Summary.
Hurricane Sandy struck the state of New Jersey and the New York metropolitan area on Monday
October 29, 2012 . It caused damage estimated to range as high
as US$50 billion, much of it due to storm surges that impacted wide stretches
of shoreline in New
Jersey ,
the heart of New
York City ,
and eastward along New
York
and Connecticut .
The ravages of the
storm could be due to factors related to global warming, such as increases in
the moisture content of air over warm ocean waters, rising sea levels, and a
blocking high pressure system that forced the path of the storm toward land.
Global warming is
expected to worsen the impacts of extreme weather events such as Hurricane
Sandy. Society is faced with the
prospect of having to remediate their effects as emergency situations each time
one occurs. Costs of such efforts affect
us all, since they ultimately create a demand for higher taxes and for higher
insurance premiums. An alternative would
be to undertake investments now to eliminate fossil fuels from our energy
economy. The sooner the world
decarbonizes its energy usage, the smaller the accumulated level of atmospheric
greenhouse gases will be, and the less harmful will be the effects of global
warming on the people of the world.
Why was Sandy destructive? The
climate science underlying the warming of the planet provides predictions, or
scenarios, in terms of probabilities of trends occurring over long time periods
and spanning wide regions of the planet.
Long term projections of future trends in the climate are not
able to ascribe causes for short term weather events, such as
hurricanes, with certainty. In addition,
not enough time has passed as of this writing for climate scientists to assess
Hurricane Sandy in terms of its relationship to the warming of the planet.
Nevertheless, three
factors from warming involved in hurricane activity include increased moisture
content of air, higher sea level, and a weather block that caused the storm to
shift its course. First, as water
temperatures get warmer, the absolute amount of water vapor that the air above
it can hold increases by about 7% per ºC (about 4% per ºF) (for any
temperature, this amount defines 100% on the scale of relative humidity). As the ocean surface warms, a storm such as a
hurricane picks up more water vapor which can be deposited as rain as the storm
proceeds.
Second, sea levels
have been rising since the industrial revolution began. Glaciers and land-based
ice sheets have been melting, contributing new water to the oceans; this is
attributed at least partly to global warming.
Also, water expands by about 0.026% per ºC at 25 ºC (0.015% per ºF at 77
ºF). This expansion can proceed only upwards. Although this percentage may seem
insignificant, increased temperatures of ocean surface water penetrate to sufficient
depths that expansion occurs throughout this layer. This results in measurable increases in sea
level as the earth warms. The long-term
rise in global average sea levels is shown below for the period 1870 to 2000.
Global average sea
level trend from 1880 to 2000, referenced to a zero value given as the average
for the period from 1961 to 1990, in mm.
Source:
Intergovernmental Panel on Climate Change, 4th Assessment Report, 2007; http://www.ipcc.ch/publications_and_data/ar4/syr/en/figure-spm-1.html.
It is seen that
over this interval the global average sea level has increased by about 190 mm
(7.5 in.). Furthermore, a report
published on Nov. 28, 2012
finds that sea levels have been increasing in recent decades even faster than
predicted earlier by the Intergovernmental Panel on Climate Change.
Third, the path
followed by Hurricane Sandy was not typical for Atlantic hurricanes. They usually track northeastward following
the coast of the eastern U. S. Sandy took an abrupt shift westward after
following a northeastward path, due to the presence of a blocking high pressure
air mass over eastern Canada and Greenland . It
is possible that the this blocking high was present as a result of an Arctic
summer in which more sea ice melted this summer than ever recorded
previously. Loss of ice results in
absorbing more heat from sunlight during the Arctic summer than when more ice
is present. It is possible that this
altered weather over the Arctic placed the blocking high in Sandy ’s path, a pattern that would not have been
present without the exceptional extent of melting of Arctic sea ice.
These and other
factors contributed to an unprecedented extent of damage from the storm surge
accompanying Hurricane Sandy; there was also damage and economic loss inland
including massive losses of electric power.
Coincidentally, a report by Grinsted and coworkers (submitted for
publication some months earlier) appeared in the Proceedings of the (U. S.) National Academy of Sciences (commentary here)
. They surveyed records of storm surges
from previous hurricanes and found, using a storm surge index, that
hurricane-associated storm surges have increased recently in correlation with
the increase in the global temperature.
