To CRCL Board members and
interested folk.
Nothing's Easy for New Orleans
Flood Control
Science section / The New York
Times / Tuesday, April 30, 2002
By JON NORDHEIMER
NEW ORLEANS - Caught between the
Mississippi and the long
shoreline of Lake Pontchartrain,
this low-lying city has
long depended on levees and luck.
Now engineers say those are not
enough to protect New
Orleans, much of it below sea
level, from a devastating
flood that could threaten it if a
storm surge from a
powerful hurricane out of the
Gulf of Mexico propelled a
wall of water into the lake and
the city.
That event could place vast
sections under 20 feet or more
of water, engineers and
scientists say, with worst-case
computer predictions showing
death tolls in the tens of
thousands with many more people
trapped by high water that
has no natural drainage outlets.
"There's no way to minimize
the amount of devastation that
could take place under such
circumstances," warned Walter
S. Maestri, director of emergency
management of Jefferson
Parish, a suburban region with
455,000 residents on the
city's western and southern
sides.
Perhaps the surest protection is
building up the coastal
marshes that lie between New
Orleans and the sea and that
have been eroding at high rates.
But restoration will
require time, a huge effort and
prohibitive sums of money,
perhaps $14 billion, according to
a study by a panel from
federal and state agencies,
universities and business.
Engineers are considering other
ways to protect the heart
of the city and provide an island
of refuge in the French
Quarter and government centers.
Though such approaches are
less expensive, they come with
their own problems. One plan
involves walling off an area to
keep out water. But where
would the wall be built and who
would benefit from it?
Many residents give little
thought to such matters,
counting on the knowledge that
New Orleans has escaped
hurricane disaster in the past.
The most nervous people are those
paid to worry about such
things, like Dr. Joseph N.
Suhayda, director of the
Louisiana Water Resources
Research Institute at Louisiana
State University. Like other
coastal researchers, he has
been using the latest geological
and meteorological data to
refine computer models of how
different storms would damage
the city.
On a bright spring day with fair
skies and no trace of the
sultry air that will dominate the
weather in the months
ahead, Dr. Suhayda and a few
colleagues drove city streets
1,000 yards from levees that hold
back Lake Pontchartrain.
At New York Avenue, near the
lakefront campus of the
University of New Orleans, the
car stopped, and the
engineer walked over and unfolded
a wood measuring stick to
its 25-foot length. He planted
one end on the pavement and
raised it until it was vertical.
The other end poked into
the sky well above a corner light
pole, but it was still
well beneath the level of a
concrete wall that rose on top
of a grassy slope 100 feet away.
"Behind that," Dr.
Suhayda said, indicating the wall, "is a
canal that runs into Lake
Pontchartrain. Its surface is
roughly about the same as the
lake's surface."
In a hypothetical situation
projected by his computers, Dr.
Suhayda continued, a slow-moving
Category 4 hurricane, with
winds up to 155 miles an hour, or
a Category 5 hurricane
with even stronger winds could
leave water 30 feet deep on
this neighborhood street, which
is more than five feet
below sea level. Though Category
5 hurricanes are very
rare, Camille in 1969 devastated
Pass Christian, Miss.,
just 50 miles east of New
Orleans, and killed scores of
residents with winds that
exceeded 200 miles an hour and a
35-foot storm surge.
In most areas vulnerable to
hurricanes, the water would
drain away quickly. That is not
the case here.
So city planners and engineers
continue to work on ways to
improve an evacuation plan for
the 1.3 million residents in
the metropolitan region and to
soften a storm's blow. Most
long-term projects intended to
blunt a hurricane involve
slowing the loss of marshlands.
One method calls for
additional control gates to let
the Mississippi pour
sediment-rich water into
surrounding lands, a process that
would eventually raise or at
least maintain their
elevation.
Other proposals are to rebuild
eroded offshore barrier
islands, erect a wall of levees
across much of the lower
delta, plug the dredged
containership channel that gives
the Gulf of Mexico waters easy
access to the vulnerable
eastern shore of Lake
Pontchartrain and help defend that
shore with higher flood gates.
Perhaps the most unconventional
is the "community haven"
concept advanced by Dr. Suhayda
and others in the belief
that radical remedies may be
necessary to soften a knockout
punch by nature. More theory than
an organized campaign, it
envisions a two-story-high wall
with flood gates at crucial
intersections to seal off the
southern part of the city
from a bend in the river at the
French Quarter to another
one eight miles west.
If the rest of the city flooded,
Dr. Suhayda said, the
"island" between the
wall and the river's levees could
become a refuge for thousands of
residents fleeing their
homes, as well as preserving the
cultural and government
center.
