Extreme
Pacific sea level events to double in future
Extreme
low sea levels occurred during August in parts of the western
Pacific associated with the ongoing strong El Niño. Data from AVISO
satellite measurements. (credit: Widlansky, et al., 2015)
25
September, 2015
Many
tropical Pacific island nations are struggling to adapt to gradual
sea level rise stemming from warming oceans and melting ice caps. Now
they may also see much more frequent extreme interannual sea level
swings. The culprit is a projected behavioral change of the El Niño
phenomenon and its characteristic Pacific wind response, according to
recent computer modeling experiments and tide-gauge analysis by
scientists Matthew
Widlansky and Axel
Timmermann at
the International
Pacific Research Center, University
of Hawaiʻi at Mānoa,
and their colleague Wenju Cai at Commonwealth
Scientific and Industrial Research Organisation (CSIRO)
in Australia.
During
El Niño, warm water and high sea levels shift eastward, leaving in
their wake low sea levels in the western Pacific. Scientists have
already shown that this east-west seesaw is often followed six months
to a year later by a similar north-south sea level seesaw with water
levels dropping by up to one foot (30 cm) in the Southern Hemisphere.
Such sea level drops expose shallow marine ecosystems in South
Pacific Islands, causing massive coral die-offs with a foul smelling
tide called taimasa (pronounced [kai’ ma’sa]) by Samoas.
El Niño and climate change combine forces
The
team of scientists recently asked, how will future greenhouse warming
affect the El Niño sea level seesaws? The scientist used
state-of-the-art climate models, which accounted for increasing
greenhouse gas concentrations, together with simulations of the
observed climate and tide-gauge records to verify the model results.
They determined that projected climate change will enhance El
Niño-related sea level extremes. By the end of this century the
experiments show that the intensified wind impacts of strong El Niño
and La Niña events are likely to double the frequency of extreme sea
level occurrences, especially in the tropical southwestern Pacific.
“From
our previous work, we know that toward the end of a very strong El
Niño event, the tide-gauge measurements around Guam quickly return
to normal reflecting the east-west seesaw, but those near Samoa
continue to drop as a result of the lagging north-south seesaw,”
explains Widlansky. “During these strong events, the summer
rainband over Samoa, called the South Pacific Convergence Zone,
shifts toward the equator and alters the trade winds and ocean
currents which in turn change the sea level.”
“The
next logical step in our work was to understand how future changes in
winds, projected by most climate models, will impact the interannual
swings in sea level,” recalls Timmermann. “We noted a trend in
greater variability and were surprised at first to find not only more
frequent and prolonged drops in sea level, but also more frequent
high sea level events. This will further increase the risk of coastal
inundations.”
Extreme
high sea level events impact vulnerable coastal communities.
(credit: M. Ford/ UH Sea Grant)
Impacting Pacific island communities
“Our
results are consistent with previous findings that showed the
atmospheric effects of both El Niño and La Niña are likely to
become stronger and more common in a future warmer climate,”
explains Cai.
“The
possibility of more frequent flooding in some areas and sea level
drops in others would have severe consequences for the vulnerable
coastlines of Pacific islands,” says Widlansky.
The
authors hope that better predictability of not only rising sea
levels, but also the sea level fluctuations examined in this study,
will aid Pacific island communities in adapting to the impacts of
climate change as well as shorter-term climate events such as the
ongoing 2015 El Niño.
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