They found that the highest values of the index occurred with the most
extreme storm events. More generally,
climate scientists foresee that the intensity, and possibly the number, of
severe tropical storms will increase as global warming proceeds.
The economic
costs of Hurricane Sandy
are hard to estimate, but are extremely high.
The New York Times reports
that New
York ’s
Governor Andrew Cuomo and New Jersey ’s Governor Chris Christie together have
assembled the aggregate damage assessment of US$71 billion. They intend to petition the U. S. federal government for assistance in
meeting these emergency expenses. This
sum includes US$9 billion estimated by Gov. Cuomo to construct new facilities
and devices intended to mitigate any new threat of more intense, more damaging
storms in the future. Gov. Cuomo broke
down his damage estimates in some detail
, itemizing the categories of government response, individual assistance,
housing, business impact, health, schools, transit, roads and bridges, parks
and the environment, water, waste and sewer, utilities, and government
operation revenue. He estimated that the
storm destroyed or damaged 305,000 housing units, caused 2,190,000 customers to
lose power, and impacted 265,300 businesses. Overall, in 16 states 8,510,000 million
customers lost power.
Gov. Christie
issued a preliminary estimate of damage in New Jersey of US$29.4 billion. His estimates included personal
property, businesses, transportation, utilities infrastructure, and effects on
the state’s tourism industry. As is
likely true for all areas impacted by the storm, more long-term effects include
loss of economic activity, induced population shifts and impacts on the value
of real estate. [Addendum on Dec. 5,
2012 : ADP , the payroll processing firm, estimated
that for the month of November, 86,000 jobs were lost because of the hurricane. Losses were highest in
manufacturing, retailing, leisure and hospitality, and temporary help
industries.]
Insured losses from
Sandy estimated by three firms fall in the range
of US$16-25 billion, according to Zacks Equity Research. In addition, one of the firms
estimated that lost economic activity can be estimated at US$50 billion; these
typically are uninsured and cannot be recovered. Many large insurance companies that cover
losses in the area hit by the storm have indicated that their ability to absorb
the benefit payments due from their coverages exceed their capacity. [Addendum on Dec. 5, 2012: For instance, the insurance companies
Travelers Corp. and Allstate report that losses they sustained due to
Hurricdane Sandy are each over US$1 billion.
]
Analysis
Extreme weather
events such as Hurricane Sandy appear to be increasing in number and severity
in recent years, in conjunction with the increasing global average
temperature. This pattern is consistent
with the expectations from climate modeling for a warming planet, which
foresees, at various locations on the surface of the earth, more intense
storms, increasing rainfall with flooding, and more extreme heat waves with
drought. Previous posts have surveyed
the economic consequences of earlier extreme weather in the U. S. and globally.
Global warming and
its harmful consequences for humanity reflect not the annual rate of
emission of greenhouse gases, but rather their total concentration
accumulated in the atmosphere. As
long as even low annual rates of emission continue, the accumulated total
continues to grow. Accumulated
atmospheric greenhouse gases determine the extent of global warming. Carbon dioxide, the principal greenhouse gas,
remains in the atmosphere for decades or centuries. Therefore the greenhouse gas level cannot
retreat to values we experienced in earlier decades. We are stuck with the greenhouse gases
currently present, and the extent of global warming they confer, indefinitely. If the world wishes to stabilize the global
average temperature, necessarily at a new, higher value, we must work toward
developing a zero-carbon energy economy.
Each extreme
weather event is a natural disaster inflicting enormous damage, both physical
and economic, on its victims. Societal
harms also arise as social and local economic structures are disrupted. Each event brings with it the need for
compensation at a large scale to help victims recover and restore their lives
and livelihoods. Eventually all citizens
pay for this, because relief comes from governments, insurance benefits, and
private charities. Costs attributed to
governments potentially lead to higher taxes that we all bear, and insurance
benefit payments lead to higher premiums that many of us will pay.
The alternative to
unscheduled needs for emergency response to extreme weather events is to invest
in creating a carbon-free energy economy. All nations of the world should be
striving to achieve a zero emissions energy economy as soon as possible. This means that instead of creating the need
for even more emergency relief by continuing “business-as-usual”, we invest
early in zero carbon energy. These
investments will help stabilize the atmospheric level of greenhouse gases at
lower levels, so that warming of the planet is attenuated.
© 2012 Henry Auer
No comments:
Post a Comment