But obtaining the money on the
scale needed is far tougher
than devising plans, especially
if some skeptics dismiss
the worst-case predictions as
scare tactics to help finance
university research or for
further environmental intrusions
on the coast.
Researchers, though, say they are
not making up the city's
potential peril, which arises
from geology and history. As
tight as a pimento in an olive,
most of New Orleans is
stuffed between the Mississippi
and the lake, and it is
settling as fast as the rest of
the delta or faster, said
Dr. Roy Dokka, a geologist at
Louisiana State.
Although much agonizing has gone
into problems of the
river, and its metaphoric temperaments
have become part of
songs and folklore, it is the
300-square-mile lake that
troubles him, Dr. Dokka said.
As New Orleans grew as a seaport,
petrochemical hub,
tourist destination and cultural
phenomenon, neighboring
marshes were drained and the
levee system expanded to keep
the water out of new suburbs and
industrial parks,
hastening the drying that led to
sinking, and making a bad
situation even worse.
A computerized cross-section of
the city's topography
recently created by L.S.U.
scientists and engineers shows a
shallow bowl-like profile. On the
southern edge along the
river, the rim rises about five
feet above sea level for
most of the French Quarter, a
half-mile-wide sloping plain
created by the river's natural earthen
banks. A flood wall
built by the Army Corps of
Engineers to hold back a
cresting river - which on normal
days moves more than
300,000 cubic feet of water a
second past the city at an
average depth of 90 feet - raised
the levee to a uniform
height of 25 feet above sea
level, or 10 feet above the
average annual high water surface
level of the river, when
water can rush by at the rate of
one million cubic feet of
water, or more, a second.
Most of the city north of the
French Quarter was reclaimed
from a boggy morass. The lowest
sections - residential
areas and shops that sit on
drained marshland at 5 to 10
feet below sea level - form a
wide band near the lake's
southern shore.
New Orleans International Airport
to the west and
industrial complexes and
residential areas to the east are
at sea level or below it.
Spider webs of city canals and
wide ditches that measure
185 miles in length feed 22
pumping stations that lift
water to a height where it can
flow into the lake, over
levees built more than a
half-century ago that stand 15 to
17 feet above sea level.
Water cascading over the levee
wall or flooding from
swollen marshes at the lake's
eastern and western ends is
just one part of the nightmare,
the experts say. Draining
the city after the storm moves
away may take weeks, they
point out. The city would be
trapped inside the levees,
steeped in a worsening
"witches' brew" of pollutants like
sewage, landfill waste, chemicals
and the bodies of drowned
humans and animals.
Bourbon Street could remain under
10 feet of water, with
water swirling above two-story
houses in neighborhoods
closer to the lake.
Dr. Ivor van Heerden, deputy
director of the L.S.U.
Hurricane Center, said that in a
worst-case situation with
incomplete evacuation "we
could have up to 45,000 killed
and 400,000 trapped on roofs,
with 700,000 evacuees who
would now be homeless."
Dr. van Heerden said it would
take at least nine weeks to
pump the city dry.
Pumping stations, which sometimes
fail in heavy seasonal
downpours in a city that receives
nearly five feet of rain
a year, would be inoperative
under those conditions for
days if not weeks, Dr. van
Heerden said. The chemical stew
that would be pumped into the
lake and surrounding marshes
would be an environmental
disaster by itself, he added. He
said that the cost in human
misery might be incalculable
but that the bills for insured
damages, public works
repairs and replacements and the
economic effects might
total $50 billion.
Despite the specter of such
losses, it has been difficult
to find enough money to build up
the protective marshlands,
said Jack C. Caldwell, head of
the state's Natural
Resources Department. Washington
has been disinclined to
earmark billions to protect the
marshland and has resisted
appeals from Baton Rouge to share
revenues from offshore
oil production with the state for
that purpose, Mr.
Caldwell said.
In the meantime, residents take
their chances every
hurricane season, which starts on
June 1. According to his
computer models, Dr. Suhayda
said, the odds that the city
will be hit by a cataclysmic
storm in any given year are
less than 1 in 100.
The American Red Cross is taking
the threat seriously. It
has declared it no longer will
provide hurricane shelters
in the New Orleans area, saying
that placing staff there in
a killer storm will represent too
much risk for its
employees, volunteers and the
general public.
-end-
http://www.nytimes.com/2002/04/30/science/earth/30ORLE.html?ex=1021137864&e
i=1&en=01aceacd56209bab
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