Ocean-atmosphere trace gas exchange. Chem. Soc. Rev. 41, 6473-506.Carpenter, L. J., S. D. Archer, and R. Beale. 2012. Ocean-atmosphere trace gas exchange. Chem. Soc. Rev. 41:6473-6506.CARPENTER L J, ARCHER S D, BEALE R. Ocean-atmosphere trace gas exchange [ J ]. Chemical ...
Ocean-atmosphere trace gas exchange. Chem. Soc. Rev. 41, 6473-506 (2012).Carpenter, L.J., Archer, S.D., and Beale, R.: Ocean-atmosphere trace gas exchange, Chem. Soc. Rev., 41, 6473-6506, doi:10.1039/C2CS35121H, 2012.
Ocean–atmosphere trace gas exchange. Chem. Soc. Rev. 41, 6473–6506 (2012). Article CAS PubMed Google Scholar Franklin, D. J., Steinke, M., Young, J., Probert, I. & Malin, G. Dimethylsulphoniopropionate (DMSP), DMSP-lyase activity (DLA) and dimethylsulphide (DMS) in 10 species...
摘要: The two-way exchange of trace gases between the ocean and the atmosphere is important for both the chemistry and physics of the atmosphere and the biogeochemistry of the oceans, including the global...关键词: Meereskunde DOI: 10.1007/978-3-642-25643-1_1 ...
The CO 2 that remains in the atmosphere acts as a greenhouse gas, absorbing long-wavelength radiation (heat) in the atmosphere. CO 2 taken up by the oceans does not affect the Earth's heat balance, so an understanding of the air-sea exchange of CO 2 is an essential part of ...
2012. Ocean-atmosphere trace gas exchange. Chem Soc Rev, 41: 6473–6506 Google Scholar Cha I T, Min U G, Kim S J, Yim K J, Roh S W, Rhee S K. 2013. Methanomethylovorans uponensis sp. nov., a methylotrophic methanogen isolated from wetland sediment. Antonie van Leeuwenhoek, ...
2014, Ocean-Atmosphere Interactions of Gases and Particles Ocean-atmosphere trace gas exchange 2012, Chemical Society Reviews Methane production in aerobic oligotrophic surface water in the central Arctic Ocean 2010, Biogeosciences View all citing articles on Scopus1 Current address: School of Environmental...
Modeling the behavior of trace elements during lunar magma ocean solidification is important to further our understanding of the chemical evolution of the
Influence of the surface microlayer on the flux of nonconservative trace gases (CO, H2, CH4, N2O) across the ocean-atmosphere interface Conrad, R., and W. Seiler (1988), Influence of the surface microlayer on the flux of nonconservative trace gases (CO, H2, CH4, N2O) across the ......
(6)] essentially enables the storage of carbon in the ocean at a level significantly greater than that possible if CO2were an inert gas. The upper 100m ocean is well-mixed and exchanges directly with the atmosphere on time scales of a year. Hence, the effectiveness of the ocean as a ...