Authors: S. T. Wilson, A. N. Al-Haj, A. Bourbonnais, C. Frey, R. W. Fulweiler, J. D. Kessler, H. K. Marchant, J. Milucka, N. E. Ray, P. Suntharalingham, B. F. Thornton, R. C. Upstill-Goddard, T. S. Weber, D. L. Arévalo-Martínez, H. W. Bange, H. M. Benway, D. Bianchi, A. V. Borges, B. X. Chang, P. M. Crill, D. A. del Valle, L. Farías, S. B. Joye, A. Kock, J. Labidi, C. C. Manning, J. W. Pohlman, G. Rehder, K. J. Sparrow, P. D. Tortell, T. Treude, D. L. Valentine, B. B. Ward, S. Yang, L. N. Yurganov
Venue: N/A
Type: Publication
Abstract: In the current era of rapid climate change, accurate characterization of climate-relevant gas dynamics – namely production, consumption, and net emissions – is required for all biomes, especially those ecosystems most susceptible to the impact of change. Marine environments include regions that act as net sources or sinks for numerous climate-active trace gases including methane (CH4) and nitrous oxide (N2O). The temporal and spatial distributions of CH4 and N2O are controlled by the interaction of complex biogeochemical and physical proces...
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Topics: 
Environmental resource management
Earth science
Oceanography
DOI:
10.5194/bg-2020-270
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