Does global warming
threaten US coastal regions with stronger hurricanes? The
facts will blow you away!
by
Dr. Anthony R. Lupo
Department of Soil and Atmospheric Sciences
University of Missouri-Columbia
Each year, Dr. William
Gray and the hurricane forecast team in the Atmospheric Science
Department at Colorado State University and the Tropical Prediction
Center issue predictions regarding the expected hurricane frequency
within the Atlantic Ocean basin for the upcoming hurricane season.
These predictions are based on many different global or local climatic
variables and parameters. The forecasts usually are issued near
the beginning of the season (early June) and are revised early in
August. This year (1999), the Atlantic Hurricane season is expected
to be busy because there is a strong connection between the absence
of an El Niño event and increased Atlantic hurricane activity.
In an attempt to remain
on the cutting edge of climate science, Vice President Al Gore has
made even longer-range predictions regarding global hurricane activity.
In many speeches on the subject of the environment, the Vice President
predicts more and stronger hurricanes as part of our globally-warmed
future. This was especially true in the wake of Hurricane Mitch.
That record-breaking storm devastated Central America in October
1998 and the Vice President linked it to global warming in his speeches.
His predictions were featured in Newsweek and resulted in
his front-cover appearance.
Intense media coverage
of that devastating hurricane brought home horrifying images of
disaster. On many occasions, the package came complete with apocalyptic
pronouncements from the Vice President and others about the likelihood
of more "Mitches."
Even before Mitch was
a cluster of thunderstorms in the Caribbean, concern had been raised
about the future occurrence and intensity of Atlantic Ocean basin
(and to some extent, global) hurricane activity. This heightened
interest is a result of the growth in population centers along the
East and Gulf Coasts of the United States and the damage brought
by recent storms such as Hugo (1989), Andrew (1992), and Fran (1996).
Each brought with it damage totaling billions of dollars even though
none were in the same category as Hurricane Mitch or Hurricane Camille,
which raked the Gulf Coast in 1969. Hurricane Camille is regarded
as the strongest hurricane to have made landfall along the US coast.
Recent articles, such
as that by Van Der Vink et al. (1998), show that damage totals
and property losses from hurricanes are increasing steadily. Kunkel
et al. (1999) found, "There has been a steady and substantial
increase in hurricane losses. However, there has been no corresponding
upward trend in hurricane frequency and intensity. The observed
increases are due entirely to increased societal exposure along
the vulnerable coastlines." In plain language, the increase
in population along the coasts, combined with increased ownership
of property – and more expensive property – means that there is
a greater likelihood of property losses as hurricanes move inland.
Kunkel, et al., go on to cite other work showing that if
damage estimates from previous years are scaled to mid-1990’s conditions,
all else being equal, there is little trend in hurricane damage
estimates along the US coastline, although the 1940’s and 1950’s
stand out as periods of significant loss, relatively speaking.
Despite these facts,
one cannot help but notice that media coverage of weather events
and weather-related disasters has increased dramatically. Studies
of this phenomenon, e.g. Ungar (1999), demonstrate that news coverage
of these events has increased at least three-fold in the last 25
years or so. The proliferation of ‘round-the-clock news sources
is a large contributor to this phenomenon. Also, sources such as
The Weather Channel increase their coverage of major storms, including
hurricanes, as they threaten US population centers.
It is likely that this
greater news coverage combined with substantial improvements in
forecasting technique and skill by the National Weather Service
(including The National Hurricane Center) has increased public awareness
of the dangers that hurricanes pose and the lead time available
for evacuation of population centers. The result is a substantial
decrease in loss of life from recent storms. Unfortunately, the
increase in media coverage has also brought with it the spread of
misinformation regarding the possibility of future hurricane disasters
– as evidenced by coverage of the Vice President’s linkage of global
warming to more and stronger hurricanes along the US coast in the
future.
While bona fide
hurricane forecasts by scientific groups such as Colorado State
University’s Department of Atmospheric Science and the Tropical
Prediction Center have a measurable record of success, it is difficult
to project with any certainty far into the future as to whether
or not there will be more or stronger hurricanes. This is especially
true for hurricanes striking the US coastline. Only by studying
past trends of hurricane activity and their linkages to global and
local environments are we provided with vague clues about future
hurricane activity.
A number of studies
– e.g. Landsea (1993), O’Brien et al. (1996), Bove et
al. (1998), and Landsea et al. (1999) – have examined
the issue of past Atlantic Ocean Basin hurricane activity, especially
those that strike the coast. Landsea et al. (1999) found
that there to have been a decrease in the number of US landfalling
hurricanes between 1944 and 1996, with no significant trend in hurricane
intensity. Landsea (1993) found that there has been a tendency toward
fewer intense hurricanes over a similar time period (1944 – 1991).
This was reflected by a tendency toward fewer landfalling, intense
hurricanes during the 1970’s and 1980’s when compared to the 1940s
and 1950s.
It is now well known that there is
a connection between the El Niño/La Niña oscillation and hurricane
activity in the Atlantic Ocean Basin. For example, there is a tendency
toward fewer hurricanes during El Niño years and more hurricanes
during La Niña years. O’Brien et al. (1996) and Bove et
al. (1998) studied this variation with respect to landfalling
US hurricanes. They found that fewer hurricanes make landfall along
the US coast during an El Niño year, and that the chance for a major
hurricane is reduced as well.
