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Page 447
Screening Out Some Sunlight
Another option for mitigating a global warming would be to try
to control the global radiation balance by limiting the amount of
incoming radiation from the sun. This could be done by increasing
the reflectivity of the earth, i.e., the albedo. Proposals for
increasing the whiteness of roofs and surface features would have
some effect, but only a fraction of incident solar radiation
reaches the earth's surface and a purposeful change in albedo would
have more impact if done high in the atmosphere. According to
Ramanathan (1988), an increase in planetary albedo of just 0.5
percent is sufficient to halve the effect of a CO2 doubling. Placing a screen in the
atmosphere or low earth orbit could take several forms: it could
involve changing the quantity or character of cloud cover, it could
take the form of a continuous sheet, or it could be divided into
many ''mirrors" or a cloud of dust. Preliminary characterizations
of some of the possibilities that might be considered are provided
below.
Estimating Screen Parameters
The calculation here assumes the screen is a continuous sheet.
Note that if the dust particles are of a size comparable to the
wavelength of light, scattering effects will have to be taken into
account.
Given the equatorial radius of the earth and a nominal low orbit
of 222 km, the radius of the sphere in which the sheet, or parasol,
is to be located is 6.6 × 103 km. Then the area of the sphere to
completely wrap the earth is 5.5 × 1014 m2.
To compensate completely for the greenhouse warming from a doubling
in the concentration of CO2 in the
atmosphere, 3,4 the parasol must cover 1 percent of
the area, or 5.5 × 1012
m2.
If this parasol must be 1 micron (µm) thick, 5.5 ×
106 m3 of material is required. At a density
of 1 g/cm3, 5.5 × 109 kg would have to be lifted into low
earth orbit. The cost of establishing such a project is dominated
by the cost of putting the parasol into orbit. At an optimistic
cost of $1,000/kg, the cost of lifting the material into orbit
would be $5.5 trillion.5 Such a
parasol would mitigate about 1000 Gt of carbon emissions, for a
cost of about $5.5/t C mitigated or about $1.5/t CO2 (rounding the number). At current launch
costs of $10,000/kg, the cost would be $55/t C mitigated or about
$15/t CO2.
The assumption that a 1 percent decrease in sunlight is
equivalent to mitigating the greenhouse effect of 1000 Gt of carbon
(or 4000 Gt CO2) is key for all of
the estimates that follow.6
Ramanathan's increase of 0.5 percent in planetary albedo quoted
above as sufficient to halve the effect of a CO2 doubling is used here and below as a 1
percent screening effect for estimating purposes. Using Figures 3.1
and 3.2 of the report of the Synthesis Panel (Part One), we see
that the total change in greenhouse gases since