Cost - effective
Control of Acidification and Ground - Level Ozone.
Not exact matches
Five cultures each were kept under
control conditions (15 °C) and at elevated water temperature (26 °C) in combination with three different concentrations
of carbon dioxide (CO2): a
control value with today's conditions, the conditions
of the Intergovernmental Panel on Climate Change's «worst case scenario» and the highest possible degree
of acidification.
Now, scientists have suggested that corals have some active
control over their skeletal growth — and that it may protect them from the worst ravages
of ocean
acidification.
For the study, five cultures were kept under a constant temperature and three different concentrations
of carbon dioxide (CO2): a
control value with today's conditions, the conditions that could be reached until the end
of this century according to the most critical calculations
of the Intergovernmental Panel on Climate Change (IPCC), and the highest possible degree
of acidification.
Geoengineering methods that don't remove carbon dioxide from the atmosphere don't undo the other effects
of high atmosphere carbon - dioxide concentrations such as ocean
acidification, and our ability to adequately
control geoengineering with sunlight - reflecting particles is not certain.
You can have a differential impact on biology and chemistry, so if you really want to assess what will be the status
of calcifying organisms in 2100 there is one part, the chemistry, for which the organisms have no
control but for the biology they can perhaps adapt and there might be a way for the organisms to mitigate the negative impacts
of ocean
acidification.
Since you state that a decrease in net calcification could result from a decrease in gross calcification, an increase in dissolution rates, or both, you distinguish between these responses and get to the conclusion that the impact
of ocean
acidification on a creature's net calcification may be largely
controlled by the status
of its protective organic cover and that the net slowdown in skeletal growth under increased CO2 occurs not because these organisms are unable to calcify, but rather because their unprotected skeleton is dissolving faster.
Key elements include curbing human carbon dioxide emissions to the atmosphere, improved
control of local pollution sources, reducing coastal habitat destruction, and better preparing coastal human communities to withstand the amount
of ocean
acidification and climate change that is unavoidable.
The Environmental Protection Agency is investigating whether it can use the Clean Water Act to
control greenhouse gas emissions because
of ocean
acidification.
Elsewhere researchers concluded that in addition to atmospheric pH, the complex interactions
controlling pH especially in coastal zones, make detection
of any trends towards
acidification «not trivial and the attribution
of these changes to anthropogenic CO2 emissions is even more problematic.»
Furthermore, by working in
controlled areas
of a natural reef community, Caldeira, Albright, and their team were able to demonstrate how
acidification affects coral reefs on the ecosystem scale, not just in terms
of individual organisms or species, as other studies have done.
The effects classified as «
acidification» encompass an array
of issues concerning relative concentrations
of various ionic compounds that are dynamically
controlled by marine life using regulatory pumps etc..
The intense variability and multiple, complex
controls on pH implies that the concept
of ocean
acidification due to anthropogenic CO2 emissions can not be transposed to coastal ecosystems directly.
Scientists pondering geoengineering ideas argue that such cooling schemes could be hard to
control and wouldn't address the
acidification of the oceans caused by CO2.