Sea
level variations escalating along eastern Gulf of Mexico coast
Around
the globe, sea levels typically rise a little in summer and fall
again in winter. Now, a new study shows that, from the Florida Keys
to southern Alabama, those fluctuations have been intensifying over
the past 20 years.
29
January, 2014
Around
the globe, sea levels typically rise a little in summer and fall
again in winter. Now, a new study shows that, from the Florida Keys
to southern Alabama, those fluctuations have been intensifying over
the past 20 years. Summer peaks have been getting higher and winter
troughs dipping lower, potentially increasing flooding from
hurricanes and stressing delicate ecosystems, the researchers report.
The
additional summer increase in sea levels over the past two decades
means storm surges can rise higher than previously thought,
increasing how much sea level rise contributes to the flooding risk
from hurricanes, according to Thomas Wahl, a postdoctoral researcher
from the University of Siegen in Germany who is working at the
University of South Florida in St. Petersburg and lead author of the
study.
Global
sea levels rose by about 5 centimeters (2 inches) from 1993 to 2011
and the newfound trend of summer sea level rise has added
approximately 5 centimeters on top of that in the eastern Gulf, the
research team reports. Wahl and colleagues from Florida and England
published their study last week in Geophysical
Research Letters, a
journal of the American Geophysical Union.
Conversely,
an increasingly downward, winter sea level trend along the eastern
Gulf Coast has reduced the flood risk from winter storm surges. At
the same time, the growing gap in the region between summer and
winter sea levels might be disrupting coastal ecosystems adapted to
what was once a relatively stable difference between the seasonal sea
levels, Wahl said.
The
team studied the entire U.S. Gulf Coast but found the trend toward a
greater summer-winter difference only along eastern Gulf shores.
Seasonal sea levels in the eastern Gulf of Mexico followed a steady
cycle from the beginning of the 1900s to the 1990s, increasing in
summer and dropping in winter by roughly the same amount year after
year. But, starting in the 1990s, sea levels have gotten both higher
in the summer and lower in the winter in the eastern Gulf, causing a
significant amplification of the annual cycle, according to the
study.
The
new work is the first to look at the changes to the sea level cycle
for the entire Gulf Coast region in the United States and the first
to encounter such a trend, according to Wahl. "This increase
over a period of almost 20 years is not found elsewhere in the
world," he said.
Wahl
and his colleagues discovered the trend in data from a set of 13 tide
gauges stretching from Key West at the tip of Florida to Port Isabel
on the Texas coast. Nearly all the tide gauges in the eastern Gulf of
Mexico, from Key West to Dauphin Island off the coast of Alabama,
showed a significant change in sea level cycle from the 1990s
onwards. The change in the sea level cycle was not observed in gauges
in the western part of the Gulf, stretching from the Louisiana coast
down to the Texas border with Mexico.
The
20-year increase in the annual amplitude, or difference between the
high summer levels and low winter levels, was 21 percent on average
and as high as 30 percent in some locations, according to the study.
For
example, in Key West, the annual amplitude of the sea level cycle for
the most recent five-year window was 12.4 centimeters (4.9 inches),
4.5 centimeters (1.8 inches) higher than the average amplitude before
1993, when the change in the seasonal sea level cycle started.
In
2013, when Wahl came to Florida on a fellowship to study the Gulf, he
started by looking at the tide gauge record in St. Petersburg. The
surprise of seeing a significant increase there in the seasonal cycle
during the last few years led him to examine the cycle of the entire
U.S. Gulf Coast in the past century.
Although
centimeter increases may seem small compared to storm surges measured
in meters, the increase means smaller surges have the potential to
inundate low-lying areas and cause erosion, Wahl explained. "These
indirect effects on storm surges in addition to the global sea level
rise are often ignored," he said.
On
the other hand, the decline in sea levels in the winter that was
observed in the eastern Gulf reduces the flood risk associated with
winter storm surges. However, changes in sea levels in the winter
could throw off, for example, the salt balance in sensitive coastal
wetlands, Wahl said.
"Very
sensitive ecosystems along the Gulf coast depend on the seasonal
cycle," he said. "If there are significant changes in the
seasonal cycle then this very likely has an effect" on these
ecosystems.
Significant
changes in the seasonal cycle might also affect oil spills, although
the researchers did not look at this effect, Wahl said. The changes
in the seasonal cycle could alter the tides and associated currents,
which could in turn influence the mixing of the oil and when it
reached land, although the impact would likely be small, he noted.
Unlike
global sea level rise, which is driven by temperature and is often
cited as an effect of climate change, the annual sea level cycle is
driven by a variety of local factors including wind, precipitation,
sea level pressure and temperature.
The annual cycle varies from
region to region, and, until recently, was thought to be constant
from year to year. Wahl said it has only been in the past few years
that scientists around the world have begun looking at possible
changes in regional sea level cycles including in the Baltic Sea,
Mediterranean Sea, Chesapeake Bay and the Caribbean.
Coastal
engineers need information about baseline sea levels in order to
build sea walls to protect coastal communities, said Philip
Woodworth, a scientist at the National Oceanography Centre in
Southampton in the United Kingdom, who did not contribute to the
study.
"A
change in the baseline of 5 centimeters could be an important
factor," he said.
Wahl
said the changes he and his co-authors saw in the seasonal cycle in
the eastern Gulf are driven by changes in air temperature and
atmospheric sea level pressure over the past two decades. The
researchers found that since 1990, summers have been getting warmer
and winters have been getting colder in the region. Atmospheric sea
level pressure, which also fluctuates with the seasons, declined more
in the summer and increased more in the winter after 1990.
Warmer
temperatures and lower sea level pressure in the summer led to the
higher water levels being seen in the eastern Gulf, while the lower
winter sea levels were driven by the colder temperatures and higher
pressure seen during that season, according to the study.
Story
Source:
The
above story is based on materials
provided by American
Geophysical Union.
Note:
Materials may be edited for content and length.
Journal
Reference:
Thomas
Wahl, Francisco M. Calafat, Mark E. Luther. Rapid
changes in the seasonal sea level cycle along the US Gulf coast from
the late 20thcentury.
Geophysical
Research Letters,
2014; DOI: 10.1002/2013GL058777
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