecedented rate resulting in rapid warming, freshening, sea ice retreat and ocean acidification of the Arctic Ocean. Trace gases such as nitrous oxide (N2O) and methane (CH4) play important roles in both the atmospheric reactivity and radiative budget of the Arctic and thus have a high potential to influence the region’s climate. However, little is known about how these rapid physical and chemical changes will impact the emissions of major climate-relevant trace gases from the Arctic Ocean. The combined consequences of these stressors present a complex combination of environmental changes which might impact on trace gas production and their subsequent release to the Arctic atmosphere. Here we present our current understanding of nitrous oxide and methane cycling in the Arctic Ocean and its relevance for regional and global atmosphere and climate and offer our thoughts on how this might change over coming decades. Supplementary Information The online version contains supplementary material available at 10.1007/s13280-021-01633-8.
- Subjects :
- 0106 biological sciences
010504 meteorology & atmospheric sciences
Environmental change
Oceans and Seas
Earth science
Geography, Planning and Development
01 natural sciences
Methane
Atmosphere
chemistry.chemical_compound
Arctic Ocean
Sea ice
Ice retreat
Humans
Environmental Chemistry
Seawater
0105 earth and related environmental sciences
geography
Nitrous oxide
geography.geographical_feature_category
Ecology
Arctic Regions
Ocean acidification
010604 marine biology & hydrobiology
General Medicine
Hydrogen-Ion Concentration
Trace gas
chemistry
Arctic
13. Climate action
Environmental science
Changing Arctic Ocean
Warming
Subjects
Details
- ISSN :
- 16547209 and 00447447
- Volume :
- 51
- Database :
- OpenAIRE
- Journal :
- Ambio
- Accession number :
- edsair.doi.dedup.....463f36277409739beb78c59902433926