7 - Geoengineering Flashcards
What is geoengineering?
The deliberate large-scale intervention in the Earth’s climate system in order to moderate global warming
What are some issues of geoengineering?
Ways of intervention
Feasibility
Uncertainties
Effectiveness, costs and environmental impact
Governance and public acceptance
Name the two types of geoengineering strategies
Carbon dioxide removal(CDR) techniques - addresses the root of climate change by removing GHGs from atmosphere
Solar radiation management(SRM) techniques - only attempts to offset effects of increased GHG concentrations by increasing albedo - does not solve root of issues
Name some examples of CDR techniques.
Pumping liquid CO2 to deep sea/into rocks
Iron fertilisation of sea
Name some examples of SRM techniques.
Stratospheric aerosols
Cloud seeding
Cloud brightening
Describe some issues of Carbon Capture and Storage(CCS).
Only applicable to large sources & storage effectiveness is questionable - may be inefficient
Describe the process of ocean storage.
Fixing a pipeline from the power plants to bodies of water - this results in more ocean acidification with gaseous or liquid CO2 being released from the pipeline & the liquid CO2 creating lakes along the ocean surface
May created CO2 lakes along ocean surface which are uninhabitable
Describe the process of geological storage.
Involves pumping gas downward into the Earth(e.g. in oil fields where infrastructure already in place)
Long term storage is limited by diffusional loss and tectonic stability - 1% loss rate
Describe the climate effects of aerosols.
Direct effect - net cooling as aerosols scatter and absorb radiation
First indirect effect - cooling as aerosols increase number concentration of cloud droplets and ice particles
Second indirect effect - cooling as aerosols decrease precipitation efficiency
Other indirect and semi-direct effects - cooling/warming
How did Mount Pinatubo demostrate the climatic effects of aerosols?
The volcanic aerosols in the stratosphere excites the positive phase of the NAO - differential heating between low and high latitudes in stratosphere, strenghtening of polar vortex in winter, planetary waves reflected back to troposphere, circulation pattern with warm air advection over NH continents
Therefore, overall tropospheric cooling although warming possible in some regions
Contrast CDR and SRM.
SRM cheaper & fast to implement although it does not address ocean acidification and affects both the hydrological cycle & atmospheric circulation