https://www.academia.edu/9394141/Great_and_desperate_measures_the_case_for_and_against_geoengineering

Great and desperate measures: the case for (and against) geoengineering

Patrick Moriarty


Great and desperate measures: the case for (and against) geoengineering
AUTHORS Damon Honnery
Associate Professor, Department of Mechanical Engineering at Monash
University
Patrick Moriarty
Adjunct Senior Research Fellow at Monash University

The latest emissions data
from the International Energy Agency suggest that our current methods for
dealing with climate change have not worked. This means we will have to
adapt to climate change, for example by selecting crops more suited to a
warmer climate and abandoning low-lying coastal areas. But adaptation
cannot be our only response; there are limits to adaption, particularly if
the rate at which temperature rises is such that the natural ecosystems we
depend upon cannot adjust in time. That leaves mitigation as our main
response. We could:
*reduce fossil fuel use by using alternative energy sources
*employ carbon capture and storage to prevent fossil fuel carbon dioxide
from entering the atmosphere
*use energy efficiency and conservation to cut overall energy use
*geoengineer the Earth’s climate.

The continued steady rise in atmospheric greenhouse gas concentrations,
especially from fossil fuel combustion, has shown the first three methods
to have been ineffective so far. Because of this failure, geoengineering is
being increasingly considered, and has even been cautiously endorsed by the
Royal Society in the UK. Geoengineering can be defined as the purposeful
manipulation of the climate on a very large scale.
The general idea is to increase the Earth’s albedo. This means reflecting
more incoming solar
radiation back into space, before it is absorbed by clouds, land and
oceans. The most commonly canvassed method is to introduce millions of
tonnes of fine particles (sulphate aerosols) into the stratosphere. Other
methods (such as placing several thousand square km of reflective mirrors
in space) have also been proposed. We could place aerosols, for instance,
by loading the particles into naval cannon shells and lofting them upwards
from ships in tropical waters. Because the aerosols would be rained out of
the atmosphere every couple of years, we would need to continually
replenish the supply. We do have some idea of the probable effects because
of our experience with massive volcanic eruptions. The 1991 Mt Pinatubo
eruption in the Philippines ejected some ten million tonnes of sulphur into
the lower tropical stratosphere. This led to a significant global cooling
of 0.5ºC in the following year. Similar effects have been observed
following other major volcanic eruptions. This natural geoengineering tells
us several things:

Aerosol placement would act rapidly to cool the climate.

The tropics are the best location for aerosol placement.

If serious side effects are found, it is easy to end the intervention by
not renewing stratospheric aerosols. Another important advantage of
geoengineering is that it promises to be far cheaper than the other
mitigation methods already mentioned. But the potential risks from
geoengineering are already becoming apparent, even before it has been
attempted. We face two CO₂ problems, not just one. And unlike the global
warming problem, there is no argument about progressive ocean
acidification. This occurs because of rising levels of dissolved CO₂ in the
oceans, the fate of about half of all emitted CO₂ to the atmosphere.
Acidification will eventually inhibit or slow calcification in some marine
organisms such as corals and some zooplankton, with potentially devastating
consequences for ocean ecosystems. And unfortunately, geoengineering cannot
help with this problem. Because geoengineering does not reduce CO₂
emissions, it cannot reduce the effect these increasing CO₂ emissions have
on the acidification of the ocean. Unless CO₂ emissions are reduced, oceans
will continue to acidify irrespective of any geoengineering. (Alternative
proposals are to dump chemicals in the ocean which neutralise the effect of
CO2, but this could disrupt ocean ecosystems.) Climate models and the
experience of large volcanic eruptions point to another problem.
Geoengineering will lower global rainfall, which will not be welcome in an
increasingly water-short world. And what would happen if the side effects
of geoengineering were so serious that we had to stop?
The world’s temperature would rapidly rise to the level it would have
reached without aerosol placement, because of the higher CO₂
atmospheric concentrations from continued releases. It is this abrupt
temperature rise that poses a serious threat to the viability of many
natural ecosystems.
We would be riding the tiger’s back –
dangerous to stay on, dangerous to get off.
Whatever the balance of the benefits and costs of geoengineering, it’s
clear that neither will be shared uniformly across the globe. There will be
winners and losers. Unlike carbon mitigation, aerosol placement could be
implemented  by a group of nations (think OECD) or even by one nation.

It is unlikely that the country or countries initiating the action will
want to be among the net losers. Given the history of weather modification
for military purposes, geoengineering is unlikely to be  politically
feasible in our divided world. Mitigation (stabilising CO₂ levels or even
returning to earlier, lower levels) is the only safe approach. We will have
to cut emission levels fast, but have little time to act. It will require
an end to our economic growth obsession.
An extension of this argument can be found in Damon and Patrick’s book:

Rise and fall of the carbon civilisation


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