// lecture 39 Flashcards
Mikhail Budyko - 1974
proposed injecting sulfur dioxide in the stratosphere to cool the earth (like volcanoes).
Edward Teller and collaborators - early 1990s
proposed putting designer (nanotech) particles into the stratosphere to deflect sunlight.
1992 - The National Academy of Sciences issues a
detailed study on geoengineering options, including a cost-benefit analysis for each option.
2006 - Paul Crutzen (Nobel Prize winner for his work on the Ozone Hole) argues
that the scope and speed of climate changes due to increasing CO2 – coupled with the lack of any progress on mitigation – requires sulfate aerosol geoengineering solution be seriously considered.
Why should we consider geoengineering?
- Many see little progress in mitigation efforts. This could be the only way we avoid serious harm.
- The potential for unanticipated climate catastrophes. what if the West Antarctic Ice Sheet started to collapse? Huge drought or lots of violent storms that are clearly linked to global warming.
- Could be a much cheaper solution than mitigation.
- Hard to rule out high climate sensitivities.
Uncertainty in Climate Sensitivity
High sensitivity climates are hard to rule out. Very high temperature changes (e.g., 8 C) are unlikely, but hard to rule out (on the other hand, small temperature changes like 1 C are essentially impossible).
Two Main Strategies of Geoengineering.
- Taking CO2 out of the atmosphere.
- “Solar radiation management”: blocking out the Sun
to cool the Earth back down. What most people are talking about when they refer to geoengineering.
Remove CO2 from the air – scrubbing CO2
This is different from, and less practical than, capturing it at the power plant, which we call carbon capture and sequestration.
- Many processes can do this, but very expensive & energy intensive. No realistic way to do this at a large scale.
Ocean Fertilization
Promote enhanced CO2 take-up by the ocean
through photosynthesis. Add trace metals (iron) where they are needed gives leverage.
- It’s not practical, because not enough carbon gets buried per unit of effort. Life in the ocean spins up, but only a small fraction of the carbon gets buried.
Promote enhanced CO2 take-up by
the land in soils or vegetation.
Ocean photosynthesis
- Life in the ocean buries some carbon in sediment – the
Biological Pump. - In some places life is limited by trace metals (e.g. Iron) and we can add some to speed up life there.
Ocean Primary productivity very Seasonal
obviously more productive with photosynthetically active radiation from Sun.
Downsides of Photosynthesis by Fertilizing the Ocean
- Studies show after the phytoplankton bloom, most carbon goes right back into the atmosphere.
- Major disruption to the base of the marine food chain.
- Could cause harmful algal blooms.
Haida Salmon Restoration Corporation
Village of Old Masset funded a project to spread 100
tons of iron sulfate off the coast of BC, to boost biological productivity, enhance salmon and store
carbon. July 2012.
Terra preta
black earth” in Portuguese; in the Amazon basin has tons of old carbon in it. Created by humans between 450 BC and AD 950. Adding charcoal to soil can keep carbon there for thousands of years! Extremely high quality soil too.