Quantifying the influence of CO<sub>2</sub> seasonality on future aragonite undersaturation onset
Ocean acidification is a predictable consequence of rising atmospheric carbon dioxide (CO<sub>2</sub>), and is highly likely to impact the entire marine ecosystem – from plankton at the base of the food chain to fish at the top. Factors which are expected to be impacted include reproduct...
Main Authors: | T. P. Sasse, B. I. McNeil, R. J. Matear, A. Lenton |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2015-10-01
|
Series: | Biogeosciences |
Online Access: | http://www.biogeosciences.net/12/6017/2015/bg-12-6017-2015.pdf |
Similar Items
-
Carbonate saturation state of surface waters in the Ross Sea and Southern Ocean: controls and implications for the onset of aragonite undersaturation
by: H. B. DeJong, et al.
Published: (2015-12-01) -
Dissolution dominating calcification process in polar pteropods close to the point of aragonite undersaturation.
by: Nina Bednaršek, et al.
Published: (2014-01-01) -
Baseline monitoring of the western Arctic Ocean estimates 20% of Canadian basin surface waters are undersaturated with respect to aragonite.
by: Lisa L Robbins, et al.
Published: (2013-01-01) -
The non-steady state oceanic CO<sub>2</sub> signal: its importance, magnitude and a novel way to detect it
by: B. I. McNeil, et al.
Published: (2013-04-01) -
Quantifying the impact of ocean acidification on our future climate
by: R. J. Matear, et al.
Published: (2014-07-01)