Kilimanjaro's Glaciers May Last Longer Than Predicted

Nick Wadhams
for National Geographic News
May 1, 2007

The fabled snows of Tanzania's Mount Kilimanjaro may not succumb to global climate change as quickly as scientists had feared.

A joint Austrian-U.S. research team that took seven years of measurements from weather stations atop Africa's tallest mountain says that its ice fields will be around for another 30 to 40 years, while the glaciers on its slopes could last even longer.

Kilimanjaro's icepacks have been retreating since the 1800s, but "the vanishing of those glaciers between 2015 and 2020 as reported some years ago is definitely unrealistic," said study participant Thomas Moelg of the University of Innsbruck.

That's good news for Tanzania's tourism industry. Thousands of tourists visit Kilimanjaro each year, and officials worry that many of these visitors will head elsewhere if the 19,340-foot (5,895-meter) peak's ice disappears (Tanzania map).

2006 Comeback

The research team found new evidence showing that lower precipitation—and not rising temperatures on the summit—is the main cause for the Kilimanjaro glaciers' retreat.

The abundant snows needed to maintain the ice fields come from weather patterns that form in the Indian Ocean. A computer simulation of weather patterns since the year 1500 showed that such systems have formed less often in recent years.

The mountain's ice, for example, retreated by about a foot and a half (a half meter) each year starting in 2000, when the researchers began taking measurements. (Related story: "Mount Kilimanjaro's Glacier Is Crumbling" [September 23, 2003].)

The glaciers now measure about 0.8 square mile (2 square kilometers), down from 4.6 square miles (12 square kilometers) in 1912.

But in 2006 an El Niño weather pattern helped bring heavy snowfall that almost buried weather stations on Kilimanjaro. The storms also thickened the peak's glaciers, increasing their thickness even though their surface area stayed the same.

El Niño had been known to bring more precipitation to low-level ecosystems in East Africa. But the finding that it did the same at higher altitudes is new.

The findings push back slightly the date the mountain is expected to completely lose its ice, the researchers say.

Continued on Next Page >>




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