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Publikováno v:
Biogeosciences, Vol 14, Iss 4, Pp 781-797 (2017)
Dissolved oxygen (DO) concentration in the ocean is an important component of marine biogeochemical cycles and will be greatly altered as climate change persists. In this study a global oceanic carbon cycle model (HAMOCC 2.0) is used to address how m
Publikováno v:
Biogeosciences; 2017, Vol. 14 Issue 4, p781-797, 17p, 2 Charts, 7 Graphs, 4 Maps