Seasonal variability of sea surface carbonate chemistry and temperature

Seasonal variability of sea surface carbonate chemistry and temperature

Ocean uptake of anthropogenic CO2 causes ocean acidification, a secular, global-scale decline in the pH of seawater. In order to better understand the implications of contemporary acidification for marine organisms and ecosystems, there is a need to better characterise natural variability in carbo...

Full description

Bibliographic Details
Main Author: Matthews, John Brian Robin
Other Authors: Weaver, Andrew J.
Language:English
en
Published: 2013
Subjects:
Ocean acidification
Sea surface temperature
Carbonate chemistry
Sea surface pH
Marine chemistry
Ocean time-series
Total alkalinity
Aragonite saturation state
Engine intake temperature
Bucket temperature
Online Access:http://hdl.handle.net/1828/5104
Matthews, J. B. R. (2013). Comparing historical and modern methods of sea surface temperature measurement - Part 1: Review of methods, field comparisons and dataset adjustments, Ocean Science, 9(4):683-694. Available from: http://dx.doi.org/10.5194/os-9-683-2013.
Matthews, J. B. R. and Matthews, J. B. (2013). Comparing historical and modern methods of sea surface temperature measurement - Part 2: Field comparison in the central tropical Pacific, Ocean Science, 9(4):695-711. Available from: http://dx.doi.org/10.5194/os-9-695-2013.

Internet

http://hdl.handle.net/1828/5104
Matthews, J. B. R. (2013). Comparing historical and modern methods of sea surface temperature measurement - Part 1: Review of methods, field comparisons and dataset adjustments, Ocean Science, 9(4):683-694. Available from: http://dx.doi.org/10.5194/os-9-683-2013.
Matthews, J. B. R. and Matthews, J. B. (2013). Comparing historical and modern methods of sea surface temperature measurement - Part 2: Field comparison in the central tropical Pacific, Ocean Science, 9(4):695-711. Available from: http://dx.doi.org/10.5194/os-9-695-2013.

Similar Items