The short documentary “Linking the Islands” looks at concrete ways Tuvalu is addressing the challenges communities face, including the installation of a disaster early warning system.
Challenges Tuvalu faces as a result of climate change
As low-lying islands lacking a surrounding shallow shelf, the communities of Tuvalu are especially susceptible to changes in sea level and undissipated storms.
At its highest, Tuvalu is only 4.6 metres (15 ft) above sea level, and Tuvaluan leaders have been concerned about the effects of rising sea levels for a few years.
It is estimated that a sea level rise of 20–40 centimetres (8–16 inches) in the next 100 years could make Tuvalu uninhabitable.
Whether there are measurable changes in the sea level relative to the islands of Tuvalu is a contentious issue. There were problems associated with the pre-1993 sea level records from Funafuti which resulted in improvements in the recording technology to provide more reliable data for analysis.
The degree of uncertainty as to estimates of sea level change relative to the islands of Tuvalu was reflected in the conclusions made in 2002 from the available data. The uncertainty as to the accuracy of the data from this tide gauge resulted in a modern Aquatrak acoustic gauge being installed in 1993 by the Australian National Tidal Facility (NTF) as part of the AusAID-sponsored South Pacific Sea Level and Climate Monitoring Project. The 2011 report of the Pacific Climate Change Science Program published by the Australian Government, concludes:
"The sea-level rise near Tuvalu measured by satellite altimeters since 1993 is about 5 mm (0.2 in) per year."Tuvalu has adopted a national plan of action as the observable transformations over the last ten to fifteen years show Tuvaluans that there have been changes to the sea levels. These include sea water bubbling up through the porous coral rock to form pools at high tide and the flooding of low-lying areas including the airport during spring tides and king tides.
The atolls have shown resilience to gradual sea-level rise, with atolls and reef islands being able to grow under current climate conditions by generating sufficient sand and coral debris that accumulates and gets dumped on the islands during cyclones. Gradual sea-level rise also allows for coral polyp activity to increase the reefs.
However, if the increase in sea level occurs at faster rate as compared to coral growth,[280] or if polyp activity is damaged by ocean acidification, then the resilience of the atolls and reef islands is less certain.
The 2011 report of Pacific Climate Change Science Program of Australia concludes, in relation to Tuvalu, states the conclusions that over the course of the 21st century:
- Surface air temperatures and sea‑surface temperatures are projected to continually increase
- Annual and seasonal mean rainfalls are projected to increase
- The intensity and frequency of extreme heat days are projected to increase
- The intensity and frequency of extreme rainfall days are projected to increase
- The incidence of drought is projected to decrease
- Tropical cyclone numbers are projected to decline in the south-east Pacific Ocean basin
- Ocean acidification is projected to continue
- Mean sea-level rise is projected to continue wiki
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