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September 28, JPEG. About halfway between Australia and Hawaii, the Pacific island nation of Tuvalu is an isolated archipelago composed of nine coral islands. All told, its mean elevation is 2 meters 6 feet above sea level, and its land area amounts to about 3 percent of that of New York City. As a low-lying island nation, Tuvalu faces more frequent and severe floods as sea levels rise. The Funafuti Conservation Area encompasses reefs and islets on the western side of the atoll. Researchers looked to Funafuti for early field studies into how coral atolls form. Based on observations made on the — voyage of the HMS Beagle , Charles Darwin proposed that the origins of the ring-like islands were volcanic. By his thinking, atolls evolved from barrier reefs that formed around extinct mid-ocean volcanoes, where corals continued to grow up as the land subsided. Scientists drilled down more than meters 1, feet into carbonate rock without hitting any volcanic material. Subsequent analysis suggested they would have needed to drill approximately twice that deep to reach volcanic rock. The drill site is marked with a commemorative plaque. While the volcanic theory is still generally accepted today, some geologists have since argued that sea level fluctuations can drive atoll formation. According to an alternative model of atoll development, flat-topped banks of carbonate rocks formed in tropical shallow-water environments between about 5 million and 2. As the climate cooled, sea levels dropped, leaving the flat expanses exposed. Slightly acidic rainwater would have then pooled on the rocks and gradually dissolved them from the center out. When sea levels rose again, corals would colonize the raised outer rims. Regardless of how much sea level fluctuations factor into atoll formation, they are a profound concern to those living on Funafati and other Tuvaluan islands today. Scientists expect sea level rise to worsen the effects of tides, waves, and storms, increasing the frequency and severity of periodic flooding on the islands. June JPEG. In a assessment , NASA scientists reported that sea level in Tuvalu was nearly 15 centimeters 6 inches higher than it was 30 years prior. The average rate of increase—5 millimeters 0. Much of the land area and critical infrastructure will sit below the average high tide level by , the report stated. Global Centre for Climate Mobility. It argues that increased scientific monitoring could improve planning for potentially catastrophic events. The country is already taking action to fortify coastal infrastructure on Funafuti and other islands through the Tuvalu Coastal Adaptation Project. Geological Survey. Story by Lindsey Doermann. View this area in EO Explorer. The Pacific island has a storied past in the study of atoll formation and a tenuous future as it adapts to sea level rise. Image of the Day Land Water. The ring shape is the result of coral reefs building up around a former volcanic island in the South Pacific. This astronaut photograph shows Tetiaroa Island, part of the Society Islands archipelago in the southern Pacific Ocean. Tetiaroa is an atoll comprised of thirteen small islets. Image of the Day Land. This astronaut photograph depicts Apataki Atoll, an atoll in the Tuamotu Islands in the south Pacific. Atolls are ring-like coral islands that nearly or entirely enclose a lagoon. The atoll traces the perimeter of what was once the coastline of a volcanic island. It was later visited by Captain Cook in EO Explorer. Funafuti Atoll, Tuvalu. View more Images of the Day:. You might also be interested in view all. Subscribe to our newsletters.

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Thank you for reporting this station. We will review the data in question. You are about to report this weather station for bad data. Please select the information that is incorrect. See more. Log In. Station Offline. Send Report. See more Reset Map. Current Station. Personal Weather Station. Location : Funafuti , Funafuti, Tuvalu. Nearby Weather Stations. Previous Day. Next Day. Top Video Stories. See more Top Video Stories. Partly Cloudy. Actual Time. Civil Twilight. Nautical Twilight. Astronomical Twilight. Length of Visible Light. Length of Day. Tomorrow will be 0 minutes 26 seconds longer. Oct Nov 1. Nov 9. Nov The time period when the sun is no more than 6 degrees below the horizon at either sunrise or sunset. The horizon should be clearly defined and the brightest stars should be visible under good atmospheric conditions i. One still should be able to carry on ordinary outdoor activities. The time period when the sun is between 6 and 12 degrees below the horizon at either sunrise or sunset. The horizon is well defined and the outline of objects might be visible without artificial light. Ordinary outdoor activities are not possible at this time without extra illumination. The time period when the sun is between 12 and 18 degrees below the horizon at either sunrise or sunset. The sun does not contribute to the illumination of the sky before this time in the morning, or after this time in the evening. In the beginning of morning astronomical twilight and at the end of astronomical twilight in the evening, sky illumination is very faint, and might be undetectable. The time of Civil Sunset minus the time of Civil Sunrise. The time of Actual Sunset minus the time of Actual Sunrise. The change in length of daylight between today and tomorrow is also listed when available.

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