Landsea (1993) demonstrates that hurricane
frequency and intensity may follow even longer-term cycles than
the El Niño-related variability. This study and others have linked
long-term pressure and sea surface temperature trends and oscillations
in the Atlantic Ocean Basin to hurricane frequency. As mentioned
above, these factors are the basis for the statistically-based annual
hurricane forecasts.
Johnston and Lupo (1999) examined variations
in Atlantic Ocean Basin hurricane activity with respect to longer-term
sea surface temperature variations in the Pacific Ocean Basin. A
50 – 70 year sea surface temperature variation, the North Pacific
Oscillation (NPO), recently has been shown to modify and modulate
the well-known shorter-term oscillation known as El Niño (Gershanov
and Barnett, 1998). They found that when the NPO generally weakens
El Niño events (as was the case during the period 1947 – 76), there
tended to be more Atlantic hurricanes, annually, and little variation
in year-to-year hurricane activity and intensity between El Niño
and La Niña years. Their study also found that there was decreased
Atlantic Ocean Basin hurricane activity during the periods from
1938 – 46 and 1977 – 98. These periods also exhibited strong El
Niño-related variability with fewer and weaker hurricanes occurring
during El Niño years than during La Niña years.
The Johnston and Lupo (1999) study
also found little long-term trend in the overall frequency of hurricane
occurrence over the Atlantic Ocean Basin (Figure 1), and
any trend was found to be statistically insignificant. The data
in Figure 1 can be downloaded directly from the Colorado State University
Archive compiled by Dr. Christopher Landsea (Landsea, 1993) http://typhoon.atmos.colostate.edu
or through the UNISYS weather processor (Vietor, 1999).
Fig. 1: (Taken from Johnston
and Lupo, 1999) The 61-year Atlantic Ocean Basin hurricane frequency
distribution and trend. Data cover the period from 1938–98.
All of these studies
demonstrate the complex relationship between long-term variations
in hurricane frequency and intensity, and the global environment.
Only by understanding these and many other factors can we properly
assess the future risk faced by US coastal areas. Only by being
prepared for the possibility of a landfalling hurricane every summer
and fall will the loss of life and property be minimized.
In assessing the Vice
President and his followers’ hurricane forecasts, it is best to
read the words of the scientists who study hurricanes at Colorado
State University and the Tropical Prediction Center http://typhoon.atmos.colostate.edu/forecasts
:
Some individuals
will interpret … hurricane activity since 1995 as being related
in some way to increased man-made greenhouse gases. … There is
no reasonable way such an interpretation can be made. Anthropogenic
greenhouse gas warming, even if a physically valid hypothesis,
is a very slow and gradual process. ... And even if man induced
greenhouse increases were to be interpreted as causing global
mean temperature increase over the last 25 years, there is no
way to relate such a small global temperature increases to more
intense Atlantic Basin hurricane activity during this same period.
Atlantic intense … hurricane activity showed a substantial decrease
during 1970 – 1994 to only about 40 percent of the amount of intense
hurricane activity which occurred 25 – 50 years ago. These up-and-down,
multi-decadal changes have occurred many times in the past and
are considered to be natural.
References:
Bove, M.C., J.B. Elsner, C.W. Landsea,
N. Xufeng, and J.J. O’Brien, 1998: Effect of El Niño on U.S. landfalling
hurricanes. Bull. Amer. Meteor. Soc., 79, 2477–2482.
Gershanov, A., and T.P. Barnett,
1998: Inderdecadal modulation of ENSO teleconnections. Bull.
Amer. Meteor. Soc., 79, 2715–2725.
Johnston, M.G., and A.R. Lupo, 1999:
The interannual Variability of Atlantic Basin Hurricane Activity.
Preprints of the Eighth Conference on Climate Variations, 13–17
September,1999, Denver, Colorado.
Kunkel, K.E., R.A. Pielke Jr., and
S.A. Changnon, 1999: Temporal fluctuations in weather and climate
extremes that cause economic and human health impacts: A review.
Bull. Amer. Meteor. Soc., 80, 1077-1098.
Landsea, C.W., R.A. Pielke Jr., A.
Mestas-Nuez, and J. Knaff, 1999: Atlantic Basin hurricanes: Indicies
of climate changes. Climatic Change [in press].
Landsea, C.W., 1993: A climatology
of intense (or Major) Atlantic hurricanes. Mon. Wea. Rev.,
121, 1703–1713.
O’Brien, J.J., T.S. Richards, and
A.C. Davis, 1996: The effect of El Niño on US landfalling hurricanes.
Bull. Amer. Meteor. Soc., 77, 773–774.
Ungar, S., 1999: Is strange weather
in the air? A study of U.S. national network news coverage of
extreme weather events. Climatic Change, 41, 133-150.
Van der Vink, G., R.M. Allen, J.
Chapin, M. Crooks, W. Fraley, J. Krantz, A.M. Lavigne, A. LeCuyer,
E.K. MacColl, W.J. Morgan, B. Ries, E. Robinson, K. Rodriquez,
M. Smith, and K. Sponberg, 1998: Why the United States is becoming
more vulnerable to natural disasters. EOS, Transactions, American
Geophysical Union, 79, 533,537.
Vietor, D., 1999: UNISYS Weather
Processor (WXP). [Available online at http://weather.unisys.com
].
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