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UNITED NATIONS FRAMEWORK CONVENTION ON CLIMATE CHANGE (UNFCCC)
Abstract
If the thermohaline slows, it will reduce the rate of mixing of the ocean waters. This will tend to isolate the surface ocean (where the phytoplankton resides) from the deep ocean (where most of the nutrients are found). It will mean a reduction in oxygen supply to the deep oceans, which would eventually become anoxic (depleted of oxygen). The result of this stratification process would not only be to kill off many deep ocean aerobic marine species but also to promote anaerobic organisms, such as sulphate reducers, that produce hydrogen sulfide as a waste product. This, in turn, would deplete soluble iron, which is an important nutrient source for phytoplankton and could serve to reduce biological activity and primary production.
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Cited by
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Energy system transformations for limiting end-of-century warming to below 1.5 °C
Rogelj, J., Luderer, G., Pietzcker, R. C., Kriegler, E., Schaeffer, M., Krey, V., & Riahi, K. (2015) · Nature Climate Change · doi:10.1038/nclimate2572 · Cited by 875
The Science of Adaptation: A Framework for Assessment
Smit, B., Burton, I., Klein, R. J. T., & Street, R. (1999) · Mitigation and Adaptation Strategies for Global Change · doi:10.1023/a:1009652531101 · Cited by 561
Will China peak its energy-related carbon emissions by 2030? Lessons from 30 Chinese provinces
Fang, K., Tang, Y., Zhang, Q., Song, J., Wen, Q., Sun, H., Ji, C., & Xu, A. (2019) · Applied Energy · doi:10.1016/j.apenergy.2019.113852 · Cited by 298
Pokorny, B., Scholz, I., & de Jong, W. (2013) · Ecology and Society · doi:10.5751/es-05458-180203 · Cited by 125
Metadata
- Venue
- The Complete Guide to Climate Change
- Publisher
- Routledge
- Published
- 2008-11-28
- Pages
- 392-403
- OpenAlex
- W2949513949
- Cited by
- 1,322
- References
- 0
- FWCI
- 69.05
- Type
- book chapter
- Language
- en
- Open access
- closed
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