This
Year’s Gulf of Mexico Dead Zone Could Be the Biggest on Record
Time,
19
June, 2013
The
near record-breaking Midwestern drought of 2012 shriveled corn crops
and toasted pasture land. But it did have one positive side effect.
The drought significantly reduced the size of the seasonal Gulf of
Mexico dead zone. Less rain led to less fertilizer runoff—the dead
zone is fed by a buildup of nitrogen-based fertilizer in the
Gulf—which meant that the 2012 summer dead zone measured just 2,889
sq. miles. That’s still a zone the size of the state of Delaware,
but it was the fourth-smallest dead zone on record, and less than
half the size of the average between 1995 and 2012.
This
year will be different. Heavy rainfall in the Midwest this spring has
led to flood conditions, with states like Minnesota and Illinois
experiencing some of the wettest spring seasons on record. And all
that flooding means a lot more nitrogen-based fertilizer running off
into the Gulf. According to an annual estimate from National Oceanic
and Atmospheric Administration (NOAA) sponsored modelers at the
University of Michigan, Louisiana State University and Louisiana
Universities Marine Consortium, this year’s dead zone could be as
large as 8,561 sq. miles—roughly the size of New Jersey. That would
make it the biggest dead zone on record. And even the low end of the
estimate would place this year among the top 10 biggest dead zones on
record. Barring an unlikely change in the weather, much of the Gulf
of Mexico could become an aquatic desert.
The
nitrogen nutrients that flow into the Gulf, especially during the
rainy spring season, encourages the growth of explosive algal blooms,
which feed on the nitrogen. Eventually those algae die and sink to
the bottom, and bacteria there get to work decomposing the organic
matter. The bacteria consume oxygen in the water as they do,
resulting in low-oxygen (hypoxic) or oxygen-free (anoxic) regions in
the bottom and near-bottom waters.
That’s
what a dead zone—water, essentially, without air. Sealife—including
the valuable shellfish popular in Gulf fisheries—either flee the
area, much as you or I would if someone were to suck all the oxygen
out of the room, or die. That’s why the dead zone matters—the
larger it is, the greater the populations of fish that might be
affected. With commercial fisheries in the Gulf worth $629 million as
of 2009—and still recovering from the impact of the 2010 oil
spill—the dead zone means business.
The
major factor driving the size of the dead zone—beyond changing
flooding patterns—is the use and overuse of fertilizers in
America’s rich Midwestern corn belt. The U.S. Geological Survey
estimated that 153,000 metric tons of nutrients flowed down the
swollen Mississippi and Atchafalaya rivers during May—a 16%
increase over the nutrient load average seen during the past 34
years. And as James Greiff of Bloomberg points out in a recent piece,
those nutrients are used disproportionately to feed one particular
crop:
The
culprits behind the dead zone are many, but one deserves special
attention: corn. Unlike, say, soybeans, which can grow without
fertilizer, corn can’t grow without it. It takes 195 pounds of
fertilizer to grow an acre of corn.
And
the U.S. grows a lot of corn — more than any other country. What’s
more, 40 percent of the U.S. corn crop is devoted to making ethanol,
which fuel companies must blend with gasoline under a congressional
mandate. The Gulf dead zone is yet another reason for Congress to
kill that mandate.
A
state-federal task force was actually set up in 2008 with the aim of
reducing the nutrient flow in the Mississippi by 45% by this year—but
as the numbers demonstrate, there hasn’t been much success. Farmers
could be encouraged to use fertilizer more efficiently—Greiff
suggests ending the practice of applying fertilizer to fields in the
fall after crops are harvested, and instead laying it down in the
spring. They should also limit the amount of water running off their
land, much of which ends up in the rivers and then the Gulf.
Of
course, Midwestern farmers care chiefly about the crops in their own
fields, not what might be happening in the Gulf of Mexico, hundreds
of miles downstream. (And the American farmer is just a bit more
politically powerful than Gulf fishermen, let alone
environmentalists.) But that invisible telecoupling is what make
today’s environmental threats—climate change, ocean
acidification, the wildlife trade—so devilishly complex. Just
thinking about it is enough to suck the oxygen right out of the room.
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