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numbers are potentially catastrophic.<br />

Recall that a global average conceals<br />

uneven distribution spatially and over<br />

the seasons. W. Michael Haneman at<br />

the University of California, Berkeley,<br />

estimates that summertime temperatures<br />

in the agriculturally rich Central<br />

Valley in California would rise some<br />

2.5 times the global average. Using the<br />

upper bound of Sokolov’s estimate, this<br />

suggests a rise of 33.3 degrees Fahrenheit,<br />

far above catastrophic levels.<br />

Second, we also do not know what,<br />

if any, binding international agreements<br />

on mitigating greenhouse gas emissions<br />

will emerge following the termination<br />

of the Kyoto Protocol obligations in<br />

2012. The aspirational target of capping<br />

temperature rise to 2 degrees Celsius<br />

agreed to at the U.N. climate summit in<br />

Cancun, Mexico, last year is ambitious<br />

but has no legal force, does not reflect<br />

either a scientific or economic consensus,<br />

and—despite local initiatives—is<br />

unlikely to be achieved.<br />

Finally, we do not know whether<br />

productivity gains through agricultural<br />

research and development, and possible<br />

productivity gains from carbon fertilization,<br />

can offset production declines<br />

due to global warming. Declines can<br />

be anticipated even if not predicted<br />

with certainty. They will result from<br />

heat stress on plants, greater scarcity<br />

and seasonal variability of water for<br />

rain-fed and irrigated crops, and the<br />

loss of highly fertile delta and river bottomlands<br />

as sea levels rise and flooding<br />

increases. The challenge will be more<br />

difficult because world population and<br />

income growth are expected to double<br />

food demand during the first half of<br />

this century.<br />

In this fraught context, should promotion<br />

of biofuels be part of a green<br />

energy strategy?<br />

Dubious Subsidies and Mandates<br />

If one considers reducing greenhouse<br />

gas emissions and especially carbon<br />

dioxide as the centerpiece of climate<br />

policy, mandates requiring that biofuels<br />

be blended into transportation fuels<br />

appear superficially attractive. Fossil<br />

fuel takes carbon from under the earth,<br />

where it is harmless, burns it and emits<br />

Year of<br />

Agriculture<br />

at<strong>SAIS</strong><br />

that carbon as carbon dioxide to the<br />

atmosphere, where it is harmful. In<br />

contrast, biofuel crops extract carbon<br />

dioxide from the atmosphere during<br />

the growth phase and release carbon<br />

dioxide when they are burned or<br />

decompose. The goal with biofuels is to<br />

recycle carbon, not to add to the active<br />

stock. Let sleeping carbon lie.<br />

This simple idea has been taken up<br />

by many governments with perhaps<br />

more enthusiasm than good sense.<br />

Aside from cost, two major problems<br />

have emerged: indirect increases in<br />

carbon emissions via the conversion<br />

of land to biofuel crops, and pressures<br />

on food production and prices. To<br />

understand these problems, recall that<br />

biofuels come in three main flavors,<br />

depending on their feedstock: ethanol,<br />

made from sugars and starches (corn,<br />

sugarcane); biodiesel from fats and oils<br />

(palm oil, rapeseed, soy); and cellulosic<br />

ethanol from cellulose (woody material,<br />

grasses). The technology for the<br />

first two has been well established for<br />

decades, but except for sugar in Brazil,<br />

the costs are high and large subsidies<br />

are needed. Cellulosic technology is at<br />

an early stage.<br />

Biofuels do not float down from the<br />

heavens like manna. They or their feedstocks<br />

must be cultivated and harvested.<br />

Shifting land from its current status to<br />

biofuel feedstock production can initially<br />

increase carbon emissions from<br />

surface biomass (often by burning vegetation)<br />

and from carbon stored in soils.<br />

For example, clearing marginal land for<br />

corn and preparing the soil will result in<br />

a pulse of carbon emissions today.<br />

Readers inside the Washington<br />

Beltway may have seen the loss of<br />

scrub forest and loblolly pine and the<br />

expansion of soy and corn fields over<br />

the past 20 years as they traversed the<br />

Eastern Shore in their summer trek to<br />

Rehoboth, Delaware. This sort of land<br />

conversion creates a “carbon debt” that<br />

can be repaid over time by the carbonneutral<br />

crop (corn, sugarcane, soy)<br />

displacing the use of fossil fuels. The<br />

debt and timescale can be significant,<br />

however, and lie at the heart of allegations<br />

that biofuels accelerate rather<br />

than moderate global warming.<br />

2011–2012 45

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