Abstract
There is growing interest in better understanding the biogeochemistry of the world oceans, largely because of the rapid increase of atmospheric carbon dioxide, CO2, and the anticipated consequences for the oceans as well as the atmosphere. Interestingly, measurements are presently showing increasing levels of CO2 in the surface layers of the ocean in relatively pristine areas, namely at the Joint Global Ocean Flux Study (JGOFS) time series sites off Hawaii and Bermuda (e.g., Karl et al., 2001). Suggested effects of rising levels of CO2 include increases in global atmospheric and oceanic temperature, shifts in weather patterns causing regional droughts and flooding, melting of ice caps, sea level rise, and changes in ocean ecology and population dynamics that may affect fisheries. A fundamental scientific, societal, and political issue concerns the partitioning of the causes of these phenomena between natural variability versus anthropogenic influences.
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Dickey, T.D. (2004). Exploration of Biogeochemical Temporal Variability. In: Follows, M., Oguz, T. (eds) The Ocean Carbon Cycle and Climate. NATO Science Series, vol 40. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-2087-2_5
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DOI: https://doi.org/10.1007/978-1-4020-2087-2_5
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